Abstract
Characterizing the UV spectral energy distribution (SED) of an exoplanet host star is critically important for assessing its planet's potential habitability, particularly for M dwarfs, as they are prime targets for current and near-term exoplanet characterization efforts and atmospheric models predict that their UV radiation can produce photochemistry on habitable zone planets different from that on Earth. To derive ground-based proxies for UV emission for use when Hubble Space Telescope (HST) observations are unavailable, we have assembled a sample of 15 early to mid-M dwarfs observed by HST and compared their nonsimultaneous UV and optical spectra. We find that the equivalent width of the chromospheric Ca ii K line at 3933 Å, when corrected for spectral type, can be used to estimate the stellar surface flux in ultraviolet emission lines, including H i Lyα. In addition, we address another potential driver of habitability: energetic particle fluxes associated with flares. We present a new technique for estimating soft X-ray and >10 MeV proton flux during far-UV emission line flares (Si iv and He ii) by assuming solar-like energy partitions. We analyze several flares from the M4 dwarf GJ 876 observed with HST and Chandra as part of the MUSCLES Treasury Survey and find that habitable zone planets orbiting GJ 876 are impacted by large Carrington-like flares with peak soft X-ray fluxes ≥10−3 W m−2 and possible proton fluxes ∼102–103 pfu, approximately four orders of magnitude more frequently than modern-day Earth.
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1. Introduction
1.1. UV and Ca ii K Emission from M Dwarfs
Recent ultraviolet (UV) studies have shown that even optically inactive M dwarfs (i.e., those displaying Hα spectra in absorption only) display evidence of chromospheric, transition region, and coronal activity (France et al. 2013; Shkolnik et al. 2014; France et al. 2016) that may significantly affect heating and chemistry in the atmospheres of orbiting exoplanets (e.g., Segura et al. 2003, 2005; Miguel et al. 2015; Rugheimer et al. 2015; Arney et al. 2017). The Measurements of the Ultraviolet Spectral Characteristics of Low-mass Exoplanetary Systems (MUSCLES) Treasury Survey (France et al. 2016) observed seven nearby (d < 15 pc), optically inactive M dwarfs with known exoplanets using the Hubble Space Telescope (HST), Chandra, and XMM-Newton. All display quiescent UV emission lines and soft X-rays (SXRs) that trace hot (T > 30,000 K) plasma in the upper stellar atmosphere (Loyd et al. 2016). UV flares were observed from each M dwarf except GJ 1214, the faintest target.21
An M dwarf's far-UV (912–1700 Å) to near-UV (1700–3200 Å) spectrum is primarily composed of emission lines that form in the stellar chromosphere and transition region, with a few lines originating in the corona. There is comparatively little continuum emission due to the cool stellar photosphere ( K). The H i Lyα emission line (1215.67 Å) is prominent, composing 27%–72% of the total 1150–3100 Å flux (excluding 1210–1222 Å) for the seven MUSCLES M dwarfs (France et al. 2016; Youngblood et al. 2016). The extreme-UV (EUV; 100–912 Å) stellar spectrum is currently not observable in its entirety. No current astronomical observatory exists to observe the 170–912 Å spectral range, and the ∼400–912 Å range is heavily attenuated by neutral hydrogen for all stars, except the Sun. Thus, the EUV must be estimated from other proxies such as Lyα (Linsky et al. 2014) or SXRs (Sanz-Forcada et al. 2011; Chadney et al. 2015). For the M3 dwarf GJ 436, these two methods produce integrated EUV fluxes that agree within 30% (Bourrier et al. 2016; Youngblood et al. 2016).
Knowledge of an exoplanet's radiation environment is critical for modeling and interpreting its atmosphere and volatile inventory. Specifically, the spectral energy distributions (SEDs) of the host stars are essential, because molecular and atomic cross sections are strongly wavelength dependent. High-energy stellar flux heats upper planetary atmospheres and initiates photochemistry (e.g., Lammer et al. 2007; Miguel et al. 2015; Rugheimer et al. 2015; Arney et al. 2017). UV-driven photochemistry can produce and destroy potential biosignatures (O2, O3, and CH4) and habitability indicators (H2O and CO2) in exoplanet atmospheres (Hu et al. 2012; Domagal-Goldman et al. 2014; Tian et al. 2014; Wordsworth & Pierrehumbert 2014; Gao et al. 2015; Harman et al. 2015; Luger & Barnes 2015). In particular, the ratio of far- to near-UV flux determines which photochemical reactions will dominate and thus the resultant planetary atmosphere. Compared to the Sun, M dwarfs have a far-UV/near-UV flux ratio (F(1150–1700 Å)/F(1700–3200 Å)) 100–1000 times larger, and thus most of the known O2 false-positive mechanisms predominately impact planets orbiting M dwarfs. Accurately measuring the intrinsic Lyα flux is critical, because Lyα composes the majority of the far-UV flux. For an atmosphere with 0.02 bars of CO2 similar to that simulated by Segura et al. (2007) with GJ 876's SED (France et al. 2012; Domagal-Goldman et al. 2014), a 20% increase (decrease) in the Lyα flux increases (decreases) the abiotic O2 and O3 column depths by nearly 30%.
M dwarfs are also prime targets for current and upcoming exoplanet searches and characterization efforts (see Scalo et al. 2007; Shields et al. 2016, for comprehensive overviews), due to their ubiquity in the solar neighborhood (Henry et al. 2006), high occurrence rates of small exoplanets (Dressing & Charbonneau 2015), and the larger transit and radial velocity signals their planets provide. The important UV region of an M dwarf's SED cannot yet be predicted by models, although semi-empirical modeling efforts are under way for individual stars (see Fontenla et al. 2016, and references therein). Thus, direct UV observations of individual stars are currently necessary to model and interpret planetary atmospheric observations, and the characterization of the high-energy SEDs of M dwarfs across a broad range of masses and ages is a community priority (e.g., Shkolnik & Barman 2014; France et al. 2016; Guinan et al. 2016; Bourrier et al. 2017).
Accurate UV spectral flux data are vital in understanding the salient physics and chemistry in an exoplanet atmosphere, as well as to break potential degenerate solutions in retrieval models. After HST and before future UV observatories begin operations, there will likely be a decade-long gap in UV observing capabilities. This gap may coincide with the majority of TESS's and CHEOPS's habitable zone (HZ) planet detections and subsequent study with the James Webb Space Telescope (JWST), so establishing a method of estimating UV spectral flux from ground-based proxies is imperative.
In the optical, the Ca ii resonance lines at 3933 Å (Ca ii K) and 3968 Å (Ca ii H), the Na i D resonance lines at 5890 and 5896 Å, Hα at 6563 Å, and the Ca ii infrared triplet (IRT) at 8498, 8542, and 8662 Å are known to be good indicators of stellar chromospheric activity (e.g., Walkowicz & Hawley 2009; Gomes da Silva et al. 2011; Lorenzo-Oliveira et al. 2016, and references therein). However, Hα and Na i D are only good indicators of stellar activity for very active stars (Cincunegui et al. 2007; Díaz et al. 2007; Walkowicz & Hawley 2009) and will not be considered here, because many of our target stars are optically inactive. The contrast between the Ca ii H and K absorption and emission cores is larger than for the Ca ii IRT, so we have limited the scope of this paper to include only one of the Ca ii resonance lines. We focus on the Ca ii K line at 3933 Å and ignore the Ca ii H line at 3968 Å, because is 1.6 Å redward and contaminates Ca ii H at low spectral resolution.
The Ca ii K line profile is a superposition of broad (>1 Å) absorption and narrow ( Å) emission. In the cooler upper photosphere, Ca+ absorbs against the photospheric continuum, and in the hot upper chromosphere, Ca+ emits. In the cool photospheres and lower chromospheres of M dwarfs, Ca is mostly neutral, so the Ca+ absorption is much narrower than for solar-type stars (Fontenla et al. 2016). The Ca+ emission traces stellar activity and has historically been measured for main-sequence stars using the Mt. Wilson S-index (Vaughan et al. 1978; Wilson 1978) and (Noyes et al. 1984). The latter corrects the S-index for a spectral type dependence. Other methods involve isolating the emission core from the absorption by fitting and subtracting a non-LTE radiative equilibrium model to the observed spectrum (Walkowicz & Hawley 2009; Lorenzo-Oliveira et al. 2016).
For the Sun, Ca ii K is known to correlate well with far-UV emission lines over the 11 yr solar cycle and to trace short-timescale variation (e.g., flares; Tlatov et al. 2015). Ca ii K originates from solar features like plages and chromospheric network (Domingo et al. 2009 and references therein) and thus correlates well with the line-of-sight unsigned magnetic flux density (e.g., Schrijver et al. 1989). Ca ii has also been observed to correlate with H i Lyα for M dwarfs (Linsky et al. 2013) despite significant differences between the atmospheric structures of G and M dwarfs (e.g., Mauas et al. 1997; Fontenla et al. 2016) and potentially different dynamo mechanisms (e.g., Chabrier & Küker 2006; Dobler et al. 2006; Browning 2008; Yadav et al. 2015). Other known M dwarf scaling relations include SXR–Ca ii K, Hα–C iv, Hα–SXR, Hα–Mg ii, Ca ii K–Mg ii, and correlations between Ca ii K and various Balmer lines (Butler et al. 1988; Hawley & Pettersen 1991; Hawley & Johns-Krull 2003; Walkowicz & Hawley 2009). We improve on these past UV–Ca ii scaling relations by increasing the size and diversity (e.g., spectral type and magnetic activity) of the M dwarf sample and expanding to more UV emission lines.
1.2. Flares and Energetic Particles
Habitability studies of M dwarf exoplanets are beginning to include estimates of stellar energetic particles (SEPs; Segura et al. 2010; Ribas et al. 2016). SEPs can be accelerated by impulsive flares where particles pass along open magnetic field lines into interplanetary space and by shock fronts associated with coronal mass ejections (CMEs; Harra et al. 2016). SEP enhancements and steady-state stellar winds can contribute significantly to planetary atmospheric loss processes by compressing an exoplanet's magnetosphere (e.g., Cohen et al. 2014; Tilley et al. 2016) and stripping atmospheric particles. SEPs, like high-energy photons, can also catalyze atmospheric chemistry. Segura et al. (2010) found that without the inclusion of particles, large UV flares do not have a long-lasting impact on an HZ planet's O3 column density. However, including SEPs, the expected NOx production will deplete a planet's O3 by ∼95%, requiring centuries for the O3 column density to re-equilibrate after a flaring event ends. This can allow harmful (Voet et al. 1963; Matsunaga et al. 1991; Tevini 1993; Kerwin & Remmele 2007) or bio-catalyzing (Senanayake & Idriss 2006; Barks et al. 2010; Ritson & Sutherland 2012; Patel et al. 2015; Airapetian et al. 2016) UV radiation to penetrate to the surface.
Direct measurements of an M dwarf's energetic particle output are not currently possible, but signatures of particle acceleration in the UV and radio should be detectable in principle. Coronal dimming, when EUV emission lines dim after part of the corona has been evacuated from a CME (Mason et al. 2014), was not observed by the Extreme UltraViolet Explorer (EUVE), likely due to insufficient sensitivity. Type II radio bursts that trace shocks associated with CMEs (Winter & Ledbetter 2015) are being searched for but have not yet been detected on other stars (Crosley et al. 2016), but other possible kinematic signatures of CMEs in observed M dwarf flares have been detected (e.g., Houdebine et al. 1990; Cully et al. 1994; Fuhrmeister & Schmitt 2004). Type III radio bursts are caused by the acceleration of suprathermal electrons from solar active regions and have been detected on the M3 dwarf AD Leo (Osten & Bastian 2006). Probing the astrosphere (analogous to the heliosphere) via high-resolution Lyα measurements allows for time-averaged measurements of the stellar mass-loss rate (Wood et al. 2005a), which includes the accumulation of impulsive events (CMEs) and the quiescent stellar wind. However, it is uncertain if the kilogauss surface magnetic fields of M dwarfs would allow the acceleration of particles into the astrosphere (Osten & Wolk 2015; Drake et al. 2016). Vidotto et al. (2016) find that rapidly rotating stars may have strong toroidal magnetic fields that could prevent stellar mass loss, and Wood et al. (2014) find that the scaling relation between SXR flux and mass-loss rate breaks down for stars with SXR surface flux >106 erg cm−2 s−1, where a fundamental change in the magnetic field topology may occur. On the Sun in 2014 October, the large active region 2192 emitted many large flares, but no CMEs. Strong overlying magnetic fields likely confined the eruption (Sun et al. 2015; Thalmann et al. 2015). As more exoplanetary atmosphere models consider the important influence of stochastic flares (Lammer et al. 2007; Segura et al. 2010; Airapetian et al. 2016; Venot et al. 2016), improving constraints on the fluxes and energies of associated particles is necessary.
To estimate SEPs for any star, we must currently rely on solar relations between SEPs and flare emission (Belov et al. 2007; Cliver et al. 2012; Osten & Wolk 2015). However, traditional flare tracers in the SXR, UV, and U band (3660 Å) originate from thermally heated plasma and probably do not trace particle acceleration processes; CME particles appear to be drawn nonthermally from cooler plasma in the ambient corona (Sciambi et al. 1977; Hovestadt et al. 1981). Yet, correlations between flare tracers and SEPs have been detected, likely due to Big Flare Syndrome (Kahler 1982). Big Flare Syndrome explains positive correlations between flare observables that do not share an identified physical process; for a larger total energy release from a flare, the magnitude of all flare energy manifestations will statistically be larger as well. Big Flare Syndrome occurs because a multitude of energy transport mechanisms between layers of the solar atmosphere makes energy transport efficient. These mechanisms include thermal conduction, radiation, bulk convection, and electron condensation and evaporation. For example, Belov et al. (2007) found a correlation between the Sun's 1–8 Å (1.5–12.4 keV) SXR flux and the >10 MeV proton flux, both observed simultaneously by the Geostationary Operational Environmental Satellite (GOES) system. Although likely due to Big Flare Syndrome, correlations like this are still extremely useful, because they enable an empirical means of estimating particle fluxes from observations of photons—essential for the study of distant stars.
Not all flares produce SEPs, and there may be a fundamental difference between SEP flares and non-SEP flares. Belov et al. (2005) note that an arbitrary SXR flare has a <0.4% chance of being associated with a proton enhancement, although this estimate would likely increase if it were easier to confidently identify associated flares and SEPs, but the probability increases for larger flares. The GOES flare classification scheme (A, B, C, M, X) is based solely on the peak 1–8 Å SXR flux as observed from Earth (1 au), and each letter represents an increased order of magnitude from 10−8 W m−2 to 10−3 W m−2 (Table 1). For example, a C3.5-class flare has a peak 3.5 × 10−6 W m−2 SXR flux at 1 au. Approximately 20% of C-class and ∼100% of X3-class flares occur with CMEs (Yashiro et al. 2006). Thus, estimating the GOES flare classification of an observed stellar flare is important for estimating the probability of associated SEPs.
Table 1. The GOES Classification Scheme of Solar Flaresa
Class | Peak Flux at 1 au | SXR Luminosity | Solar Occurrence | Probability of | Expected Peak >10 MeV | ||
---|---|---|---|---|---|---|---|
(W m−2) | (erg cm−2 s−1) | (W) | (erg s−1) | Rate (hr−1)b | CMEc | Proton Flux (pfu)d at 1 au | |
X100 | 10−2 | 101 | 2.8 × 1021 | 2.8 × 1028 | <2 × 10−6e | ⋯ | ⋯ |
X10 | 10−3 | 100 | 2.8 × 1020 | 2.8 × 1027 | 2 × 10−5f | ∼100% | 3300 |
X | 10−4 | 10−1 | 2.8 × 1019 | 2.8 × 1026 | 0.002 | 80%–100% | 90 |
M | 10−5 | 10−2 | 2.8 × 1018 | 2.8 × 1025 | 0.02 | 40%–80% | 2 |
C | 10−6 | 10−3 | 2.8 × 1017 | 2.8 × 1024 | 0.15 | <40% | <1f |
B | 10−7 | 10−4 | 2.8 × 1016 | 2.8 × 1023 | >0.15g | ⋯ | ⋯ |
Notes.
aClassifications are based on the uncorrected GOES peak flare flux in the long (1–8 Å) band at 1 au. For example, a C3.5-class flare has a peak flux of 3.5 × 10−6 W m−2 at 1 au, and an X20-class flare has a peak flux of 2 × 10−3 W m−2. bVeronig et al. (2002). cYashiro et al. (2006). dCliver et al. (2012); 1 pfu = 1 proton cm−2 s−1 sr−1. eNone have been observed during the GOES era (1976–present). fBetween 1991 August 25 and 2017 February 6, only five flares ≥X10 class were observed. gBelow the sensitivity limits of GOES detectors.Download table as: ASCIITypeset image
To estimate the SEP flux during the great AD Leo flare of 1985 (Hawley & Pettersen 1991), Segura et al. (2010) used scaling relations for active M dwarfs between broadband near-UV and 1–8 Å flare flux (Mitra-Kraev et al. 2005) and solar scaling relations between 1–8 Å flare flux and >10 MeV proton flux (Belov et al. 2005, 2007). Much of the recent UV flare data of M dwarfs have been confined to the far-UV (Loyd & France 2014; France et al. 2016), where HST's COS and STIS spectrographs are most efficient, so we have developed a new method of particle flux estimation from far-UV emission line flares (Section 5).
Ideally, we would directly compare protons with a far-UV emission line directly accessible by HST, but high-cadence, disk-integrated, spectrally resolved far-UV observations of the Sun do not exist. To improve the method of SEP estimation from observed flares, we search for a potential correlation between energetic protons (>10 MeV) received at Earth and an EUV emission line, He ii at 304 Å, which has a similar formation temperature to two high-S/N lines observable in far-UV spectra (Si iv λλ1393, 1402 and He ii λ1640).
This paper is organized as follows. In Section 2, we describe our sample of M dwarfs and list the sources of the observations used in this work. We also describe the reductions performed. Section 3 describes the method we used to measure the Ca ii K equivalent widths of our sample of M dwarfs, and in Section 4 we present the UV–Ca ii scaling relations. In Section 5 we describe the UV–proton scaling relations and their application. We present a summary of the main findings of this work in Section 6.
2. Observations and Reductions
2.1. The M Dwarf Sample
We selected stars with HST UV spectra and ground-based optical spectra either obtained directly by us or available in the VLT/XSHOOTER or Keck/HIRES public archives. The 15 stars that meet this criterion (listed in Table 2) are all early to mid-M dwarfs, are nearby (d < 15 pc), and exhibit a broad range of rotation periods (2 to >100 days) and a broad range of ages (∼10 Myr to ∼10 Gyr). Nine of the 15 M dwarfs are known to host exoplanets.
Table 2. The M Dwarf Sample
No. | Star | d | R | Spectral | W (Ca ii K) | W(Ca ii K) | Data | No. of | ||
---|---|---|---|---|---|---|---|---|---|---|
(pc) | (R⊙) | Type | (K) | (days) | (Å) | (Å) | Includedb | Ca ii K Spectra | ||
1 | GJ 832a | 5.0a | 0.56f | M2f | 3590f | 45.7q | 0.88 ± 0.09 | 0.73 ± 0.07 | H, X, R | 8 |
2 | GJ 876a | 4.7a | 0.38g | M4g | 3130g | 96.7r | 0.82 ± 0.15 | 0.17 ± 0.03 | H, X, R, D | 314 |
3 | GJ 581a | 6.2a | 0.30z,h | M2.5h | 3500h | 132.5q | 0.36 ± 0.08 | 0.25 ± 0.05 | H | 351 |
4 | GJ 176a | 9.3a | 0.45g | M2.5g | 3680g | 39.5s | 1.76 ± 0.27 | 1.76 ± 0.27 | H, D | 256 |
5 | GJ 436a | 10.1a | 0.45aa,i | M3i | 3420i | 39.9q | 0.58 ± 0.07 | 0.33 ± 0.04 | H, D | 257 |
6 | GJ 667Ca | 6.8a | 0.46j | M1.5o | 3450o | 103.9q | 0.44 ± 0.11 | 0.27 ± 0.06 | H | 39 |
7 | GJ 1214a | 14.6b | 0.21k | M4.5o | 2820o | >100t | 1.16 ± 0.2 | 0.040 ± 0.007 | X, M | 10 |
8 | AD Leo | 4.7c | 0.44f | M3f | 3410f | 2.2u | 11.57 ± 1.61 | 6.31 ± 0.88 | H, R | 44 |
9 | EV Lac | 5.1a | 0.36f | M4f | 3330f | 4.38v | 14.86 ± 2.52 | 6.47 ± 1.10 | H | 24 |
10 | Proxima Cena | 1.3d | 0.14l | M5.5l | 3100l | 83.5w | 13.7 ± 5.93 | 2.50 ± 1.08 | X, M, R | 7 |
11 | AU Mic | 9.9a | 0.83m | PMS M1m,p | 3650p | 4.85x | 12.13 ± 2.17 | 11.44 ± 2.05 | H, R | 52 |
12 | YZ CMi | 6.0a | 0.36f | M4f | 3200f | 2.78y | 21.23 ± 4.67 | 5.92 ± 1.30 | H, X | 20 |
13 | GJ 821 | 12.2a | 0.37f | M2f | 3670f | ⋯ | 0.33 ± 0.06 | 0.32 ± 0.06 | H | 26 |
14 | GJ 213 | 5.8a | 0.25f | M4f | 3250f | ⋯ | 0.44 ± 0.12 | 0.15 ± 0.04 | H | 7 |
15 | GJ 1132a | 12.0e | 0.21n | M4n | 3270n | 125n | 1.40 ± 0.01 | 0.504 ± 0.005 | M | 1 |
Notes. Rotation period () uncertainties are typically ≥10%, and effective temperature () uncertainties are typically ±100–200 K unless determined from interferometry (then ±20–100 K). We have rounded all values to the nearest 10 K.
aStars with known exoplanets. b(H) Keck/HIRES, (X) VLT/XSHOOTER, (R) CASLEO/REOSC, (D) APO/DIS, (M) Magellan/MIKE.References. (a) van Leeuwen (2007), (b) Anglada-Escudé et al. (2013), (c) Jenkins (1952), (d) Lurie et al. (2014), (e) Jao et al. (2005), (f) Houdebine et al. (2016), (g) **von Braun et al. (2014), (h) **von Braun et al. (2011), (i) **von Braun et al. (2012), (j) Kraus et al. (2011), (k) Berta et al. (2011), (l) **Demory et al. (2009), (m) **White et al. (2015), (n) Berta-Thompson et al. (2015), (o) Neves et al. (2014), (p) McCarthy & White (2012), (q) Suárez Mascareño et al. (2015), (r) Rivera et al. (2005), (s) Robertson et al. (2015), (t) Newton et al. (2016), (u) Hunt-Walker et al. (2012), (v) Roizman (1984), (w) Benedict et al. (1998), (x) Vogt et al. (1983), (y) Pettersen (1980), (z) Henry et al. (1994), (aa) Hawley et al. (1996). **Interferometry measurements.
A machine-readable version of the table is available.
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Seven of the 15 stars are exoplanet host stars from the MUSCLES Treasury Survey (stars 1–7 in Table 2), and are weakly active with Hα absorption spectra and rotation periods greater than 39 days. These stars are all likely a few billion years old, and they range from M1.5 to M4.5 spectral type. We also included other weakly active M dwarfs, including MEarth planet host GJ 1132 (Berta-Thompson et al. 2015) and two stars from the "Living with a Red Dwarf" program (stars 13–15; Guinan et al. 2016). To increase the diversity in our sample, we included the well-known "flare" stars with HST observations (stars 8–12 in Table 2). These stars are highly active (Hα emission spectra), have short rotation periods (<7 days), and are likely young (<1 Gyr), with the exception of Proxima Centauri ( days, ∼5 Gyr old; see Reiners & Basri 2008; Davenport et al. 2016).
2.2. M Dwarf UV and Optical Data
A goal of the MUSCLES Treasury Survey was to obtain ground-based optical spectra contemporaneous with the HST UV observations. Scheduling changes and weather did not allow for any truly simultaneous UV–optical observations, but several targets have spectroscopic data obtained with the Dual Imaging Spectrograph (DIS) on the ARC 3.5 m telescope at Apache Point Observatory (APO) or the REOSC echelle spectrograph on the 2.15 m telescope at Complejo Astronómico El Leoncito (CASLEO) within a day or two of the HST observations. We also gathered spectra of GJ 1132, GJ 1214, and Proxima Cen on the nights of 2016 March 7–9 using the MIKE echelle spectrograph on the Magellan Clay telescope. Because M dwarfs are prime targets of radial velocity exoplanet searches, there is a wealth of high-resolution Ca ii spectra in the public archives of major observatories, including VLT and Keck. The archival spectra compose the bulk of our Ca ii measurements.
APO/DIS (R ∼ 2500) and CASLEO/REOSC (R ∼ 12,000) spectra were reduced using standard IRAF22 routines. See details in Cincunegui & Mauas (2004) for CASLEO reductions and Cincunegui et al. (2007) and Buccino et al. (2014) for presentation of some of the Proxima Cen and AD Leo observations. Magellan/MIKE spectra (R ∼ 25,000) were reduced using the standard MIKE pipeline included in the Carnegie Python Distribution (CarPy). Science-level VLT/XSHOOTER (R ∼ 6000) data products were obtained from the ESO Science Archive Facility, and Keck/HIRES (R ∼ 60,000) pipeline-reduced spectra were obtained from the KOA archive. As we are interested in looking at as many spectra as possible and measuring only equivalent widths of the Ca ii K line, the pipeline-extracted spectra using MAKEE 23 suit our purposes well. We did not use spectra where the automatic extraction failed or the wavelength calibration was incorrect. We also did not co-add the adjacent orders on which Ca ii K appears, but instead averaged the equivalent width measurements (Section 3) from each order to create one equivalent width measurement per echellogram.
The HST UV spectra were obtained either from the MAST online archive, including the MUSCLES High-Level Science Products24 (HLSPs; Loyd et al. 2016), or the StarCAT portal.25 GJ 1132's (star 15) STIS G140M spectrum was obtained on 2016 February 13. For the seven MUSCLES M dwarfs (stars 1–7), the UV line fluxes come from Youngblood et al. (2016) and France et al. (2016). The UV emission lines of stars 8–14 were directly measured from archival HST spectra or obtained from Wood et al. (2005b).
For AD Leo (star 8) and Proxima Centauri (star 10), we reconstructed the Lyα profiles using the methods described in Youngblood et al. (2016). Proxima Cen's reconstruction is included as part of a 5 Å–5.5 μm SED on the MUSCLES HLSP website.26 The differences between our Lyα reconstructions and those presented in Wood et al. (2005b) are small, ∼20% in integrated Lyα flux for AD Leo and ∼4% in integrated Lyα flux for Proxima Cen. We also reconstructed the Lyα profile of GJ 1132 (star 15; erg cm−2 s−1) for the first time using the methods from Youngblood et al. (2016). Note that the Lyα error bars have been averaged for symmetry in Table 3. All UV fluxes used in this work are shown in Table 3.
Table 3. UV Emission Line Fluxes of the M Dwarf Sample
No. | Star | Si iii | Lyαb | b | Si ii | C ii | Mg ii | ||||
---|---|---|---|---|---|---|---|---|---|---|---|
1 | GJ 832a | 2.55E–15 | 6.33E–17 | 9.50E–13 | 6.00E–14 | 7.65E–16 | 6.33E–17 | 3.78E–15 | 8.18E–17 | 1.84E–13 | 2.02E–15 |
2 | GJ 876a | 8.11E–15 | 1.01E–16 | 3.90E–13 | 4.00E–14 | 1.19E–15 | 7.06E–17 | 1.06E–14 | 1.26E–16 | 3.11E–14 | 9.31E–16 |
3 | GJ 581a | 2.94E–16 | 3.54E–17 | 1.10E–13 | 3.00E–14 | 7.93E–17 | 4.41E–17 | 4.81E–16 | 4.26E–17 | 1.88E–14 | 7.54E–16 |
4 | GJ 176a | 2.15E–15 | 5.84E–17 | 3.90E–13 | 2.00E–14 | 7.34E–16 | 6.49E–17 | 5.43E–15 | 9.66E–17 | 1.56E–13 | 1.53E–15 |
5 | GJ 436a | 5.15E–16 | 4.00E–17 | 2.10E–13 | 3.00E–14 | 1.87E–16 | 4.47E–17 | 1.09E–15 | 5.85E–17 | 3.84E–14 | 1.01E–15 |
6 | GJ 667Ca | 5.07E–16 | 3.91E–17 | 5.20E–13 | 9.00E–14 | 1.29E–16 | 6.13E–17 | 6.50E–16 | 4.63E–17 | 4.12E–14 | 1.10E–15 |
7 | GJ 1214a | 8.05E–17 | 2.77E–17 | 1.30E–14 | 1.00E–14 | 1.36E–17 | 2.09E–17 | 9.83E–17 | 3.00E–17 | 1.66E–15 | 2.70E–16 |
8 | AD Leo | 1.41E–13 | 8.88E–16 | 8.07E–12 | 2.00E–13 | 1.64E–14 | 2.58E–16 | 1.66E–13 | 4.83E–16 | 2.79E–12c | 2.79E–13c |
9 | EV Lac | 3.86E–14 | 1.46E–15 | 2.75E–12c | 5.50E–13c | 2.49E–15 | 4.95E–16 | 3.76E–14 | 6.42E–16 | ⋯ | ⋯ |
10 | Proxima Cena | 2.03E–14 | 7.57E–16 | 4.37E–12 | 7.00E–14 | 2.14E–15 | 2.08E–16 | 2.61E–14 | 2.79E–16 | ⋯ | ⋯ |
11 | AU Mic | 8.78E–14 | 3.45E–16 | 1.07E–11 | 4.00E–13 | 1.09E–14 | 8.97E–17 | 1.44E–13 | 1.81E–16 | 4.20E–12c | 4.20E–13c |
12 | YZ CMi | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | 1.10E–12 | 1.42E–15 |
13 | GJ 821 | 5.58E–16 | 6.56E–16 | ⋯ | ⋯ | 9.52E–17 | 9.52E–18 | 1.05E–16 | 2.89E–17 | 2.62E–14 | 2.69E–15 |
14 | GJ 213 | ⋯ | ⋯ | ⋯ | ⋯ | 1.62E–16 | 1.62E–17 | 2.32E–16 | 2.32E–17 | 7.13E–15 | 2.30E–15 |
15 | GJ 1132a | ⋯ | ⋯ | 2.64E–14 | 1.62E–14 | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ |
No. | Star | Si iv | He ii | C iv | N v | EUVe | ||||
---|---|---|---|---|---|---|---|---|---|---|
1 | GJ 832a | 3.33E–15 | 9.19E–17 | 6.81E–15 | 2.93E–16 | 7.64E–15 | 2.88E–16 | 3.51E–15 | 7.54E–17 | 8.65E–13 |
2 | GJ 876a | 8.44E–15 | 1.36E–16 | 5.51E–15 | 2.92E–16 | 2.29E–14 | 4.34E–16 | 1.07E–14 | 1.26E–16 | 3.43E–13 |
3 | GJ 581a | 4.44E–16 | 6.71E–17 | 7.22E–16 | 1.90E–16 | 1.84E–15 | 1.84E–16 | 5.34E–16 | 4.48E–17 | 1.01E–13 |
4 | GJ 176a | 2.30E–15 | 8.64E–17 | 6.73E–15 | 3.03E–16 | 1.23E–14 | 2.83E–16 | 3.10E–15 | 7.56E–17 | 3.57E–13 |
5 | GJ 436a | 6.81E–16 | 6.92E–17 | 1.50E–15 | 2.13E–16 | 2.39E–15 | 1.76E–16 | 9.56E–16 | 5.04E–17 | 1.90E–13 |
6 | GJ 667Ca | 8.25E–16 | 7.17E–17 | 1.94E–15 | 2.25E–16 | 2.97E–15 | 2.05E–16 | 7.16E–16 | 5.31E–17 | 4.73E–13 |
7 | GJ 1214a | 4.79E–17 | 3.74E–17 | 7.43E–17 | 1.44E–16 | 5.23E–16 | 1.21E–16 | 1.84E–16 | 3.58E–17 | 1.29E–14 |
8 | AD Leo | 1.74E–13 | 5.39E–16 | 3.02E–13 | 9.45E–16 | 5.66E–13 | 1.21E–15 | 1.41E–13 | 5.89E–16 | 8.16E–12 |
9 | EV Lac | 1.82E–14 | 9.76E–16 | 7.41E–14 | 1.58E–15 | 1.41E–13 | 1.96E–15 | 3.91E–14 | 9.03E–16 | 2.60E–12 |
10 | Proxima Cena | 2.72E–14 | 3.83E–16 | 3.08E–14 | 5.87E–16 | 1.38E–13 | 9.13E–16 | 4.00E–14 | 4.56E–16 | 3.86E–12 |
11 | AU Mic | 9.53E–14 | 1.63E–16 | 2.75E–13 | 3.50E–16 | 3.55E–13 | 3.85E–16 | 7.42E–14 | 1.82E–16 | 1.42E–11 |
12 | YZ CMi | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ |
13 | GJ 821 | 8.16E–17 | 4.29E–17 | 6.84E–16 | 2.53E–16 | 6.69E–16 | 1.90E–16 | 1.95E–16 | 1.95E–17 | ⋯ |
14 | GJ 213 | 2.13E–16 | 2.13E–17 | 2.57E–16 | 2.57E–17 | 5.22E–16 | 1.55E–16 | 3.58E–16 | 3.58E–17 | ⋯ |
15 | GJ 1132a | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | ⋯ | 2.31E–14 |
Notes. All emission-line fluxes are as observed from Earth (erg cm−2 s−1). All flux measurements for stars 1–7 come from Youngblood et al. (2016) and France et al. (2016). The Lyα reconstructed flux for AU Mic also comes from Youngblood et al. (2016). All other measurements are from this work, except where noted.
aStars with known exoplanets. bReconstructed Lyα fluxes. Asymmetric error bars from Youngblood et al. (2016) have been averaged. cWood et al. (2005b). eCalculated using the reconstructed Lyα fluxes (Table 3) and scaling relations from Linsky et al. (2014), which have been re-shown in Table 6.A machine-readable version of the table is available.
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2.2.1. Interstellar Medium Corrections
Five out of nine of our UV emission lines (Lyα, Mg ii, C ii, Si ii, and Si iii) are affected by absorption from the interstellar medium (ISM), and here we describe our attempts to mitigate the effect of ISM absorption on our measurements. All the reported Lyα fluxes have been reconstructed from the wings of the observed line profile using the technique described in Youngblood et al. (2016) or Wood et al. (2005b) for EV Lac. The Mg ii fluxes were corrected uniformly for a 30% ISM absorption, assuming a typical log10 N(Mg ii) ∼ 13 for stars within 20 pc (Redfield & Linsky 2002). Many of the Mg ii observations are not sufficiently resolved to allow for a profile reconstruction, and we do not apply a correction factor scaling either with distance or H i column densities measured along the line of sight, because the Mg+ abundance varies in the local ISM. C ii λ1334 is the most significantly impacted of the C ii λλ1334, 1335 doublet, and so we excluded its contribution from the reported C ii fluxes.
We do not apply ISM corrections to the Si ii (see Redfield & Linsky 2004, for a discussion of Si ii absorption in the local ISM) or Si iii fluxes, noting that the ISM's effect on Si iii is likely small. The intrinsic narrowness of the M dwarf emission lines may mean that for some sightlines, the ISM absorption coincides with the stellar emission line, but for others the ISM absorption is shifted away from the emission, and the line's flux is not attenuated. Ca+ from the ISM can significantly attenuate Ca ii H and K, but only for distant stars (d > 100 pc; Fossati et al. 2017). Because all of our targets are within 15 pc, Ca ii ISM absorption is likely negligible, and we do not apply a correction.
2.3. Solar X-Ray, UV, and Proton Data
We utilize time-series solar irradiance (disk-integrated) measurements from the Extreme ultraviolet Variability Experiment (EVE) suite of instruments on board the Solar Dynamics Observatory (SDO; Woods et al. 2012). We use the He ii (304 Å) irradiance from the 2010–2014 era from the MEGS-A channel (50–370 Å with 1 Å spectral resolution). MEGS-A operates at a 10 s cadence, but we use 1-minute averages in this work to reduce noise.
Time-series solar SXR irradiance measurements and in situ proton measurements come from the Geostationary Operational Environmental Satellite (GOES) system.27 SXRs are measured in a 1–8 Å (1.5–12.4 keV) band. Note that we do not divide the GOES 1–8 Å flux by 0.7, the recommended correction factor, to obtain absolute flux units. This is because we utilize the GOES SXR flare classification scheme below, which operates on data that have not been corrected, and recent SXR observations with the MinXSS cubesat suggest that this correction factor is incorrect (Woods et al. 2017). We utilize the proton measurements from the >10 MeV and >30 MeV channels.
3. Ca ii K Equivalent Widths
To isolate the chromospheric Ca ii K emission line so we can compare it to the UV emission line fluxes, we must correct for the absorption by subtracting a radiative equilibrium model. This is particularly important for the low-resolution spectra, which typically cannot resolve the emission cores. Only the CASLEO/REOSC spectra are flux calibrated, so to be consistent with the rest of the spectra, we normalized the flux in the isolated Ca ii K emission core to nearby continuum, making this measurement akin to an equivalent width. Busà et al. (2007), Marsden et al. (2009), and Walkowicz & Hawley (2009) used this "residual" equivalent width technique in their analyses of Ca ii lines. Note that we do not use the widely used S-index (Vaughan et al. 1978; Wilson 1978) or index (e.g., Noyes et al. 1984), because for our medium-resolution spectra the emission line is blended with the Ca ii H emission core line.
The residual equivalent width is given by
is the observed Ca ii K profile, is the radiative equilibrium PHOENIX model (Husser et al. 2013) scaled to in the Ca ii K absorption wings, and are the interactively chosen bounds of integration around the narrow chromospheric Ca ii K emission, and is the average observed flux in the continuum region (before subtraction of the PHOENIX model) from 3937 to 3940 Å. We selected the 3937–3940 Å region for continuum normalization because it is close to the Ca ii K line (3933 Å), and the spectral response curves of the various CCDs we are using are unlikely to vary significantly over ∼7 Å. Walkowicz & Hawley (2009) and Rauscher & Marcy (2006) normalize their effective equivalent widths using continuum regions 3952.8–3956.0 Å and 3974.8–3976.0 Å. We do not believe that there is a significant difference between these continuum choices, because neither are truly continuum, due to the high density of absorption lines in this spectral region.
The PHOENIX models were retrieved from the Husser et al. (2013) grid using literature values for (Table 2) and assuming log and [Fe/H] = 0 (solar). However, for the seven MUSCLES targets, we use the PHOENIX models incorporated into the high-level science products available on MAST. See Loyd et al. (2016) for details about the parameters used to retrieve these models. The PHOENIX models have resolution R = 500,000 around Ca ii K (Husser et al. 2013) and were convolved with a Gaussian kernel to match the resolution of the spectra from the various instruments used (Section 2). The PHOENIX models were also shifted in velocity space to the rest frame of each target before fitting. We scaled the PHOENIX spectra to match three points in the broad Ca ii K absorption wings.
The M dwarfs in our sample have a broad range of effective temperatures, so we must account for a dependence on spectral type in this residual equivalent width measurement (see Appendix A for more details on the following description). Stars of earlier spectral type have brighter continuum fluxes than later-type stars, affecting the normalization of the emission core's flux. Walkowicz & Hawley (2009) restricted their Ca ii analysis to a single spectral subtype (M3 V) to avoid the issue of a spectral type dependence. To correct the residual equivalent widths ( from Equation (1)) for spectral type dependence, we normalized to the value for a reference star parameterized by K, log g = 5, and [Fe/H] = 0. The normalization or "correction" factor is the ratio of the star's average continuum flux and the reference star's average continuum flux. Both continuum averages come from the PHOENIX models. The corrected residual equivalent width is given by
Here x(T) is the average continuum flux value from 3936.9 to 3939.9 Å from a PHOENIX model for a star with temperature T, and x(3680 K) is the PHOENIX model's average continuum flux value for the reference star. The reference star's effective temperature corresponds to GJ 176 and was chosen arbitrarily. To find the continuum values, x(T), we used a grid of PHOENIX models from K to K, all with log10 g = 5 and [Fe/H] = 0 (solar). We fit a cubic spline function to the average flux values in the 3936.9–3939.9 Å region to determine the correction factor x(T)/ (Table 4, Figure 1). The uncertainty in introduced by the correction factor has two roughly equivalent sources: the uncertainty in and the assumption of log10 g = 5 and [Fe/H] = 0 for all our stars. Uncertainties in are likely 100–200 K, and this translates to a ∼20% uncertainty in the correction factor at the high-temperature end ( K), to ∼70% uncertainty around K, and to ∼100% uncertainty at the low-temperature end ( K). The surface gravity of our M dwarf sample ranges from ∼4.75 to 5.0, and given the coarseness of the PHOENIX grids, log10 g = 5 is a good assumption. The metallicity ranges from −0.5 to 0.5, but [Fe/H] = 0 is valid for most of the M dwarfs in our sample. Examining the average flux values in the 3936.9–3939.9 Å region for PHOENIX models sampling a range of surface gravity and metallicity values, we find that the dispersion in x(T)/x(3680 K) values for a given temperature is of similar magnitude to the dispersion in x(T)/x(3680 K) values (assuming log10 g = 5 and [Fe/H] = 0) between K bins (Figure 1).
Table 4. Correction Factors for Calculating (Equation (2))
T | x(T)/x(3680 K) | T | x(T)/x(3680 K) |
---|---|---|---|
2400 | 1.1613 × 10−3 | 3300 | 0.39680 |
2500 | 2.5175 × 10−3 | 3400 | 0.53075 |
2600 | 5.6663 × 10−3 | 3500 | 0.68191 |
2700 | 1.2907 × 10−2 | 3600 | 0.85061 |
2800 | 2.9381 × 10−2 | 3700 | 1.0425 |
2900 | 5.9956 × 10−2 | 3800 | 1.2642 |
3000 | 0.11061 | 3900 | 1.5233 |
3100 | 0.18269 | 4000 | 1.8277 |
3200 | 0.27899 |
Note. To calculate the correction factors x(T)/x(3680 K), we computed x(T), the average stellar surface flux values from 3936.9 to 3939.9 Å for PHOENIX models from the Husser et al. (2013) grid for a range of temperatures T (K), all with log10 g = 5 and [Fe/H] = 0 (solar). From a cubic spline fit to the x(T) values, we find x(3680 K) = 7.7453 × 1012 erg cm−2 s−1 cm−1.
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We also examined the effect of PHOENIX model parameters on during the model subtraction and the effect of interactively choosing the integration limits. Using a single Keck/HIRES spectrum and three PHOENIX model spectra, we measured 30 times and compared to the "true" measurement for that spectrum and its photometric error bar (the true measurements are shown in Figure 2 and used to calculate the equivalent width values reported in Table 2). We find that the PHOENIX model chosen for subtraction has a negligible effect on the equivalent width measurements, but that the uncertainty introduced from differences in the interactively chosen integration bounds is slightly larger than the photometric uncertainty. We do not correct the photometric error bars on the individual equivalent width measurements, and the error bars reported in Table 2 come from the dispersion in the many equivalent width measurements made for each target (described fully in Section 4.1).
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Standard image High-resolution image4. UV–Ca ii Relation
In this section we present scaling relations between Ca ii K and far- and near-UV emission lines, as well as the total EUV flux (100–912 Å). See Appendix B for a presentation of scaling relations between the far- and near-UV emission lines themselves.
4.1. Ca ii K Variability
A total of 10 out of 15 members of our M dwarf sample have tens to hundreds of archival Ca ii K observations, and we derived our equivalent width measurements from all the spectra to avoid biases from stellar activity on all timescales (i.e., flares, rotation, stellar magnetic activity cycle). Equivalent width light curves are shown in Figure 2 for the 15 stars. Variability is observed, especially over the course of a few days, but no definitive signs of cyclic activity due to stellar rotation or the stellar dynamo are observed, nor are they ruled out. Approximately 20% spreads in the Ca ii K equivalent widths are typically observed over the course of a few days (see Figures 3 and 4) and are likely due to flares and rotation of starspots into and out of view. Figure 3 shows the evolution of the Ca ii K emission profile for GJ 876 over the course of 4 days and the corresponding change in the corrected Ca ii K equivalent widths.
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Standard image High-resolution imageFor each target, we computed a mean Ca ii K equivalent width with an uncertainty equal to the standard deviation of the measurements (Table 2). GJ 1132 has only one equivalent width measurement, so the photometric error bar was reported for that measurement. The averages from stars with few observations could be strongly skewed if they coincide with an unresolved episode of high activity. The targets with the fewest observations are GJ 832, GJ 1214, GJ 1132, Proxima Cen, and GJ 213 (see Section 2 and Table 2 for the list of sources for our optical spectra).
Figure 4 shows the demographics of our sample (stellar rotation period and effective temperature ) compared to the corrected Ca ii K equivalent widths and the observed scatter in those values. In general, the fast rotators ( days) have the largest equivalent widths. Unsurprisingly, these stars are the well-known flare stars AD Leo, EV Lac, AU Mic, and YZ CMi, and they are also the youngest stars (<1 Gyr) in the sample. Between Prot ∼ 40 and 85 days, most stars exhibit small equivalent widths, but Proxima Cen (star 10) and GJ 176 (star 4) are outliers. West et al. (2015) find that late M dwarfs (M5–M8) rotating faster than 86 days and early M dwarfs (M0–M4) rotating faster than 26 days exhibit greater optical activity (i.e., an Hα emission spectrum and greater Ca ii equivalent width; Walkowicz & Hawley 2009). Proxima Cen meets this optical activity criterion, but GJ 176 does not. However, even the "optically inactive" stars (Hα absorption spectrum) in our sample exhibit UV activity.
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Standard image High-resolution imageThe right panel of Figure 4 shows the scatter observed in the Ca ii K light curves normalized to . The scatter ranges from ∼10% to 25% (although Proxima Cen's scatter is 43%), with no clear dependence on and a possible positive correlation with , although our sample is sparse for K and > 60 days.
4.2. UV–Optical Correlations
For our 15 M dwarf sample, we compare the average Ca ii K corrected equivalent widths () reported in Table 2 with UV emission line surface fluxes. By using the corrected Ca ii K equivalent width (Section 3) and UV surface fluxes, we attempt to minimize spectral type dependences in our results. We note, however, that the uncertainties in the stellar radii (used to compute the stellar surface flux) are large, and there may be a systematic bias for the lowest-mass stars. Direct interferometric measurements yield vastly different radii for mid-M dwarfs of similar effective temperatures; in particular, directly measured radii are tens of percent larger than radii determined by indirect means (von Braun et al. 2014). The nine UV lines we used for comparison are listed with their formation temperatures in Table 5.
Table 5. Fit Parameters for UV Surface Flux and Ca ii K Equivalent Width Relations
Transition Name | Wavelength (Å) | log a | α | β | ρ | n | σ |
---|---|---|---|---|---|---|---|
Si iii | 1206.50 | 4.7 | 1.35 ± 0.26 | 3.21 ± 0.16 | 0.80 | 2.0 × 10−3 | 0.59 |
H i Lyα | 1215.67 | 4.5 (line core) | 0.88 ± 0.10 | 5.46 ± 0.06 | 0.95 | 1.1 × 10−5 | 0.18 |
"active" | 1.21 ± 0.16 | 5.20 ± 0.12 | ⋯ | ⋯ | ⋯ | ||
"inactive" | 0.10 ± 0.17 | 5.19 ± 0.08 | ⋯ | ⋯ | ⋯ | ||
Si ii | 1260.42, 1264.74, 1265.00 | 4.5 | 0.99 ± 0.18 | 2.58 ± 0.11 | 0.82 | 6.7 × 10−4 | 0.42 |
C ii b | 1335.71 | 4.5 | 1.29 ± 0.23 | 3.38 ± 0.14 | 0.82 | 6.0 × 10−4 | 0.54 |
Mg ii c | 2796.35, 2803.53 | 4.5 (line core) | 1.06 ± 0.13 | 4.88 ± 0.08 | 0.94 | 7.1 × 10−6 | 0.27 |
Si iv | 1393.76, 1402.77 | 4.9 | 1.35 ± 0.24 | 3.22 ± 0.14 | 0.84 | 3.6 × 10−4 | 0.54 |
He ii | 1640.4d | 4.9 | 1.33 ± 0.15 | 3.53 ± 0.09 | 0.91 | 1.2 × 10−5 | 0.41 |
C iv | 1548.19, 1550.78 | 5.0 | 1.31 ± 0.26 | 3.84 ± 0.16 | 0.81 | 8.8 × 10−4 | 0.56 |
N v | 1238.82, 1242.8060 | 5.2 | 1.2 ± 0.26 | 3.36 ± 0.15 | 0.77 | 1.9 × 10−3 | 0.55 |
EUVe | 100–912 | ⋯ | 0.80 ± 0.09 | 5.49 ± 0.06 | 0.94 | 1.5 × 10−5 | 0.18 |
"active" | 1.37 ± 0.18 | 5.10 ± 0.14 | ⋯ | ⋯ | ⋯ | ||
"inactive" | 0.12 ± 0.18 | 5.15 ± 0.08 | ⋯ | ⋯ | ⋯ |
Notes. All relations have the form log10 = (α × log10 ) + β, where is the surface flux of the UV emission line in erg cm−2 s−1 and is the Ca ii K equivalent width in Å. ρ is the Pearson correlation coefficient, n is the probability of no correlation, and σ is the standard deviation of the data points about the best-fit line (dex). The additional fit parameters for Lyα and EUV surface flux apply separately to the "active" () and "inactive" M dwarfs (). Combining the active and inactive fit components, σ = 0.12 for Lyα, and σ = 0.13 for the EUV.
aFormation temperatures are from the CHIANTI database (Dere et al. 1997; Landi et al. 2013). bDoes not include the 1334.54 Å line, due to significant ISM absorption. cFluxes corrected for 30% ISM absorption (see Section 2.2 and Youngblood et al. 2016). dAverage wavelength of the multiplet. eEUV fluxes calculated from Lyα fluxes using scaling relations from Linsky et al. (2014).Download table as: ASCIITypeset image
Figure 5 shows the correlations between and surface flux () for nine UV emission lines and the EUV flux, which is derived from Lyα (see Section 4.2.1), with their power-law fits of the form log10 FS,UV = (α × log10 ) + β (Table 5). We find statistically significant correlations between Ca ii K and all nine UV emission lines, which have formation temperatures ranging from 30,000 to 160,000 K. As expected, the correlations with the least scatter are for Mg ii and Lyα (0.27 and 0.18 dex, respectively), both optically thick lines with formation temperatures similar to Ca ii K. Ca ii has been previously found to correlate positively with Lyα (Linsky et al. 2013) and Mg ii (Walkowicz & Hawley 2009). Note that due to the large uncertainty in GJ 1214's Lyα flux (Youngblood et al. 2016), we do not include it in the fit, although its effect on the fit is small. GJ 1214 is an outlier from the fits for all nine UV lines, and GJ 876 is a significant outlier for all but Mg ii and Lyα. Of the seven MUSCLES M dwarfs, GJ 876 exhibited the most frequent and largest flares. These flares were observed in all lines except Mg ii and Lyα, which were observed on different HST visits from the other far-UV emission lines, so GJ 876's apparently elevated UV surface fluxes in Figure 5 may be due to these flares. There is no clear dependence on fit quality (as measured by the Pearson correlation coefficients or the standard deviation of the fit) with the formation temperature of the UV line.
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Standard image High-resolution imageBy eye, it appears that some of the Ca ii–UV correlations in Figure 5 may be better fit by two power laws with a break around , the transition in this data set between the "inactive" () and "active" () M dwarfs. In the Lyα and EUV panels in Figure 5, we show two power-law fits in addition to the single power-law fit. As with the single power-law fits, GJ 1214 is excluded. The broken power-law fits indicate that for these two UV surface fluxes, the Ca ii–UV correlations become approximately constant at low stellar activity (Table 5). Greater study of the low-activity M dwarfs is necessary to determine whether the UV fluxes become approximately constant in that regime, as the apparent flattening of many of the correlations is largely due to a single star: GJ 1214.
4.2.1. Estimating the EUV Spectrum from Ca ii K
Predicting an M dwarf's Lyα flux is important not only because Lyα constitutes a major fraction of the far-UV flux, but also because it is a means for estimating the EUV spectrum, which currently cannot be observed for any star except the Sun. In Figure 5 and Table 5, we have determined the scaling relation between the total EUV flux (100–912 Å) and for our stars. The fit is very similar to the Lyα–Ca ii K best-fit line, because the EUV fluxes were derived from scaling relations with Lyα from Linsky et al. (2014).
In Table 6, we substitute our Ca ii–Lyα scaling relation into the Lyα–EUV scaling relations in Table 5 of Linsky et al. (2014) to allow the reader to directly reconstruct the EUV spectrum from a Ca ii K measurement. We have also re-shown the scaling relations from Linsky et al. (2014) in Table 6, although they have been simplified for brevity.
Table 6. Formulae for Estimating EUV Fluxes from Lyα and Ca ii K
Flux in Wavelength | ||
---|---|---|
Band at 1 au | Linsky et al. (2014) | |
(erg cm−2 s−1) | Table 4 | This Worka |
F(100–200 Å) | · F(Lyα) | · · (4.65 × 10−3 R⋆) |
F(200–300 Å) | · F(Lyα) | · · (4.65 × 10−3 R⋆) |
F(300–400 Å) | · F(Lyα) | · · (4.65 × 10−3 R⋆) |
F(400–500 Å) | · F(Lyα) | · · (4.65 × 10−3 R⋆) |
F(500–600 Å) | · F(Lyα) | · · (4.65 × 10−3 R⋆) |
F(600–700 Å) | · F(Lyα) | · · (4.65 × 10−3 R⋆) |
F(700–800 Å) | · F(Lyα) | · · (4.65 × 10−3 R⋆) |
F(800–912 Å) | · F(Lyα) | · · (4.65 × 10−3 R⋆) |
Note. F(Lyα) is the Lyα flux at 1 au (erg cm−2 s−1), and is the Ca ii K corrected equivalent width (Equation (2)).
aSubstituted Lyα– scaling relation from Table 5 into the relation from Linsky et al. (2014); R⋆ in units of R⊙; uncertainties propagated from fit uncertainties in Table 5.Download table as: ASCIITypeset image
4.2.2. Estimating the Uncertainties on Derived UV Surface Fluxes
Here we estimate the uncertainties in the UV fluxes estimated from Ca ii K using the presented scaling relations (Tables 5 and 6). Important sources of error include the nonsimultaneity of our UV and optical observations, the uncertainties in the Ca ii K and UV measurements, the uncertainties in the stellar radii and distances (although the uncertainties in distances for these nearby stars are small) that are used to calculate surface flux, and the uncertainties in the stellar effective temperatures, surface gravities, and metallicities used to calculate the equivalent width correction factors. The error bars on the values come from the dispersion in the many equivalent width measurements made for each target (with the exception of GJ 1132, which has only one measurement), and these error bars range from ∼10% to 25%, although Proxima Cen's error bar is close to 45%.
Of the nine UV emission lines, Lyα and Mg ii have the least scatter about the best-fit line (0.18 and 0.27 dex, respectively). This is important, because these two emission lines compose the majority of the far-UV and near-UV emission line flux, respectively, for the M dwarfs. Considering F(emission line)/(nine emission lines) for the nine stars with measurements for all nine emission lines, F(Lyα)/(nine emission lines) = 65%–91% and F(Mg ii)/(nine emission lines) = 6%–27%. The other emission lines compose smaller percentages of the total emission line flux: ∼0.1%–5% each. For example, the scatter in the Si iii–Ca ii K scaling relation is the largest (σ = 0.59 dex), but F(Si iii)/(nine emission lines) = 0.09%–1.7%.
Due to the limited number of EUV observations of M dwarfs, quantifying the true uncertainty in the calculated EUV spectrum is challenging. Here we estimate the uncertainty and list all the main sources of error. Linsky et al. (2014) used EUVE observations (100–400 Å) of six M dwarfs with HST/STIS Lyα observations, including au Mic, Proxima Cen, AD Leo, EV Lac, and YZ CMi. The 400–912 Å spectra were provided by semiempirical models (Fontenla et al. 2014). Scaling relations for eight ∼100 Å bandpasses in the EUV were derived, with dispersions of 13%–24%. Linsky et al. (2014) describe three sources of uncertainty in their technique: errors in the EUV fluxes, errors in the reconstructed Lyα fluxes, and errors associated with stellar variability (the EUV and Lyα observations were not simultaneous). The observed dispersion (13%–24%) in the scaling relations is surprisingly small given the expected magnitudes of the three uncertainty sources. Linsky et al. (2014) attribute this to the avoidance of EUVE observations containing flares.
The scatter in our own Ca ii K–Lyα relationship is surprisingly small (σ = 0.18 dex) given the uncertainties listed in the first paragraph of this subsection. The error bars range from ∼10% to 30%, and Youngblood et al. (2016) find that the uncertainties in the reconstructed Lyα fluxes range from ∼5% to 20% for moderate- to high-S/N observations. GJ 1214 was the lowest-S/N observation and had a ∼100% uncertainty in the reconstructed flux, but was not included in the Ca ii K–Lyα fit.
Starting with a measurement with an assumed 30% uncertainty and using the Ca ii K–Lyα scaling relation from Table 5, we find that the propagated uncertainty in the calculated Lyα flux is unchanged, indicating that the uncertainty in the Ca ii K equivalent width dominates. Using the calculated Lyα flux to estimate the EUV spectrum and adding the 30% uncertainty in quadrature with the 24% dispersion from Linsky et al. (2014) yields an uncertainty of ∼40% for the resulting EUV flux.
We have assumed no additional uncertainty due to the variations in metallicity of our target stars. Metallicity variations likely have the largest impact on the H i Lyα–Ca ii relations, but it appears that this effect is negligible compared to other sources of scatter for our near-solar-metallicity (−0.5 ≤ [Fe/H] ≤ 0.5) target stars. The metallicity effect could become significant for metal-poor stars ([Fe/H] < −1), where the relative abundance of Ca with respect to H is approximately an order of magnitude less than for solar-metallicity stars, and we caution against applying these correlations to stars with any physical parameters beyond the bounds of our 15-star sample. The addition of metal-poor M dwarfs into the sample would allow for a determination of the effect of metallicity on these UV–optical correlations.
5. Energetic Proton Estimation from UV Flares
HST has observed dozens of spectrally and temporally resolved far-UV flares from M dwarfs (Loyd & France 2014; France et al. 2016; R. O. P. Loyd et al. 2017, in preparation), which can be used to constrain the time-dependent energy input into the upper atmospheres of orbiting exoplanets. Energetic particles from stellar eruptive events are not frequently included in these energy budgets, because there are no observational constraints for stars other than the Sun. Existing solar correlations between SXRs and protons detected near Earth (i.e., Belov et al. 2007; Cliver et al. 2012) cannot be directly applied to HST's UV flares, because we do not know the energy partition between stellar UV emission lines and SXRs during flares. Thus, we have developed a new scaling relation between energetic protons detected near Earth and UV flares from the Sun.
Ideally, we would determine the relationship between energetic protons detected by the GOES satellites and far-UV spectra of the Sun, because this would be directly comparable to the flares detected by HST. However, there are no disk-integrated, high-cadence solar observations of UV emission lines within HST's STIS or COS nominal far-UV spectral ranges (1150–1700 Å). We elected to use an EUV emission line from high-cadence solar irradiance measurements as a proxy for far-UV emission lines. SDO/EVE measured the solar spectral irradiance of the Sun from 50 to 370 Å in the MEGS-A channel at 10 s cadence from 2010 to 2014. The only high-S/N ion with a formation temperature similar to those accessible by HST STIS/COS in the far-UV is He ii at 304 Å (log ; CHIANTI; Dere et al. 1997; Landi et al. 2013). The far-UV flare tracers Si iv (1393, 1402 Å; log ) and He ii (1640 Å; log ) observed by HST have similar formation temperatures to He ii λ304. After determining the relationship between >10 MeV proton flux and He ii λ304, we use the semiempirical model of GJ 832 (M1.5 V; Fontenla et al. 2016) to scale He ii λ304 flux to Si iv and He ii λ1640 flux. In Section 5.4, we estimate the proton flux from an Si iv flare observed with HST from the M4 dwarf GJ 876, and in Section 5.5, we discuss the limitations of applying these proton scaling relationships to flares on M dwarfs.
5.1. The Solar Flare and Proton Enhancement Sample
We identified 36 proton enhancements in the GOES >10 MeV and >30 MeV proton channels with an associated SXR (1–8 Å with GOES) and He ii λ304 flare. Our confidence levels for the proton–flare association varied, and we assigned each event a quality index (q) ranging from 1 (lowest confidence) to 4 (highest confidence). The number of events assigned to q = 1, 2, 3, and 4 is 7, 11, 7, and 11, respectively. Reasons for a low q include difficulty in identifying a proton enhancement's precursor flare and/or reliably measuring the properties of both fluxes. There can be too many candidate precursor flares, low S/N, difficulty in defining the beginning and end of the proton and flare events, and uncertainty in measuring background flux level. Figure 6 shows an example high-confidence event (q = 4) and a low-confidence event (q = 1). For the q = 1 example event, the onset of the >10 MeV protons after the photon flares is much more gradual than most events, and the >30 MeV proton flux shows no significant rise. The He ii λ304 light curve also shows many events, which may be confused, and estimation of the background level is challenging.
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Standard image High-resolution imageWe find that the proton, UV, and SXR flux errors are dominated by systematics in defining a background flux level to subtract and the duration of the flare. We applied a linear fit to the background around each event. For some events, this was straightforward, but for others, this method likely increases uncertainty in the measurement. We determined the beginning and end of the flare by where the light curve intersected the background level fit. To estimate the uncertainties in our measurements, we remeasured 4 of the 36 events three times, each time slightly changing the background fit and the beginning and end of the flare. We estimate the uncertainty in the background-subtracted flux to range from 10% to 300% for SXR, 10%–200% for He ii λ304, and 10%–30% for the protons. These ranges are a reflection of the varying quality factors: q < 3 events have the largest uncertainties, and q ≥ 3 events have the smallest uncertainties. If we consider just the fluence (no background subtraction) or the peak fluxes, the uncertainties drop to 10% for the SXRs and He ii λ304, indicating that background subtraction and not flare duration is the dominant uncertainty.
The 36 He ii λ304 flares have mean durations 5.3 ± 4.6 hr and on average peak a few minutes after the SXR flare peak, although there is large scatter in this average. When examining only the q ≥ 3 events, the average He ii λ304 peak occurs ∼5 minutes before the SXR peak. Kennedy et al. (2013) used He ii λ304 to trace the impulsive phase flares and found He ii λ304 to peak 1–4 minutes before the SXR peak, which traces the more gradual phase of the flare, and Milligan et al. (2012) found for an X-class flare that He ii λ304 peaked 18 s before the GOES SXRs. The associated proton enhancements begin within about 2 hr of the SXR peak and on average last for 3 days. Part of the scatter in the He ii λ304–proton relationships presented in Figure 7 is due to overlapping flares with contributing protons. In the duration of a proton enhancement, the same or another active region could flare again and accelerate protons that reach Earth. Many of the >10 MeV enhancements have many peaks over the course of several days, while the >30 MeV enhancements typically only have a rapid initial peak and a gradual decline. The peak proton fluxes between the two channels generally do not coincide temporally; the >10 MeV peak particle flux typically occurs after the >30 MeV peak. The energy-dependent arrival times of protons are not completely explained by differing speeds; it is thought that higher-energy protons are accelerated with electrons close to the solar surface and that either lower-energy protons are accelerated at a later time (farther from the solar surface) or their escape from the Sun is delayed owing to trapping by shocks (Krucker & Lin 2000; Xie et al. 2016).
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Standard image High-resolution imageIn their sample of 58 SXR and proton enhancement events, Cliver et al. (2012) found a statistically significant correlation (ρ = 0.52, n = 3 × 10−5), but our 36-event sample yields ρ = 0.18, n = 0.3 (Figure 8). If we force both samples to cover the same parameter space (enclosed in the vertical lines in Figure 8), the correlation coefficients become similar: ρ = 0.41, n = 0.003 for 50 of Cliver et al. (2012) events, and ρ = 0.35, n = 0.05 for 33 of our events. The different n values are due to the different sample sizes.
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Standard image High-resolution image5.2. Solar UV–Proton Scaling Relations
We observe statistically significant correlations between He ii λ304 fluence (time-integrated flux with units J m−2) and proton fluence and peak proton flux (all fluence and flux values background subtracted; Figure 7). The data were fitted with power laws (log10 x = α × log10 y + β), and the parameters for the fits are presented in Table 7. The scatter in these fits is large (σ = 0.75–0.84 dex).
Table 7. Correlations between UV Flare Fluence (F) and the Peak Intensity (I) and Fluence (F) of Energetic Protons during Solar Flares
x | y | α | β | ρ | n | σ |
---|---|---|---|---|---|---|
1.06 ± 0.21 | 2.42 ± 0.17 | 0.83 | 2.2 × 10−5 | 0.76 | ||
0.85 ± 0.20 | 1.62 ± 0.16 | 0.80 | 6.5 × 10−5 | 0.75 | ||
1.20 ± 0.26 | 2.23 ± 0.21 | 0.84 | 1.0 × 10−5 | 0.84 | ||
1.01 ± 0.25 | 1.37 ± 0.20 | 0.82 | 3.6 × 10−5 | 0.84 | ||
1.06 ± 0.21 | 3.34 ± 0.25 | ⋯ | ⋯ | ⋯ | ||
1.20 ± 0.26 | 3.27 ± 0.31 | ⋯ | ⋯ | ⋯ | ||
1.06 ± 0.21 | 4.05 ± 0.36 | ⋯ | ⋯ | ⋯ | ||
1.20 ± 0.26 | 4.07 ± 0.45 | ⋯ | ⋯ | ⋯ |
Note. The power-law fits (log10 x = α × log10 y + β) are based on the q ≥ 3 background-subtracted data (Figure 7). ρ is the Pearson correlation coefficient, n is the probability of no correlation, and σ is the standard deviation of the data points about the best-fit line (dex).
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The near identical formation temperatures of He ii λ304, Si iv, and He ii λ1640 suggest that the ratios of their fluxes are likely to be similar for all stars with metallicities similar to solar values. Thus, we estimated these ratios using synthetic spectra of the Sun (CHIANTI; Dere et al. 1997; Landi et al. 2013) and GJ 832 (Fontenla et al. 2016). For the Sun, / and /. For GJ 832, / and /. The ratios for these two stars are very similar, so we will use the GJ 832 ratios in the subsequent analysis. However, we note that the ratios could change by a factor of a few during a flare as estimated by comparing flux ratios of various lines for the active and quiet-Sun models listed in Table 1 of Fontenla et al. (2016). More M dwarf atmosphere models calculated at a range of activity levels would be valuable.
We apply the quiescence ratios to our proton–He ii λ304 relations (Table 7) to relate Si iv and He ii λ1640 flare flux to proton enhancements. Using one of the correlations listed in Table 7 and replacing with , we find that
where is the background-subtracted Si iv (λλ1393, 1402) flare fluence (J m−2) as would be observed at 1 au from the star, and is the background-subtracted peak >10 MeV proton enhancement intensity (pfu; 1 pfu = 1 proton cm−2 s−1 sr−1) as would also be observed at 1 au. If instead the proton fluence (, [pfu · s]) rather than peak proton flux is used, the relationship becomes
Similarly, we can derive and from :
and
5.3. UV-based GOES Flare Classification
When using Equations (3)–(6), it is important to note that not all far-UV flares will be accompanied by particle events. Less energetic flares are less likely to produce particles. The solar relation was quantified by Yashiro et al. (2006) using the GOES SXR classification scheme as the metric of flare strength. Specifically, they associated a probability of a CME with each GOES flare class. To relate this to far-UV data, we used our 36 events to fit an empirical power law between peak SXR intensity and peak He ii λ304 intensity (W m−2; Figure 9):
The Pearson correlation coefficient is 0.58 with n = 2.2 × 10−4 for the 36 events used in this analysis. The scatter about the best-fit line in Figure 9 is 0.52 dex, so the resulting classifications for M dwarf flares will be accurate within a factor of a few. This level of accuracy will be problematic for small flares ( class), but less so for large flares, due to the ∼100% chance of associated proton enhancement (Table 1). Using our conversion ratio (/) and assuming //, we can estimate the peak SXR flux from the peak Si iv and He ii λ1640 flux:
and
Approximately 20% of C-class flares ( W m−2 at 1 au) and ∼100% of X3-class or greater flares (FSXR ≥ 3 × 10−4 W m−2 at 1 au) have associated CMEs (Yashiro et al. 2006; Table 1). Recall that is the peak 1–8 Å flare intensity measured at 1 au from the star and is not corrected for pre-flare flux levels. An X-class or greater flare (≥10−4 W m−2 at 1 au) corresponds to any Si iv flare with a background-subtracted peak intensity value ≥1.6 × 10−5 W m−2 = 1.6 × 10−2 erg cm−2 s−1 at 1 au and to any He ii λ1640 flare with a background-subtracted peak intensity value ≥3.2 × 10−6 W m−2 = 3.2 × 10−3 erg cm−2 s−1 at 1 au.
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Standard image High-resolution image5.4. Application to Observed Flares from GJ 876
The MUSCLES Treasury Survey observed several large flares from GJ 876 (d = 4.7 pc) with HST and Chandra in 2015 June and July (France et al. 2016; R. O. P. Loyd et al. 2017, in preparation; Figure 10). Due to an HST safing event, the Chandra and HST observations were not simultaneous as originally planned. On 2015 June 5, the SXR luminosity of GJ 876 was observed to increase by a factor >10 (Figure 10(a)), and on 2015 July 7, factor of ∼40–100 increases were observed in the far-UV lines, including Si iv (Figure 10(b)), and more modest increases (factor of ∼5) were observed in the far-UV continuum (France et al. 2016). He ii λ1640 was observed with a different grating than Si iv, so the two emission lines were not observed simultaneously, and no clear flare was observed in He ii λ1640 on 2015 July 8 (Figure 10(c)), although the C iv light curve indicates that GJ 876 did flare during this observation. In this section and Table 8, we characterize the magnitude of these flares with the GOES flare classification scheme and estimate the probability and magnitude of an associated particle enhancement received in GJ 876's HZ ( au; Kopparapu et al. 2014). See Section 5.5 for a discussion on the limitations of these results.
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Standard image High-resolution imageTable 8. GJ 876 Flare Properties
Flare | Peak SXR Flux (W m−2) | GOES | >10 MeV Proton Flux (pfu) | ||
---|---|---|---|---|---|
1 au | Class | 1 au | |||
GJ 876 flares: | |||||
2015 Jun 4 | 2.2 × 10−5 | 6.6 × 10−4 | M2.2 | 8 | 240 |
2015 Jun 5 | 9.5 × 10−5 | 2.9 × 10−3 | M9.5 | 80 | 2400 |
2015 Jul 7 | 3.8 × 10−3 | 1.1 × 10−1 | X38 | 75 | 2300 |
Reference flares: | |||||
Carrington | 4.5 × 10−3 | ⋯ | X45 ± 5 | ⋯ | ⋯ |
Event 1859a | |||||
2003 Nov 4 | 3.06 × 10−3 | ⋯ | X30.6 | 400 | ⋯ |
solar flareb | |||||
Great AD Leo | 0.23 | 9 | X2300 | 1.5 × 106 | 5.9 × 108 |
flare of 1985c | |||||
DG CVn | 60 | 6000 | X600,000 | ⋯ | ⋯ |
2014 Apr 24d |
Note. au for GJ 876; 0.16 au for AD Leo; 0.1 au for DG CVn; 1 au for the Sun.
Reference. (a) Cliver & Dietrich (2013), (b) Kiplinger & Garcia (2004), (c) Segura et al. (2010), (d) Osten et al. (2016).
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Table 9. UV–UV Emission Line Scaling Relations
UV1, UV2 | m | b | ρ | n | σ | ||
---|---|---|---|---|---|---|---|
Lyα, Si iii | 0.60 | 0.09 | 3.66 | 0.35 | 0.89 | 6.4E–04 | 0.23 |
Si ii, Si iii | 0.82 | 0.04 | −0.11 | 0.18 | 0.97 | 2.3E–07 | 0.15 |
C ii, Si iii | 1.01 | 0.07 | 0.13 | 0.30 | 0.94 | 8.1E–06 | 0.27 |
Mg ii, Si iii | 0.79 | 0.35 | 2.26 | 1.11 | 0.84 | 2.2E–03 | 0.36 |
Si iv, Si iii | 1.01 | 0.04 | −0.01 | 0.16 | 0.92 | 1.7E–05 | 0.29 |
He ii, Si iii | 1.15 | 0.14 | −0.2 | 0.6 | 0.95 | 1.6E–06 | 0.26 |
C iv, Si iii | 1.03 | 0.04 | 0.49 | 0.19 | 0.96 | 7.5E–07 | 0.21 |
N v, Si iii | 0.87 | 0.04 | 0.52 | 0.18 | 0.96 | 1.0E–06 | 0.20 |
Si ii, Lyα | 1.16 | 0.21 | −3.83 | 1.29 | 0.87 | 1.1E–03 | 0.30 |
C ii, Lyα | 1.71 | 0.27 | −6.26 | 1.60 | 0.88 | 7.4E–04 | 0.40 |
Mg ii, Lyα | 1.38 | 0.15 | −2.68 | 0.84 | 0.96 | 1.1E–04 | 0.19 |
Si iv, Lyα | 1.71 | 0.25 | −6.27 | 1.47 | 0.90 | 4.1E–04 | 0.38 |
He ii, Lyα | 1.91 | 0.29 | −7.26 | 1.71 | 0.96 | 1.6E–05 | 0.32 |
C iv, Lyα | 1.58 | 0.19 | −4.86 | 1.15 | 0.92 | 2.0E–04 | 0.32 |
N v, Lyα | 1.43 | 0.21 | −4.58 | 1.25 | 0.88 | 9.1E–04 | 0.35 |
C ii, Si ii | 1.33 | 0.11 | −0.05 | 0.38 | 0.93 | 4.1E–06 | 0.28 |
Mg ii, Si ii | 1.57 | 0.27 | 0.54 | 0.78 | 0.86 | 6.0E–04 | 0.47 |
Si iv, Si ii | 1.31 | 0.09 | −0.12 | 0.30 | 0.92 | 1.1E–05 | 0.30 |
He ii, Si ii | 1.57 | 0.14 | −0.59 | 0.49 | 0.93 | 3.7E–06 | 0.32 |
C iv, Si ii | 1.3 | 0.08 | 0.47 | 0.28 | 0.9 | 2.4E–05 | 0.33 |
N v, Si ii | 1.18 | 0.10 | 0.23 | 0.36 | 0.92 | 1.0E–05 | 0.27 |
Mg ii, C ii | 0.75 | 0.25 | 2.23 | 0.84 | 0.83 | 1.7E–03 | 0.39 |
Si iv, C ii | 0.99 | 0.13 | −0.10 | 0.60 | 0.98 | 1.6E–09 | 0.14 |
He ii, C ii | 1.15 | 0.05 | −0.41 | 0.23 | 0.94 | 1.3E–06 | 0.30 |
C iv, C ii | 0.93 | 0.12 | 0.76 | 0.55 | 0.98 | 1.4E–08 | 0.17 |
N v, C ii | 0.79 | 0.10 | 0.74 | 0.46 | 0.98 | 3.5E–09 | 0.15 |
Si iv, Mg ii | 0.92 | 0.38 | −1.04 | 1.78 | 0.82 | 2.1E–03 | 0.44 |
He ii, Mg ii | 0.97 | 0.13 | −1.10 | 0.61 | 0.96 | 4.1E–06 | 0.23 |
C iv, Mg ii | 0.84 | 0.27 | −0.15 | 1.31 | 0.85 | 8.4E–04 | 0.39 |
N v, Mg ii | 1.27 | 0.51 | −2.73 | 2.42 | 0.80 | 3.4E–03 | 0.53 |
He ii, Si iv | 1.13 | 0.24 | −0.17 | 1.07 | 0.94 | 1.9E–06 | 0.29 |
C iv, Si iv | 0.93 | 0.06 | 0.89 | 0.26 | 0.96 | 1.1E–07 | 0.21 |
N v, Si iv | 0.84 | 0.04 | 0.59 | 0.18 | 0.97 | 5.9E–08 | 0.17 |
C iv, He ii | 0.82 | 0.16 | 1.02 | 0.80 | 0.95 | 6.3E–07 | 0.25 |
N v, He ii | 0.67 | 0.13 | 1.07 | 0.64 | 0.92 | 7.4E–06 | 0.29 |
N v, C iv | 0.85 | 0.06 | 0.08 | 0.29 | 0.99 | 4.9E–10 | 0.11 |
Note. Scaling relations are power laws of the form log10 FS, UV1 = m× log10 FS, UV2 + b, where is the surface flux in erg cm−2 s−1, ρ is the Pearson correlation coefficient, n is the probability of no correlation, and σ is the standard deviation of the data points about the best-fit line (dex).
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Table 10. UV Emission Line Scaling Relations with Stellar Rotation Period
UV | m | b | ρ | n | σ | ||
---|---|---|---|---|---|---|---|
Si iii | −1.40 | 0.29 | 5.37 | 0.44 | −0.86 | 7.3E–04 | 0.44 |
Lyα | −0.92 | 0.22 | 6.97 | 0.31 | −0.86 | 7.5E–04 | 0.29 |
Si ii | −0.85 | 0.13 | 3.93 | 0.18 | −0.88 | 3.8E–04 | 0.28 |
C ii | −1.37 | 0.29 | 5.49 | 0.44 | −0.86 | 8.0E–04 | 0.44 |
Mg ii | −1.18 | 0.15 | 6.52 | 0.23 | −0.95 | 3.0E–05 | 0.25 |
Si iv | −1.32 | 0.30 | 5.31 | 0.45 | −0.84 | 1.1E–03 | 0.43 |
He ii | −1.26 | 0.19 | 5.52 | 0.27 | −0.93 | 4.5E–05 | 0.30 |
C iv | −1.40 | 0.32 | 6.03 | 0.49 | −0.82 | 1.9E–03 | 0.49 |
N v | −1.31 | 0.32 | 5.38 | 0.48 | −0.81 | 2.5E–03 | 0.47 |
Note. Scaling relations are power laws of the form log10 FS, UV = m;× log10 Prot + b, where is the surface flux in erg cm−2 s−1 and is the rotation period in days, ρ is the Pearson correlation coefficient, n is the probability of no correlation, and σ is the standard deviation of the data points about the best-fit line (dex).
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Table 1 provides comparison points for solar flares, and in Table 8 we note the GOES classification and other parameters for well-known solar and stellar flares to give context for the GJ 876 flares. The Carrington event of 1859, arguably the largest solar flare ever recorded, has been calculated to be an X45 (±5) class flare (Cliver & Dietrich 2013). The November 4 solar flare of the Halloween storms in 2003, probably the largest flare observed during the space age, is estimated to be an X30.6-class flare (Kiplinger & Garcia 2004; note that the GOES detectors saturate for events between X10 and X20). For the great AD Leo flare of 1985 (Hawley & Pettersen 1991), Segura et al. (2010) estimated that an HZ planet ( au) would have received peak >10 MeV proton and SXR fluxes of 5.9 × 108 pfu and 9 W m−2, respectively. The peak SXR flux at 1 au (0.23 W m−2) would make this an X2300-class flare. Osten et al. (2016) found that the superflare observed from the young M dwarf binary system DG CVn was equivalent to an X600,000-class flare (60 W m−2 at 1 au, or 6000 W m−2 at 0.1 au, the approximate HZ distance). We note, however, that there is evidence that SXR–proton scaling relations should break down for such large events (>X10-class; Hudson 2007; Drake et al. 2013).
We measure the peak flux for the large GJ 876 SXR flare observed at ∼45 ks in Figure 10(a) to be (9.72 ±1.28) × 10−13 erg cm−2 s−1 in the 0.3–10 keV bandpass (1.25–41 Å). A total of 11% ± 1.3% of the flare flux was emitted at energies 1.5–10 keV (1.25–8 Å), similar to the GOES long channel (1–8 Å), so we find that this flare is equivalent to an M9.5-class flare (error range: M7.8–X1.1; Table 1). X1-class flares have an 80%–100% chance of associated energetic particles from the Sun (Yashiro et al. 2006), with an estimated peak proton flux of ∼80 pfu at 1 au (Cliver et al. 2012). The SXR and proton fluxes received in GJ 876's HZ will be ∼30 × larger: 2.8 × 10−3 W m−2 and 2400 pfu, respectively. Veronig et al. (2002) find that the Sun emits X-class flares roughly every month, but flares that unleash SXR fluxes of 10−3 W m−2 on Earth occur only approximately once every 5 yr.
The smaller GJ 876 SXR flare observed at ∼7 ks in Figure 10(a) is estimated to be equivalent to an M2.2-class flare (Table 1). This smaller flare has a 40%–80% chance of associated energetic particles (Yashiro et al. 2006) with an estimated peak proton flux of ∼8 pfu at 1 au. M-class flares are emitted by the Sun about every other day (Veronig et al. 2002), but flares that are a factor of 30 larger in SXR and proton fluxes, as would be experienced in GJ 876's HZ, occur only a few times per year.
GJ 876's 1031 erg UV flare (Δλ = 400–1700 Å) observed on 2015 July 7 with HST (France et al. 2016) emitted 1.2 × 1029 erg in the Si iv emission line over ∼25 minutes (Figure 10(b)). Using Equation (3) and the fluence at 1 au, we find that the peak proton flux received at 1 au during the flare was ∼75 pfu, or ∼2300 pfu at 0.18 au. Using the SXR–UV scaling relation (Equation (8)) and the observed Si iv flare peak, we find that this flare was X38-class with an estimated error of a factor of ∼3 (X13–X114). Note that the peak proton flux calculated for this 2015 July 7 Si iv flare (∼2300 pfu at 0.18 au) is similar to the peak proton flux calculated for the 2015 June 5 SXR flare (∼2400 pfu at 0.18 au), but that the GOES classifications are different: M9.5 compared to X38, or a factor of 40 difference in SXR flux.
In total, Chandra observed three M- to X-class flares in 8.25 hr, and HST observed six comparable flares (within an order of magnitude) in 12.35 hr, including observations from the MUSCLES pilot survey (France et al. 2013). Thus, we estimate that GJ 876 emits flares of this magnitude at a rate of ∼0.4–0.5 hr−1. From Veronig et al. (2002), the Sun's rate of M-class flares is ∼0.02 hr−1, a factor of ∼20 less frequent than GJ 876. However, note that these M-class flares are effectively 30× stronger (i.e., X10-class) in GJ 876's HZ at 0.18 au. The Sun emits X10-class flares approximately once every 5 yr, so planets in the GJ 876 HZ are receiving SXR flare fluxes ≥10−3 W m−2 associated with proton fluxes ∼103 pfu about four orders of magnitude more frequently than Earth.
In Figure 11, we show the effect of frequent X-class flares with associated proton enhancements on the O3 column depth in an Earth-like atmosphere with no magnetosphere (Segura et al. 2010; M. A. Tilley et al. 2017, in preparation). For comparison to the M- to X-class GJ 876 flares analyzed in this section, we show the dramatic responses of O3 after the great AD Leo flare (Segura et al. 2010) and the Carrington event (see Table 8). To represent the GJ 876 flares discussed in this section, we scaled the SED of the great AD Leo flare (Hawley & Pettersen 1991) down in intensity and duration to match flares of the dM4e star GJ 1243 (Hawley et al. 2014). This resulted in ∼X1-class flares with ∼4-minute durations. Peak proton fluxes were assigned as 1.2 × 103 pfu (a typical value for the flares discussed in this section), and we provide two cases distinguished by their flare frequency: 0.08 hr−1 (Case A) and 0.5 hr−1 (Case B; similar to GJ 876's observed flare frequency). Both the Case A and Case B flares turn off after a period of 40 months, but via extrapolation, we show that for Case A, the O3 column approaches near-complete depletion at approximately 1013 s (318 kyr) of similar, constant stellar activity. Case B shows near-complete O3 depletion after only approximately 5 × 109 s (160 yr). Given the several-gigayear period of high activity during the evolution of early to mid-M dwarfs, both scenarios indicate massive, and likely complete, O3 depletion. This suggests that planetary surfaces in the HZ would be bathed in stellar UV flux. A detailed analysis of atmospheric effects will be presented in the upcoming work by M. A. Tilley et al. (2017, in preparation).
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Standard image High-resolution image5.5. Limitations of the Method
Our new method of proton flux estimation due to stellar flares has important limitations, but it will be useful until advancements are made in the indirect detection of particles from stellar eruptive events (e.g., coronal dimming or Type II or III radio bursts; Crosley et al. 2016; Harra et al. 2016) or in our understanding of particle acceleration under kilogauss magnetic field strengths. The scaling relations are statistical and are relatively inaccurate for individual flares.
The first caveat to the method is that we are necessarily assuming that particle acceleration in M dwarf atmospheres is similar to that in the Sun. This could be a poor assumption as M dwarfs have different atmospheric structure and stronger surface magnetic fields. Magnetic processes are ultimately responsible for flares and particle acceleration. Also, fast-rotating M dwarfs have extremely large surface magnetic fields with photospheres possibly saturated with active regions. Overlying magnetic fields could prevent the acceleration of particles away from the stellar atmosphere (e.g., Vidotto et al. 2016). This phenomenon was observed on the Sun in 2014 October when the large active region 2192 emitted many X-class flares, which have a >90% probability of an associated CME, but no CMEs were ejected. Strong overlying magnetic fields were observed and have been cited as a possible explanation for the lack of associated CMEs (Sun et al. 2015; Thalmann et al. 2015).
We should be careful when extrapolating solar-based SXR–particle scaling relations to large energies. There is evidence for a break in the SXR–proton power law around X10-class flares (see Lingenfelter & Hudson 1980; Hudson 2007, and references therein). It is unclear whether only the expected proton flux flattens out for increasingly large SXR flares (>X10), or whether the frequency of >X10-class flares also breaks from the expected power-law frequency distribution (e.g., Veronig et al. 2002). This uncertainty is partly due to the rarity of these energetic events, but also because the GOES SXR detectors saturate around 10−3 W m−2. Drake et al. (2013) find that extrapolating SXR–CME scaling relations to energies applicable to highly active solar-type stars would require CMEs to account for ∼10% of the total stellar luminosity, a likely unreasonable fraction. Those authors conclude that the SXR–CME scaling relations must flatten out at some point.
Predicting proton flux even for the Sun is not an easy feat, because the mechanisms of particle acceleration are not well understood. SXRs and UV photons during flares correlate with particle flux, and Kahler (1982) proposes that such correlations are manifestations of "Big Flare Syndrome," which describes how the energy of an eruptive event can power numerous physical processes that are not directly linked. Thermally heated plasma (T > 80,000 K) emits short-wavelength photons that we observe as a flare, but particles are accelerated by a nonthermal process, and the ambient corona is thought to be the major contributor to CME mass (Sciambi et al. 1977; Hovestadt et al. 1981). For our purposes of estimating proton fluxes from M dwarfs and their effects on orbiting planets, a correlation between photons and particles without direct causation is valuable.
Another limitation is our use of the GJ 832 synthetic spectrum from Fontenla et al. (2016) to estimate He ii λ304 flare flux from far-UV Si iv or He ii λ1640 flare flux. The model is applicable to the quiescent star, and flux ratios between emission lines likely change during a flare. Comparing flux ratios between the active and quiet-Sun models listed in Table 1 of Fontenla et al. (2016), the ratios of emission lines formed at different temperature change by a factor of a few during a flare. In a future work, we will improve the flux ratio relations using flare atmospheres.
We chose He ii λ304 as a proxy because of its similar formation temperature to Si iv λλ1393,1402 (and He ii λ1640), but we note that the electrons responsible for the collisional excitation of He ii λ304 (40.8 eV above ground) must have significantly higher energies than the thermal electrons at = 80,000 K (kB eV) that collisionally excite Si iv (8.8 eV above ground; Jordan 1975). Higher-energy electrons could diffuse down through the transition region, as recombination/ionization timescales are much longer than dynamical timescales (e.g., Shine et al. 1975; Golding et al. 2014, 2016). Also, the He ii line fluxes receive some contribution from recombination, and this becomes more important during flares.
Another challenge in the analysis is quantifying the probability that any ejected particles will intersect the exoplanet. There are many unknowns here, including the interplanetary magnetic field topology that charged particle trajectories will follow (Parker 1958); the opening angle of the accelerated particles; the planet's cross section, which may be larger than owing to the presence of a magnetosphere; and the direction of the particle ejection with respect to the planet's orbital plane (see Kay et al. 2016). A thorough treatment of this issue is beyond the scope of this work.
6. Summary
In this paper, we have developed methods for estimating the high-energy radiation and particle environments of M dwarfs for use when direct observations are unavailable. We have empirically determined scaling relations that can be used to estimate the UV spectra of M dwarfs from optical spectra and the energetic particle flux from UV flares. The main results of this work are summarized as follows.
- 1.Time-averaged Ca ii K (3933 Å) residual equivalent width correlates positively with stellar surface flux of nine far- and near-UV emission lines, including H i Lyα (Table 5). The presented Ca ii K and UV scaling relations allow for the UV spectrum of any M dwarf to be approximated from ground-based optical spectra.
- 2.We present a scaling relation between Ca ii K equivalent width and the EUV spectrum for M dwarfs based on the Lyα–EUV scaling relations presented in Linsky et al. (2014) and the Ca ii K–Lyα scaling relation determined in this work (Table 6). We estimate that the Ca ii-based EUV fluxes are accurate within 40%.
- 3.We present a new method to estimate the energetic (>10 MeV) proton flux emitted during far-UV emission line flares (specifically Si iv λλ1394, 1402 and He ii λ1640; Table 7). The UV–proton scaling relations are derived from solar irradiance observations and in situ proton measurements near Earth.
- 4.We present methods to estimate the GOES flare classification corresponding to far-UV Si iv and He ii flares (Equations (8) and (9)). This is important for estimating the probability that any far-UV flare will have an accompanying proton enhancement. Larger solar flares have a higher probability of associated particle enhancements.
- 5.We analyze several flares observed with Chandra and Hubble from the M4 dwarf GJ 876 as part of the MUSCLES Treasury Survey and place the flare properties in context with solar flares (Section 5.4). We find that planets in GJ 876's HZ experience large, Carrington-like flares (soft X-ray flux >10−3 W m−2) and particle enhancements approximately four orders of magnitude more frequently than Earth. Flare activity at the level observed on GJ 876 is predicted to lead to complete stripping of O3 from an Earth-like planet on timescales between 102 and 105 yr.
M dwarfs are currently a prime target for exoplanet searches and characterization efforts with current and near-future technologies including JWST, but important questions have been raised about these planets' potential habitability. JWST will be able to characterize only a few M dwarf exoplanets, and we need to ensure that HZ terrestrial planets orbiting nearby M dwarfs with the maximum probability of hosting a detectable atmosphere are chosen for JWST target selection. The stellar host's UV SED and energetic particle flux are important drivers of chemistry, heating, and mass loss, but we do not have the space telescope resources for reconnaissance of every nearby M dwarf system, and energetic particles cannot be measured directly across interstellar distances. In this paper, we have provided tools to estimate UV SEDs from comparatively easy to obtain Ca ii measurements and energetic particle fluxes from observed UV and X-ray flares.
The data presented here were obtained as part of the HST Guest Observing programs #12464 and #13650, as well as the COS Science Team Guaranteed Time programs #12034 and #12035. This work was supported by NASA grants HST-GO-12464.01 and HST-GO-13650.01 to the University of Colorado at Boulder. This work is also based on data from the Chandra X-ray Observatory (ObsIDs: 17315 and 17316) and supported by CXO grant G05-16155X. Observations were also obtained with the Apache Point Observatory 3.5 m telescope, which is owned and operated by the Astrophysical Research Consortium. This research has made extensive use of the Keck Observatory Archive (KOA), which is operated by the W. M. Keck Observatory and the NASA Exoplanet Science Institute (NExScI), under contract with the National Aeronautics and Space Administration. The ESO Science Archive Facility was also used to access VLT/XSHOOTER science products. This paper includes data gathered with the 6.5 m Magellan Telescopes located at Las Campanas Observatory, Chile. A.Y. thanks Don Woodraska for assistance with the GOES and SDO/EVE data, Juan Fontenla for providing the GJ 832 synthetic spectrum, and Lauren W. Blum for helpful discussions. E.R.N. acknowledges support from an NSF Astronomy and Astrophysics Postdoctoral Fellowship under award AST-1602597, and A.S. acknowledges the support of UNAM-PAPIIT project IN109015.
Facilities: HST (COS, STIS), ARC (DIS), CXO, Keck:I (HIRES), CASLEO:JST (REOSC), VLT:Kueyen (XSHOOTER), Magellan:Clay (MIKE), SDO (EVE), GOES.
Software: IRAF, Astropy (Robitaille et al. 2013), IPython (Perez & Granger 2007), Matplotlib (Hunter 2007), Pandas (McKinney 2010), NumPy and SciPy (van der Walt et al.2011).
Appendix A: Equivalent Width Correction
The following exemplifies how a spectral type dependence is introduced in Ca ii K equivalent width measurements and how it can be removed. See Figure 12 for examples on how the PHOENIX models used in Section 3 change as a function of spectral type.
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Standard image High-resolution imageTwo stars, A and B, have different spectral types ( and ) and are observed at different distances, and , from Earth. These stars have the same Ca ii emission core surface flux (erg cm−2 s−1), , and therefore should have the same Ca ii K equivalent widths, . From flux-calibrated Ca ii spectra, we perfectly isolate the emission core from the observed line profile by fitting and subtracting a radiative equilibrium model, and we integrate over the residual Ca ii K emission, finding and for Star A and Star B, respectively.
To convert the observed fluxes into equivalent widths, we normalize to nearby continuum, which has an average surface flux x(T). Because Star A is warmer, x() > x(), and the resulting equivalent widths are not equal:
and
To correct the equivalent widths so that they are equal for Star A and Star B, we multiply by x(T) scaled to a reference value x(). The "corrected" equivalent width is given by
Figure 12 shows radiative equilibrium model spectra (PHOENIX; Husser et al. 2013) for three spectral subtypes from our sample—3100, 3300, and 3500 K. The cooler spectral subtypes have narrower Ca ii absorption, as well as fainter continuum.
Appendix B: UV–UV Correlations
Here we present scaling relations between the nine far- and near-UV emission lines presented in Tables 3 and 5, and between these UV emission lines and the stellar rotation periods presented in Table 2. See Section 2.2 for a discussion of the UV spectra, including Lyα reconstructions and other corrections made for ISM absorption. All observed fluxes have been converted to surface fluxes using the stellar radii and distances presented in Table 2.
In Figure 13, we show the positive correlations between UV surface fluxes (, ) and their power-law fits of the form log10 FS,UV1 = m × log10 FS,UV2 + b, which are also shown in Table 9. We find statistically significant correlations for all 36 combinations of the nine UV emission lines. The Pearson correlation coefficients range from 0.80 to 0.99, and the scatter about the best-fit lines ranges from 0.11 to 0.53 dex.
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Standard image High-resolution imageIn Figure 14, we present the negative correlations between stellar rotation period () and the nine UV emission lines with their power-law fits of the form log10 FS, UV1 = m× log10 Prot + b. The power-law fits are also shown in Table 10. All of the correlations are statistically significant, although our M dwarf sample is divided between two widely separated populations: days and > 39 days. Within the slowly rotating population or the fast-rotating population, most of the correlations are not statistically significant.
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Standard image High-resolution imageYoungblood et al. (2016) presented scaling relations between Lyα and Mg ii, Si iii, C iv, and for a smaller sample of M dwarfs. The shallow correlations (m < 0.15) found between Lyα and Si iii and C iv were not statistically significant and were consistent with zero, likely due to the small sample size and the small range of explored parameter space. This work's power-law exponents between Lyα and Si iii and C iv are m = 0.60 ± 0.09 and m = 0.63 ± 0.08, respectively, compared to the m = 0.07 ± 0.31 and m =0.13 ± 0.35 values found by Youngblood et al. (2016). For Lyα and Mg ii, our power-law exponent m = 0.73 ± 0.08 is consistent with the m = 0.77 ± 0.10 value from Youngblood et al. (2016), as is our exponent for the Lyα and relation: m = −0.92 ± 0.22 compared to m = −0.86 ± 0.16.
Footnotes
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The smaller flares from the MUSCLES M dwarfs show factor of flux increases, which are below the signal-to-noise ratio (S/N) threshold of GJ 1214's light curves (R. O. P. Loyd et al. 2017, in preparation).
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IRAF is distributed by the National Optical Astronomy Observatory, which is operated by the Association of Universities for Research in Astronomy, Inc., under cooperative agreement with the National Science Foundation.
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