Evidence for He i 10830 Å Absorption during the Transit of a Warm Neptune around the M-dwarf GJ 3470 with the Habitable-zone Planet Finder

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Published 2020 May 11 © 2020. The American Astronomical Society. All rights reserved.
, , Citation Joe P. Ninan et al 2020 ApJ 894 97 DOI 10.3847/1538-4357/ab8559

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0004-637X/894/2/97

Abstract

Understanding the dynamics and kinematics of outflowing atmospheres of hot and warm exoplanets is crucial to understanding the origins and evolutionary history of the exoplanets near the evaporation desert. Recently, ground-based measurements of the meta-stable helium atom's resonant absorption at 10830 Å has become a powerful probe of the base environment which is driving the outflow of exoplanet atmospheres. We report evidence for the He i 10830 Å in absorption (equivalent width ∼0.012 ± 0.002 Å) in the exosphere of a warm Neptune orbiting the M-dwarf GJ 3470, during three transits using the Habitable Zone Planet Finder near-infrared spectrograph. This marks the first reported evidence for He i 10830 Å atmospheric absorption for a planet orbiting an M-dwarf. Our detected absorption is broad and its blueshifted wing extends to −36 km s−1, the largest reported in the literature to date. We modeled the state of helium atoms in the exosphere of GJ3470b based on assumptions on the UV and X-ray flux of GJ 3470, and found our measurement of flux-weighted column density of meta-stable state helium $({N}_{\mathrm{He}{}_{3}^{2}{\rm{S}}}=2.4\times {10}^{10}\,{\mathrm{cm}}^{-2})$, derived from our transit observations, to be consistent with the model, within its uncertainties. The methodology developed here will be useful to study and constrain the atmospheric outflow models of other exoplanets like GJ 3470b, which are near the edge of the evaporation desert.

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1. Introduction

The conventional probe for escaping atmospheres has been the Lyα absorption from the ionized exosphere during a planetary transit. This technique has produced exosphere discoveries around hot Jupiters, and hot and warm Neptunes, e.g., HD 209458b (Vidal-Madjar et al. 2003), GJ 436b (Kulow et al. 2014), and GJ 3470b (Bourrier et al. 2018). Ehrenreich et al. (2015) mapped an extended comet-like trail of escaping atmosphere from GJ 436b using the absorption signatures in the blue wings of Lyα. Bourrier et al. (2018) performed a similar analysis for GJ 3470b using Lyα observations from the Hubble Space Telescope (HST) and detected an extended exosphere with neutral hydrogen around GJ 3470b.

While Lyα is a powerful probe of evaporating atmospheres, it has two major drawbacks. The extinction loss due to interstellar absorption of Lyα, as well as the contamination from geocoronal emission, render the central core of the Lyα line unusable. This implies one can probe only the high velocity regions of the exospheres via fitting the wings of the Lyα line. The UV observations also have to be done from space—above the Earth's atmosphere—rendering them expensive and hard to do for a large number of systems.

Oklopčić & Hirata (2018) recently suggested the absorption lines of a metastable state of helium at 10830 Å as an alternative probe of evaporating exoplanet atmospheres. He i 10830 Å lines are not affected by the interstellar medium, and are observable from the ground using high-resolution near-infrared spectrographs. Since the core of the line is accessible, even the low velocity base regions of the outflowing exosphere are detectable. High-resolution spectra enable us to isolate the stellar spectrum from the planet's absorption spectrum, which is modulated by the radial velocity of the planet. High resolution is also crucial for removing contamination from narrow telluric absorption lines for ground-based observations.

The search for He i 10830 Å absorption is not new. Seager & Sasselov (2000) proposed that this would be a large signature in an F9V type star, HD 209458, though a search by Moutou et al. (2003) with VLT/ISAAC did not yield a detection. Turner et al. (2016) had identified He i 10830 Å along with other lines as a potential transition for transit spectroscopy. Recently, a handful of detections were made successfully around K-star planets, namely WASP-107b (Spake et al. 2018; Allart et al. 2019), HD 189733 b (Salz et al. 2018), HAT-P-11b (Allart et al. 2018; Mansfield et al. 2018), and WASP-69b (Nortmann et al. 2018), and one G-star planet HD 209458b (Alonso-Floriano et al. 2019).

In this paper, we report the evidence for He i 10830 Å during the transit of GJ 3470b, a warm Neptune orbiting an M-dwarf star, using the Habitable-zone Planet Finder (HPF) on the 10 m Hobby–Eberly Telescope (HET) at the McDonald Observatory. Section 2 outlines our HPF observations. We discuss our He i 10830 Å results and associated modeling in Section 3, and we finally summarize our key conclusions in Section 4.

2. Observations and Data Reduction

We observed GJ 3470 at different phases of GJ 3470b's orbit using the HPF spectrograph (Mahadevan et al. 2014; Metcalf et al. 2019). HPF is a near-infrared precision radial velocity spectrograph covering the wavelength regime of 8079–12786 Å at a resolution of R∼55,000. HPF is actively temperature controlled to the mK level to enable exquisite spectral stability and precision radial velocities in the NIR (Stefansson et al. 2016). Due to the HET design (Ramsey et al. 1998; Shetrone et al. 2007), we are limited to observe for a track length of ∼1 hr per night at GJ 3470's decl. We observed three transits of GJ 3470b on 2018 November 30 UT, 2019 January 19 UT, and 2019 April 16 UT, when the transits aligned with the observable window of the HET. Out-of-transit observations were conducted on 2019 January 4 UT, 2019 January 27 UT, and 2019 April 17 UT. Three frames of 916 s integration time were taken in each of the ∼1 hr tracks during in-transit and out-transit observations. The median signal-to-noise ratio of individual spectra was ∼100 per pixel for the first transit, and ∼200 for the second and third transit. The median number of pixels per resolution element in HPF is 2.8.

Echelle spectra of GJ 3470 from HPF were reduced using our HPF spectral extraction pipeline. The pipeline first generates 2D flux images (in units of electrons per second) from the up-the-ramp H2RG readout data (Ninan et al. 2018). A formal pixel-by-pixel variance image is also generated and propagated through the pipeline. The simultaneous star, sky, and calibration fiber spectra (as well as variance estimates) are then extracted from this 2D image (Kaplan et al. 2018).

To minimize scattered light contamination, no simultaneous calibration light spectra were used during the observations. The wavelength calibration of the extracted spectra was done using custom built frequency stabilized laser comb (LFC; Metcalf et al. 2019) measurements taken throughout the night, inversely weighted by the time difference between science and LFC images following the methodology in Metcalf et al. (2019) and Stefansson et al. (2020). All of our analyses and plots are in vacuum wavelengths. The spectra are then flat corrected and deblazed.

Sky emission lines are subtracted using the simultaneous sky spectrum. This step also subtracts out the smooth background scattered light due to the proximity of the sky fiber to the star fiber image on the detector. A 7 pixel median filter smoothing was applied to the sky fiber data in regions devoid of emission lines to reduce the noise in continuum regions of the sky emission spectrum. Stellar continuum was also removed by fitting a quadratic polynomial continuum. Telluric absorption lines were corrected using an improved version of the TERRASPEC code (Bender et al. 2012), a wrapper around LBLRTM (Clough et al. 2005). A good sky emission line subtraction and telluric absorption correction was crucial since He i 10830 Å falls close to strong OH emission lines as well as water absorption lines. The residuals in the sky and telluric corrected regions are still dominated by imperfect modeling and they are significantly above the photon noise.

Due to HET's constrained pointing—resulting in short (∼1 hr long) observation windows on GJ 3470—our out-of-transit and in-transit observations are spread across multiple nights. To down-weight the region of the spectrum partially recovered from sky and telluric corrections, the variances of those regions are artificially inflated by a large factor (∼100). In doing so, this allows us to combine multiple epochs (with different barycentric shifts) weighted by the variance and obtain an average spectrum without residual artifacts from imperfect telluric and sky emission subtraction dominating.

The GJ 3470 system's parameters used in this paper are summarized in Table 1.

Table 1.  Orbital Parameters of GJ 3470b Used in the Calculation

Parameter Value Description References
γ 26.090 Absolute stellar RV ($\,\mathrm{km}\ {{\rm{s}}}^{-1}$) Gaia Collaboration et al. (2018)
${T}_{\mathrm{eff}}$ 3600 Stellar effective temperature (K) Awiphan et al. (2016)
$[\mathrm{Fe}/{\rm{H}}]$ 0.20 Stellar metallicity Awiphan et al. (2016)
$\mathrm{log}g$ 4.695 Stellar surface gravity Awiphan et al. (2016)
M* 0.51 ± 0.06 Stellar mass (${M}_{\odot }$) Biddle et al. (2014)
R* 0.48 ± 0.04 Stellar radius (${R}_{\odot }$) Biddle et al. (2014)
T0 2456677.727712 ± 0.00022 Transit midpoint (BJDTDB) Dragomir et al. (2015)
T14 0.07992 ± 0.001 Transit duration (days) Dragomir et al. (2015)
P 3.3366413 ± 0.0000060 Period (days) Dragomir et al. (2015)
e 0.114 ± 0.052 Eccentricity Kosiarek et al. (2019)
ω −1.44${}_{-0.04}^{+0.1}$ Argument of periastron (rad) Kosiarek et al. (2019)
K ${8.21}_{-0.46}^{+0.47}$ RV semi amplitude ($\,{\rm{m}}\ {{\rm{s}}}^{-1}$) Kosiarek et al. (2019)
Mpl ${12.58}_{-1.28}^{+1.31}$ Mass of the planet (${M}_{\oplus }$) Kosiarek et al. (2019)
b ${0.47}_{-0.110}^{+0.074}$ Impact Parameter Dragomir et al. (2015)

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3. Results and Discussion

3.1. Evidence for He i 10830 Å Absorption during Transits

The blue curve at the top of Figure 1 shows the weighted average of all the in-transit spectra from three transit epochs divided by the average of the out-of-transit spectra. The vacuum wavelengths of the He 10830 Å triplet in the planet's rest frame are marked by the orange vertical lines. Since the telluric correction as well as the sky emission line subtraction are not perfect, regions of sky/telluric contamination have enlarged error bars as discussed in Section 2. The weighted average of all combinations of transits taken two at a time is also shown in the curves below. The single peak observed at 10833 Å is not present in Transits 2 and 3, it is only seen in Transit 1. However, since 10833 Å was separated from the telluric band only during Transit 1, it did not get averaged out in the final weighted average. Since Transit 1 had only half the S/N compared to the other two transits we suspect this is an artifact due to photon and detector noise (see blue curves in Figure 5 for the individual ratio spectrum from Transit 1). For a null result comparison, one of the out-of-transit epochs is also shown in Figure 1. These data are processed the same way as other in-transit spectra, and we do not see any signatures of absorption inside the He 10830 Å triplet window.

Figure 1.

Figure 1. Evidence of broad He 10830 absorption (EW: 0.012 ± 0.002 Å) in the wavelength range 10832.2–10833.4 Å in the in-transit/out-transit spectrum during three transits of GJ 3470b. The x-axis shows vacuum wavelength in the planet's rest frame at midtransit. The rest vacuum wavelengths of the He 10830 Å triplet lines in planet's rest frame are marked by the vertical dashed and solid orange lines. The gray region highlights the broad absorption discussed in this paper, and it is the wavelength window we used to measure reported equivalent widths. The expected line profile from our simple model described in Section 3.3.1 is also shown for comparison by the red curves. An out-of-transit epoch divided by the reference out-of-transit spectrum is also shown at the bottom, demonstrating the lack of any absorption in out-of-transit data.

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3.2. Column Density Measurement from Equivalent Width (EW) Analysis

We measure the integrated EW of the detected broad absorption in the vacuum wavelength range (10831.9 Å to 10833.6 Å ) in Figure 1 to be 0.012 ± 0.002 Å. We ignored the J = 0 line (10832.06 Å in vacuum) of the triplet since its oscillator strength is only one-eighth of the other two lines combined, so it is below our continuum noise (the J = 0 line is the dashed orange line in Figure 1). The resonant scattering absorption of He i 10830 Å is directly proportional to the number density of He i in the 23S metastable triplet state. We use the curve of growth analysis in the optically thin regime to estimate the column density of $\mathrm{He}{\,}_{3}^{2}{\rm{S}}$ metastable atoms,

Equation (1)

where ${N}_{\mathrm{He}{}_{3}^{2}{\rm{S}}}$ is the column density of $\mathrm{He}{\,}_{3}^{2}{\rm{S}}$ metastable atoms in ${\mathrm{cm}}^{-2}$, EW is the measured combined EW of J = 1 and J = 2 lines of He 10830 Å triplet in units of Å, λ2 and λ3 are the wavelengths of the J = 1 and J = 2 triplet lines in units of microns, and ${f}_{{{ik}}_{2}}$ and ${f}_{{{ik}}_{3}}$ are the oscillator strengths of the lines taken from the NIST Atomic Spectra Database Lines Database (Drake 2006).

Substituting our measured EW, we obtain ${N}_{\mathrm{He}{}_{3}^{2}{\rm{S}}}=2.4\times {10}^{10}\ \,{\mathrm{cm}}^{-2}$. This measured EW is a flux-weighted average across the unresolved stellar disk during the transit. Hence, the column density we measure is also a stellar disk flux-weighted average column density of the exosphere during the transit.

3.3. Theoretical Column Density from an Exosphere Model

We modeled the steady-state helium distribution in the outflowing exosphere of GJ 3470b using the formalism and state transition coefficients outlined in Oklopčić & Hirata (2018). Using hydrodynamic simulations Salz et al. (2016) show that the exosphere of GJ 3470b is not isothermal. We therefore do not use a Parker wind model for our atmospheric analysis, but solve for the steady-state helium distribution using the velocity and density field of the exosphere from the Salz et al. (2016) PLUTO-CLOUDY hydrodynamic simulations. To be internally consistent, we also used the GJ 3470 stellar SED used by Salz et al. (2016).

The X-ray spectrum of GJ 3470 we used from Salz et al. (2016) is calculated using the plasma emission model from CHIANTI (Dere et al. 1997, 2009) normalized to the X-ray luminosity of GJ 3470b estimated based on the stellar rotation period and the stellar mass (Pizzolato et al. 2003). The EUV flux (100 Å to ∼912 Å), which is critical for these calculations due to the strong dependence of helium ionization, comes from the scaling of the model-dependent Lyα flux (Linsky et al. 2014). The model-dependent Lyα flux of GJ 3470 itself is estimated by the Linsky et al. (2013) model based on the X-ray luminosity. See Section 2.2 of Salz et al. (2016) for more details. This model-dependent irradiance spectrum of GJ 3470 is the source of the biggest uncertainty in our calculations. However, the model-dependent Lyα flux Salz et al. (2016) derive, and the value we adopt here, is consistent with the Lyα flux measured by Bourrier et al. (2018) during three transits of GJ 3470b using the Space Telescope Imaging Spectrograph instrument on board the HST.

As most of the free electrons in the atmospheres of exoplanets come from ionized hydrogen, to obtain the electron density of the GJ 3470 atmosphere, we first solved for the steady-state of hydrogen following Oklopčić & Hirata (2018). To obtain the steady-state distribution of helium atoms, we briefly discuss here the relevant system of integro-differential equations from Oklopčić & Hirata (2018), given by,

Equation (2)

and,

Equation (3)

where f1 and f3 are the fractions of neutral helium in the ground state of the singlet and triplet states, respectively, v is the velocity of the outflowing exosphere as a function of radius we adopt from Salz et al. (2016), ne is the density of free electrons we obtained by solving the steady-state of hydrogen, and α1 and α3 are the helium recombination rates to singlet and triplet state from Osterbrock & Ferland (2006), respectively. The collision coefficients qijk and Q31 are from Oklopčić & Hirata (2018), calculated using coefficients from Bray et al. (2000) and Roberge & Dalgarno (1982). The radiative decay rate A31 from the helium metastable state to singlet state is adopted from Drake (1971). Φ1 and Φ3 are the effective photoionization rate coefficients calculated using,

Equation (4)

where Fλ is the irradiated flux on GJ3470b described earlier in this section, aλ is the photoionization cross section taken from Brown (1971) for the singlet state, and from Norcross (1971) for the triplet state. For the singlet state, the integral is evaluated up to the ionization wavelength of helium (504 Å), while for the triplet state the integral is computed in the interval starting at the Lyman limit19 (911.6 Å) to the metastable state ionization wavelength (2583 Å).

To calculate the optical depths τ1 and τ3 as a function of radius for the singlet and metastable states of helium, we compute the following integrals,

Equation (5)

and,

Equation (6)

where mp is the proton mass, ρ(r) is the density of the GJ3470b exosphere from Salz et al. (2016), fH+ is the fraction of ionized hydrogen we obtained by solving the steady-state of hydrogen. aoH and aoHe are GJ3470b's irradiation flux-averaged hydrogen and helium ionization cross sections in the wavelength range up to helium ionization (504 Å). aoHe2S3 is the flux-averaged cross section of $\mathrm{He}{\,}_{3}^{2}{\rm{S}}$ in the wavelength range 911.6 Å (hydrogen ionization) to 2583 Å ($\mathrm{He}{\,}_{3}^{2}{\rm{S}}$ ionization).

We solve Equations (2) and (3) iteratively as an initial boundary value partial differential equation by starting with an initial estimate for the optical depth integral term (Equations (5) and (6)). Using the resulting solution, we updated the integral term in Equations (5) and (6). The final solutions converged within one or two iterations since the integral term has impact only in the high opacity base region of the outflowing atmosphere. The differential equation of $\mathrm{He}{\,}_{3}^{2}{\rm{S}}$ metastable atoms (Equation (3)) is very stiff for high densities of GJ 3470b, and we therefore used a Radau solver with adaptive dense gridding (Hairer & Wanner 1996).

The one-dimensional radial density distribution of $\mathrm{He}{\,}_{3}^{2}{\rm{S}}$ metastable atoms obtained above is then integrated assuming a spherical exosphere to obtain column densities at different impact parameters from the planet (Figure 2(b)). We expect the model to fail beyond the Roche-lobe due to complex stellar wind interactions. We estimate the volume equivalent Roche-lobe radius of the GJ 3470b system to be 3.12 Rp following Eggleton (1983). The teardrop shaped Roche-lobe's extent on the star–planet axis is 5.96 Rp (Salz et al. 2016). Both of these points are explicitly highlighted in Figure 2. Assuming an impact parameter of b = 0.47 (Dragomir et al. 2015), Figure 2(a) shows the 2D projection of the system during the midpoint of the transit. In Figure 2(a) we also illustrate the stellar disk on top of the column density map of $\mathrm{He}{\,}_{3}^{2}{\rm{S}}$ metastable atoms. To estimate the flux-averaged column density, we used a quadratic limb-darkening model where we calculated the limb-darkening coefficients using the EXOFAST web-applet20 using the stellar effective temperature, metallicity, and surface gravity from Table 1, in the J band. This flux-weighted average column density is dependent on how far the exosphere extends beyond the Roche-lobe; the predicted background stellar disk flux-weighted average column density of $\mathrm{He}{\,}_{3}^{2}{\rm{S}}$ metastable atoms as a function of the extent of GJ 3470b's exosphere is shown by the dashed line in Figure 2(b)).

Figure 2.

Figure 2. (a) The 2D diagram showing the projection of the Roche lobe radii as well as the GJ3470 stellar disk on top of the spherical 1D $\mathrm{He}{\,}_{3}^{2}{\rm{S}}$ metastable atom column density map predicted by our 1D simulation of GJ 3470b. The volume equivalent Roche lobe radius as well as the Roche lobe extent on the star–planet axis is marked by the dotted and dashed circles respectively. The large circle marks the disk of the star. (b) The radial cut plot of the column density along the blue line in left figure is shown here as "Radial ${N}_{\mathrm{He}{}_{3}^{2}{\rm{S}}}$." The volume equivalent Roche lobe radius as well as the Roche lobe extend on the star–planet axis is marked by the square and dot respectively. The triangle marks the radius of the star. The dashed line shows the background stellar disk flux-averaged column density predicted by our model at the center of the transit. It is a function of the assumed extent of the exosphere beyond the volume equivalent Roche lobe as shown on left.

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3.3.1. Line Profile Model

The broad absorption we present evidence for during the transit of GJ 3470b is possibly the broadest He 10830 Å absorption reported in the literature to date. It spans a velocity range of −36 to +9 km s−1. Figure 3(a) shows the outflowing exosphere velocity from Salz et al. (2016). The wind reaches only velocities up to ∼10 km s−1 inside 3.12 Rp—the volume equivalent Roche-lobe radius. Both the volume equivalent Roche lobe radius as well as the Roche lobe extent on the star–planet axis (5.96 Rp) is marked by vertical lines in the plot.

Figure 3.

Figure 3. (a) The top left panel shows the one-dimensional wind velocity model for GJ 3470b from Salz et al. (2016). The volume equivalent Roche lobe radius as well as the Roche lobe extent on the star–planet axis is marked by the square and dot respectively. (b) The lower left panel shows the time of flight for a helium atom to reach a certain radius from the volume equivalent Roche lobe radius. (c) The line-of-sight velocity field of exosphere around GJ 3470b, Earth observer is toward the left side of the axis and the host star is toward the right side.

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The line-of-sight velocity of the helium atoms we see during the transit is the sum of the hydrodynamic driven wind velocity plus the stellar radiative acceleration, and the planet's orbital radial velocity at the instant of their escape from the planet's gravitational potential. For example, helium atoms escaping the planet potential ∼2.5 hr before the transit will have a line-of-sight velocity of ∼−30 km s−1 during the transit due to change in the line-of-sight component of planet's orbital velocity. Figure 3(b) shows the time a helium atom will take to travel the distance based on the wind model after it leaves the Roche lobe. Atoms that escape the potential 2.5 hr before the transit will be at ∼8 Rp, which is well within the projected stellar disk.

For calculating the line profile predicted by our model, we need to calculate the line-of-sight velocity field of the GJ 3470b exosphere at all impact parameter positions and radial distances. For the region inside the volume equivalent Roche Lobe, we consider only the line-of-sight projection of the radial hydrodynamic wind velocity. For the region outside the Roche lobe, we added the line-of-sight component of the hydrodynamic wind to the difference in the planet's radial velocity between present and the time at which gas at a certain altitude escaped the Roche lobe. Figure 3(c) shows this velocity field. The observer on Earth is toward the left side of the axis and the host star is toward the right side. The negative line-of-sight velocity implies gas is moving toward the observer. In reality, there will be additional blueshift due to the interaction with stellar wind. We do not include any stellar wind induced blueshift of the exosphere in our line model.

To model the line profile, we used the Voigt profile. The modeling methodology is mostly similar to Oklopčić & Hirata (2018), the only difference is in not assuming a spherically symmetric velocity field, and using the GJ 3470b system's impact parameter and stellar disk limb-darkening model while integrating the absorption line profile across the stellar disk. The temperature of the gas for the thermal Gaussian component of the modeled Voigt profile was taken to be 7000 K (Salz et al. 2016; Bourrier et al. 2018). The He 10830 line's Einstein coefficient for the Lorentzian component of the Voigt profile was taken from NIST Atomic Spectra Database Lines Database (Drake 2006). The oscillator strengths for the cross section calculation of each triplet line is also taken from the NIST Database. These cross sections, along with the radial density distribution of the metastable helium we obtained in our model (Section 3.3) were integrated to obtain the optical depth at different impact parameter distances from the planet. Density of metastable helium outside 13 Rpl (radial limit of our 1D model) was set to zero in our integrals. Using a quadratic limb-darkening model, we averaged the transmission curve across the disk to obtain the net transmission profile of the He 10830 triplet lines in GJ 3470b during the transit. Since the measured column density is less than the model predicted column density by a factor of 10 (see Section 3.4), we scaled down the density distribution from our model also by a factor of 10. This predicted line profile is overplotted over all the transit and out of transit ratio spectra in Figure 1.

3.3.2. Limits of the Model

The simplified one-dimensional model we presented here is to check whether the strength of our claimed helium 10830 Å absorption in the exoplanet atmosphere is within the limits of expected physical conditions. A true three-dimensional wind model where the stellar irradence is only on one side of the planet is known to have lesser density on average in all angles by a factor of 4 than the one-dimensional symmetric wind model we used (Stone & Proga 2009).

The other major source of uncertainty in our model is the irradiated flux in the wavelengths shorter than helium ionization (λ < 512Å). As briefly outlined in the section above, it is estimated by a chain of empirical models. We expect the helium ionization flux to have a significant influence on the population of metastable He atoms. To study the impact, we simulated how the predicted column density of $\mathrm{He}{\,}_{3}^{2}{\rm{S}}$ metastable atoms changes when we suppress the irradience at wavelength shorter than 504 Å by different factors.21 Results are shown in Figure 4. Since we wanted to probe only the impact on the steady state of helium atoms, the underlying velocity field and density used in the differential equation was kept fixed, and is the same as the Salz et al. (2016) hydrodynamic model for the original irradiance. It is very instructive to see that the observed column density of metastable helium is reduced proportionally to the reduction in the helium ionization flux.

Figure 4.

Figure 4. The column density of $\mathrm{He}{\,}_{3}^{2}{\rm{S}}$ metastable atoms predicted by the 1D simulation of GJ 3470b is reduced proportionally to the flux in wavelengths less than 504 Å when everything else—including the density and velocity—is kept fixed. The volume equivalent Roche lobe radius as well as the Roche lobe extent on the star–planet axis is marked by the square and dot respectively. The triangle marks the radius of the star. The dashed lines show the flux-averaged column density predicted by this model at the center of the transit as a function of the extent of the exosphere beyond the volume equivalent Roche lobe. The horizontal orange line shows the measured average column density in transits of GJ 3470b using HPF.

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In real systems, since the mass outflow is proportional to the energy absorbed in the lower atmosphere from irradiance, there will be an additional proportional reduction in density when the EUV flux irradiation is reduced. Hence, the combined effect of reduction in helium ionizing radiation is quadratic on the column density of meta-stable helium atoms.

A few more ways the underlying density of the wind we used in our simulation from Salz et al. (2016) can be impacted is summarized in Table 2 of Salz et al. (2016).

3.4. On the Difference between the Predicted and Measured Column Densities

As described in Section 3.2, the measured flux-weighted column density of He ${}_{3}^{2}{\rm{S}}$ is ${N}_{\mathrm{He}{}_{3}^{2}{\rm{S}}}=2.4\times {10}^{10}\,{\mathrm{cm}}^{-2}$. This is a factor of 10 less than predicted by our one-dimensional hydrodynamic model described in Section 3.3. However, as discussed in Section 3.3.2, if we correct our simulation for the 3D model simplification to the 1D model by the factor of 4 (Stone & Proga 2009), and assume the helium ionization radiation is lesser by a factor of 1.6 (which is well within the error of the empirically derived EUV SED of GJ3470 in Salz et al. 2016), we reduce the predicted metastable helium by a factor of $4\times {1.6}^{2}=10$. Hence, our observations are consistent with our simplified model under the caveats outlined in Section 3.3.2.

3.5. On the Difference in Model Line Profile and the Observed Absorption Signature

We discuss a few possible reasons for differences in the shape of the simple model and observed line profile below.

Stellar Activity: Some M dwarfs can be active, and exhibit time variability in the He 10830 absorption line (we note that not all M dwarfs are active). In comparison to other transmission spectroscopy lines like Ca ii K, Na i D, and Hα, active regions typically have He 10830 in absorption (Cauley et al. 2018). Thus, when a planet transits an active spot region on the host star, He 10830 is more likely to result in an emission signature, than an absorption signature. Thus He 10830 absorption signatures in-transit spectroscopy are more likely to originate in the exosphere than from the stellar chromosphere. However, under high density chromosphere conditions (Andretta & Giampapa 1995), or active flares, it is possible to obtain He 10830 in emission from the recombination cascade of ionized helium (Huenemoerder & Ramsey 1987). We do not see any indication of flares during transit in the Ca II IR triplet lines. If the absorption we detected was due to GJ 3470b transiting a very active emission spot, we would expect the absorption signal to not be present in all the in-transit spectra taken (see Figure 5). We have a total of nine in-transit spectra, (three spectra from three transits each). Since the phase of each spectrum is slightly different, it is improbable that there was an unusually strong emission spot of He 10830 during each of our transits. Hence, stellar activity cannot explain the absorption signal we detected during transit of GJ3470b. Stellar activity, however, could probably explain some of the emission structures, and there by the net absorption strength variations we measured across the three transits.

Figure 5.

Figure 5. Individual in-transit by out-of-transit ratio HPF spectrum of all nine epochs from the three transits are shown here. Blue curves are the three spectra from the first transit, green are the second transit spectra, and red are the third transit spectra. The black curve is the weighted average with error bars of all the in-transit by out-of-transit spectra. Translucent parts of the curves are telluric and sky emission line corrected regions in each spectrum. They are deweighted to remove any systematic artifacts from influencing the final average. The x-axis shows vacuum wavelength in the planet's rest frame at midtransit. The rest of the vacuum wavelengths of the He 10830 Å triplet lines in the planet's rest frame are marked by the vertical dashed and solid orange lines.

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Telluric Absorption and Sky Emission: Systematics in telluric and sky emission line modeling could potentially cause profile variations in the regions with high error bars in Figure 1. The regions with small error bars are free of any telluric or sky emission line contamination in at least one epoch out of the three transit observations. Hence, imperfect telluric line modeling errors cannot explain the absorption signature.

Stellar Wind: Even though our simple model, which includes the orbital dynamics and the hydrodynamic outflow velocity, could explain the large blueshifted profile seen in the data, it does not fully explain the shape of the detected line. Some component of this discrepancy could be variability; however, we suspect the stellar wind to play a major role. Since stellar wind accelerates the exosphere toward Earth like a comet tail, it could further blueshift the exosphere at the base of the exosphere skewing the line profile to shorter wavelengths. Further monitoring of the GJ 3470b's He 10830 signature during transits will reveal greater insights on the system.

4. Conclusion

We report evidence for He 10830 Å absorption from meta-stable helium atoms in the base of the outflowing exosphere of the M-dwarf planet GJ 3470b in three transits using the HPF near-infrared spectrograph at the 10 m HET at the McDonald Observatory. This measurement marks the first evidence for He 10830 absorption in an M-dwarf planet. Further, we detect the helium absorption in the velocity range of −36 to +9 km s−1, marking the largest blueshift of He 10830 absorption reported so far in the literature. From our observed absorption, we measure an EW of $\mathrm{EW}=0.012\pm 0.002\,\mathring{\rm A} $, corresponding to a disk surface flux-averaged column density of ${N}_{\mathrm{He}{}_{3}^{2}{\rm{S}}}=2.4\times {10}^{10}\,{\mathrm{cm}}^{-2}$. Both the velocity range and the column density we measure are consistent with our exosphere model based on the work of Salz et al. (2016) and Oklopčić & Hirata (2018) to within the model uncertainties of the UV and X-ray flux of GJ 3470. These observations suggest that detection of the He 10830 absorption around hot Neptunes is now within reach of ground-based facilities—opening up a new window to probe these systems. Puzzling aspects of the broad absorption seen remain, and we have attempted to discuss their source. We recommend future ground- and space-based observations to probe the physics of this absorption signal at even higher signal to noise.

The authors wish to thank M. Salz and A. Oklopčić for discussions that contributed to this work. We thank the anonymous referee for a thoughtful reading and suggestions that improved the quality of the manuscript.

This work was partially supported by funding from the Center for Exoplanets and Habitable Worlds. The Center for Exoplanets and Habitable Worlds is supported by the Pennsylvania State University, the Eberly College of Science, and the Pennsylvania Space Grant Consortium. We acknowledge support from NSF grants AST-1006676, AST-1126413, AST-1310885, AST-1517592, AST-1310875, the NASA Astrobiology Institute (NAI; NNA09DA76A), PSARC, and NIST in our pursuit of precision radial velocities in the NIR. Computations for this research were performed on the Pennsylvania State University's Institute for CyberScience Advanced CyberInfrastructure (ICS-ACI). We acknowledge support from the Heising-Simons Foundation via grant 2017-0494. This work was supported by NASA Headquarters under the NASA Earth and Space Science Fellowship Program through grants NNX16AO28H and 80NSSC18K1114. Part of this research was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with NASA.

These results are based on observations obtained with the Habitable-zone Planet Finder Spectrograph on the Hobby–Eberly Telescope. We thank the Resident astronomers and Telescope Operators at the HET for the skillful execution of our observations of our observations with HPF. The Hobby–Eberly Telescope is a joint project of the University of Texas at Austin, the Pennsylvania State University, Ludwig-Maximilians-Universität München, and Georg-August Universität Gottingen. The HET is named in honor of its principal benefactors, William P. Hobby and Robert E. Eberly. The HET collaboration acknowledges the support and resources from the Texas Advanced Computing Center.

This research has made use of NASA's Astrophysics Data System Bibliographic Services.

Facility: HET (HPF). -

Software: barycorrpy (Kanodia & Wright 2018), astropy (Astropy Collaboration et al. 2018), numpy (van der Walt et al. 2011), scipy (Jones et al. 2001), matplotlib (Hunter 2007), CoCalc (SageMath 2019), GNU parallel (Tange 2011).

Footnotes

  • 19 

    Photons of energy higher than the Lyman limit are many orders of magnitude more likely to be absorbed by the hydrogen than $\mathrm{He}{\,}_{3}^{2}{\rm{S}}$, hence the beginning of the integral window was chosen to be at 911.6 Å.

  • 20 
  • 21 

    The reason we chose 504 Å for this test instead of 512 Å is because photons of energy higher than 504 Å are more likely to ionize a helium atom than a hydrogen atom due to the factor of 10 lower abundance of helium than hydrogen. We want to probe the impact on helium ionization alone without significant change to hydrogen ionization.

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10.3847/1538-4357/ab8559