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Table 1

Parameters of the planets considered for the comparison with the results of Salz et al. (2016a).

Planet Mpl [M] Rpl [R] Teq [K] a [AU] M* [M] FX [erg s−1 cm−2] FEUV [erg s−1 cm−2] salz2016 [g s−1] wind [g s−1] def [g s−1]
GJ 3470 b 14.0 4.14 650 0.036 0.539 1170.4 6431.6 1.86 × 1011 1.51 × 1011 2.10 × 1011
HAT-P-11 b 26.4 4.70 850 0.053 0.8 449.1 2706.3 8.08 × 1010 8.01 × 1010 8.69 × 1010
GJ 1214 b 6.36 2.69 550 0.014 0.18 147.5 739.0 1.98 × 1010 2.05 × 1010 2.54 × 1010
GJ436b 23.2 4.25 650 0.029 0.45 38.6 583.6 1.88 × 1010 1.53 × 1010 1.56 × 1010
HD 97658 b 7.95 2.35 750 0.08 0.85 92.2 860.5 1.23 × 1010 1.12 × 1010 1.50 × 1010
HD 149026 b 114.4 7.28 1440 0.043 1.3 7655.8 12134 1.10 × 1011 1.11 × 1011 1.50 × 1011
HD 189733 b 349.8 12.31 1200 0.031 0.81 5600.2 15073 1.59 × 1010 1.39 × 1010 2.05 × 1010
HD 209458 b 219.4 15.67 1320 0.047 1.12 40.4 1113.6 8.16 × 1010 1.67 × 1011 2.62 × 1011
WASP-80b 174.88 10.64 800 0.034 0.57 2177.6 8870.9 1.46 × 1011 1.92 × 1011 2.18 × 1011

Notes. The last three columns correspond to the atmospheric mass-loss rate obtained by Salz et al. (2016a, Salz2016) and obtained with our model including (wind) and excluding (def) wind advection in the Cloudy computation. According to Salz et al. (2016a), the planetary and stellar parameters were adopted from the following studies. GJ 3470 b: Bonfils et al. (2012); Biddle et al. (2014) ; HAT-P-11 b: Bakos et al. (2010); GJ 1214b: Charbonneau et al. (2009); Berta et al. (2011); GJ 436 b: Butler et al. (2004); Knutson et al. (2011); HD 97658 b: Howard et al. (2011); HD 149026 b: Sato et al. (2005); Knutson et al. (2009); HD 189733 b: Bouchy et al. (2005); Henry & Winn (2008); Southworth (2010); Knutson et al. (2009); HD 209458 b: Charbonneau et al. (2000); Henry et al. (2000); Torres et al. (2008); Silva-Valio (2008); Crossfield et al. (2012); and WASP-80 b: Triaud et al. (2013). The values of the atmospheric mass-loss rates given here are a factor of four higher compared to those given in Table 3 of Salz et al. (2016a), as we do not apply surface averaging.

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