May 27, 2020 (1.0)
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Crustal Hydration of Ocean-scale Volumes Controlled the Martian Climate and Habitability
Logarithmic hydrogen escape (H/s) represented in color per individual climate case (described in the text). Surface temperature is varied by each row of subplots from 190-300 K. Mesospheric temperature is varied by each column of subplots from 130-170 K. Surface pressure is varied from 0.002-5 bar on the x-axis of each subplot. Three climate con...
Uploaded on September 8, 2022