In 1D N2-CO2-H2O model atmospheres, increasing background N2 pressure warms the climate under low CO2 via H2O dilution and under high CO2 via H2O loading, while high N2 induces cooling via Rayleigh scattering that can be overwhelmed by enhanced H2O absorption.
Title resolution pending
2 Pith papers cite this work. Polarity classification is still indexing.
2
Pith papers citing it
fields
astro-ph.EP 2years
2026 2verdicts
UNVERDICTED 2representative citing papers
Mars provides key diagnostics for volatile delivery, atmospheric escape, and climate processes on small rocky exoplanets near the edge of habitability.
citing papers explorer
-
Revisiting the greenhouse effect of non-greenhouse gases in the atmospheres of Earth-like planets
In 1D N2-CO2-H2O model atmospheres, increasing background N2 pressure warms the climate under low CO2 via H2O dilution and under high CO2 via H2O loading, while high N2 induces cooling via Rayleigh scattering that can be overwhelmed by enhanced H2O absorption.
-
Mars as an Exoplanet: Lessons from a Planet at the Edge of Habitability
Mars provides key diagnostics for volatile delivery, atmospheric escape, and climate processes on small rocky exoplanets near the edge of habitability.