Warm early Mars surface enabled by high-altitude water ice clouds

Despite receiving just 30% of the Earth?s present-day insolation, Mars had water lakes and rivers early in the planet?s history, due to an unknown warming mechanism. A possible explanation for the >102-y-long lake-forming climates is warming by water ice clouds. However, this suggested cloud greenhouse explanation has proved difficult to replicate and has been argued to require unrealistically optically thick clouds at high altitudes. Here, we use a global climate model (GCM) to show that a cloud greenhouse can warm a Mars-like planet to global average annual-mean temperature (T) -265 K, which is warm enough for low-latitude lakes, and stay warm for centuries or longer, but only if the planet has spatially patchy surface water sources. Warm, stable climates involve surface ice (and low clouds) only at locations much colder than the average surface temperature. At locations horizontally distant from these surface cold traps, clouds are found only at high altitudes, which maximizes warming. Radiatively significant clouds persist because ice particles sublimate as they fall, moistening the subcloud layer so that modest updrafts can sustain relatively large amounts of cloud. The resulting climates are arid (area-averaged surface relative humidity -25%). In a warm, arid climate, lakes could be fed by groundwater upwelling, or by melting of ice following a cold-to-warm transition. Our results are consistent with the warm and arid climate favored by interpretation of geologic data, and support the cloud greenhouse hypothesis.

Automated summary

Given just 30% of Earth's present-day insolation, Mars had water lakes and rivers early in its history due to an unknown warming mechanism that could be a cloud greenhouse effect. This effect can warm a Mars-like planet to temperatures suitable for low-latitude lakes for centuries if the planet has spatially patchy surface water sources. In warm, arid climates, lakes could be fed by groundwater upwelling or ice melting following a cold-to-warm transition.