Archive: Tidally Locked Earth

Surface Temperature

The surface temperature changes rapidly over land masses to day-side values of about 290 K and to night-side values of about 240 K. The ocean

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Precipitation

Precipitation patterns change rapidly (within a few months) from the zonally-elongated intertropical convergence zone that is typical of Earth today to a configuration in which

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Sea Ice

Because the ocean is actively convecting where it is near freezing, no sea ice forms during this simulation, except near the coasts. However, the ocean

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