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- W2033767972 abstract "Global climate model simulations using high-obliquity (70°), higher CO2 and CH4 but reduced O3 concentrations produce warm climate conditions for Archean boundary conditions (reduced solar forcing). Solar radiation under high-obliquity is distribution in such a way as to warm high latitudes and cool low-latitudes. Global mean air temperatures of approximately 280°K are found with a 25% reduction in the solar forcing, 4760 ppmv CO2 and 25 ppmv CH4. High-obliquity could also explain why polar oceans on Mars may have occurred in its history. A substantial increase in the amount of insolation is accounted for if Mars had an obliquity of 70°." @default.
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- W2033767972 date "2001-12-01" @default.
- W2033767972 modified "2023-09-23" @default.
- W2033767972 title "High-obliquity simulations for the Archean Earth: Implications for climatic conditions on early Mars" @default.
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- W2033767972 doi "https://doi.org/10.1029/2000je001427" @default.
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