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We explain how GCM boundary condition choices such as ocean-lake coverage-depth, rotation rate, atmospheric constituents and other factors influence surface conditions in ROCKE-3D paleo-Venus simulations. Studies such as these should also be considered when examining liquid water habitability in similar exoplanet experiments. We also describe how one ingests 3D topographic data from NASAs Venus Magellan Spacecraft radar observations into the ROCKE-3D Planetary General Circulation Model.

生成讲解博客的中文版本

生成AI智能校验的中文版本