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University of Cambridge > Talks.cam > Institute of Astronomy Seminars > A new convection scheme for exoplanet atmospheres
A new convection scheme for exoplanet atmospheresAdd to your list(s) Download to your calendar using vCal
If you have a question about this talk, please contact Hannah Uebler. Convection is an essential process for transporting heat and moisture in planetary atmospheres. The standard Earth picture of moist convection rising from the surface is only one of a number of modes of convection. Notably, convection in atmospheres with a high condensible mass fraction (non-dilute atmospheres), or with a lighter background gas than the condensible species (e.g. water convection in a hydrogen dominated atmosphere) – acts very differently and can be much weaker or even shut down entirely in the latter case. Here I present a new mass-flux scheme which can capture these variations and simulate convection in a wide range of parameter space for use in 3D climate models. A validation using the case of Trappist-1 e is presented. This talk is part of the Institute of Astronomy Seminars series. This talk is included in these lists:
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