An atmospheric general circulation model for Pluto with predictions for New Horizons temperature profiles
Angela M. Zalucha

TL;DR
This paper presents a comprehensive 3-D atmospheric model for Pluto that incorporates various heating and cooling processes, surface interactions, and predicts temperature profiles and light curves relevant for New Horizons and ground observations.
Contribution
The study develops a detailed Pluto GCM including non-LTE processes, subsurface effects, and surface-atmosphere exchange, providing novel predictions for temperature profiles and observational signatures.
Findings
Prograde jets identified at multiple altitudes.
Flow direction over poles varies with altitude.
Methane concentration affects temperature profiles and occultation light curves.
Abstract
Results are presented from a 3-D Pluto general circulation model (GCM) that includes conductive heating and cooling, non-local thermodynamic equilibrium (non-LTE) heating by methane at 2.3 and 3.3 microns, non-LTE cooling by cooling by methane at 7.6 microns, and LTE CO rotational line cooling. The GCM also includes a treatment of the subsurface temperature and surface-atmosphere mass exchange. An initially 1 m thick layer of surface nitrogen frost was assumed such that it was large enough to act as a large heat sink (compared with the solar heating term) but small enough that the water ice subsurface properties were also significant. Structure was found in all three directions of the 3-D wind field (with a maximum magnitude of order 10 m/s in the horizontal directions and 10 microbar/s in the vertical direction). Prograde jets were found at several altitudes. The direction of flow…
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