An Extremely Elongated Cloud over Arsia Mons Volcano on Mars: II. Mesoscale modeling
Jorge From: Jorge Hern\'andez-Bernal, Aymeric Spiga, Agustin Sanchez, Lavega, Teresa del Rio Gaztelurrutia, Francois Forget, Ehouarn Millour

TL;DR
This study uses mesoscale modeling to investigate the physics behind the formation and characteristics of the extremely elongated Arsia Mons Elongated Cloud on Mars, revealing windstorm dynamics but not fully capturing the cloud's microphysics.
Contribution
It applies the LMD mesoscale model to Mars' Arsia Mons, providing new insights into the wind-driven processes influencing the cloud's morphology and dynamics.
Findings
Downslope windstorm triggers vertical updrafts.
Model captures diurnal cycle of the cloud head.
Microphysics of the cloud are not fully reproduced.
Abstract
In a previous work (Hern\'andez-Bernal et al. 2021) we performed an observational analysis of the Arsia Mons Elongated Cloud (AMEC), which stands out due to its impressive size and shape, quick dynamics, and the fact that it happens during the martian dusty season. Observations show that its morphology can be split in a head, on the western slope of the volcano of around 120 km in diameter; and a tail, that expands to the west reaching more than 1000 km in length, making the AMEC the longest orographic cloud observed so far in the solar system. In this work we run the LMD (Laboratoire de M\'et\'eorologie Dynamique) Mesoscale Model to gain insight into the physics of the AMEC. We note that it is coincident in terms of local time and seasonality with the fastest winds on the summit of Arsia Mons. A downslope windstorm on the western slope is followed by a hydraulic-like jump triggering a…
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