Please use this identifier to cite or link to this item:
http://hdl.handle.net/20.500.12666/487
Title: | Modelling martian dust devils using in-situ wind, pressure, and UV radiation measurements by Mars Science Laboratory |
Authors: | Kahanpää, H. Viúdez Moreiras, Daniel |
Keywords: | Mars;Mars Atmosphere;Dynamics;Meteorology |
Issue Date: | 1-May-2021 |
Publisher: | Elsevier BV |
DOI: | 10.1016/j.icarus.2020.114207 |
Published version: | https://www.sciencedirect.com/science/article/abs/pii/S0019103520305406 |
Citation: | Icarus 359: 114207(2021) |
Abstract: | NASA's Mars Science Laboratory rover Curiosity (MSL) has measured simultaneous fluctuations in wind and atmospheric pressure caused by passing convective vortices, i.e. dustless dust devils. We study the dynamics of these vortices by fitting a mathematical vortex model to the wind and pressure measurements of MSL. The model matches the data adequately well in 29 out of the 33 studied vortex pass events having sufficient data quality. Clockwise and counterclockwise rotating directions are equally common among the studied convective vortices. The vortices seem to prefer certain trajectories, e.g. avoiding steep slopes. However, our results show that due to sensitivity constraints of the method, central pressure drops of Martian dust devils can usually not be accurately determined by fitting a theoretical vortex model to simultaneous pressure and wind measurements of a single station. We also present a methodology extension for further constraining the trajectories and the strengths of dust laden vortices (i.e. dust devils), based on concurrent in-situ solar irradiance measurements. We apply this methodology to the only evidently dust laden vortex in our data set and show that its dust lifting capacity is probably based not only on wind stress lifting. |
Description: | Martian dust devils are studied by in-situ wind, pressure, and UV data. A methodology for fitting a mathematical vortex model to the data is presented. Clockwise and counterclockwise rotating vortices are equally common. The dust devils prefer relatively flat terrain. Martian dust devils appear to lift dust not only by wind stress. |
URI: | http://hdl.handle.net/20.500.12666/487 |
E-ISSN: | 1090-2643 |
ISSN: | 0019-1035 |
Appears in Collections: | (CAB) Artículos |
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