Logo image
A hot flow anomaly at Mars
Journal article   Open access   Peer reviewed

A hot flow anomaly at Mars

Glyn Collinson, Jasper Halekas, Joseph Grebowsky, Jack Connerney, David Mitchell, Jared Espley, Gina DiBraccio, Christian Mazelle, Jean-Andre Sauvaud, Andrei Fedorov, …
Geophysical research letters, Vol.42(21), pp.9121-9127
11/16/2015
DOI: 10.1002/2015GL065079
url
https://doi.org/10.1002/2015GL065079View
Published (Version of record) Open Access

Abstract

One of the most important modes of planet/solar wind interaction are "foreshock transients" such as hot flow anomalies (HFAs). Here we present early observations by the NASA Mars Atmosphere and Volatile EvolutioN spacecraft, confirming their presence at Mars and for the first time at an unmagnetized planet revealing the underlying ion perturbations that drive the phenomenon, finding them to be weaker than at magnetized planets. Analysis revealed the HFA to be virtually microscopic: the smallest on record at similar to 2200 km across and commensurate with the local proton gyroradius, resulting in a much stronger perturbation in solar wind protons than alpha particles. As at Venus, despite being physically diminutive, the HFA is still large (0.66 R-M) when compared to the relative size of the induced magnetosphere. Given the associated order of magnitude decrease in solar wind dynamic pressure (411 pPa double right arrow 70 pPa), we find that HFAs at Mars have the potential to directly impact the topside ionosphere. We thus hypothesize that the loss of a planetary magnetic dynamo left Mars far more vulnerable to the pressure pulses resulting from HFAs and related foreshock transients.
Geology Geosciences, Multidisciplinary Physical Sciences Science & Technology

Details

Metrics

Logo image