TY - JOUR
T1 - Dust storm and electron density in the equatorial D region ionosphere of Mars
T2 - Comparison with Earth's ionosphere from rocket measurements in Brazil
AU - Haider, S. A.
AU - Batista, I. S.
AU - Abdu, M. A.
AU - Muralikrishna, P.
AU - Shah, Siddhi Y.
AU - Kuroda, T.
N1 - Funding Information:
Authors are thankful to MGS and Mars Odyssey data team and M.D. Smith (Michael.d.smith@nasa.gov) for providing the data for this work. Authors also acknowledge MCD team of E. Millour (ehouarn.millour@lmd.jussieu.fr) for providing freely accessible Mars Climate Data (http://www-mars.lmd.jussieu.fr). One of the authors, S.A. Haider, also thanks FAPESP for support through visiting scientist fellowship by the process 2014/2199S-3 to work at INPE, Brazil.
Publisher Copyright:
©2015. American Geophysical Union. All Rights Reserved.
PY - 2015/10/1
Y1 - 2015/10/1
N2 - We report the first model result for the dust densities and electron densities in the D region ionosphere of Mars for aerosol particles of different sizes during a major dust storm that occurred in Martian Year (MY) 25 at low latitude. These calculations are made at latitude 10S and solar longitudes (Ls) = 200, 220, 250, and 280 for high, medium, low, and absence of dust storms, respectively. Four corresponding dust layers were found at 50 km, 50 km, 38 km, and 25 km during these events. During high dust storm period, the optical depth and dust density increased by a factor of ~20 from its normal condition. The electron densities estimated for the D region ionosphere of Mars for submicron sized dust particles are largest as compared to that estimated for larger particles. The electron density reduced by ~2 orders of magnitude during high dust storm. The estimated electron density in the clear atmosphere of Mars is compared with measurements of Earth's ionosphere at nearly the same geophysical condition.
AB - We report the first model result for the dust densities and electron densities in the D region ionosphere of Mars for aerosol particles of different sizes during a major dust storm that occurred in Martian Year (MY) 25 at low latitude. These calculations are made at latitude 10S and solar longitudes (Ls) = 200, 220, 250, and 280 for high, medium, low, and absence of dust storms, respectively. Four corresponding dust layers were found at 50 km, 50 km, 38 km, and 25 km during these events. During high dust storm period, the optical depth and dust density increased by a factor of ~20 from its normal condition. The electron densities estimated for the D region ionosphere of Mars for submicron sized dust particles are largest as compared to that estimated for larger particles. The electron density reduced by ~2 orders of magnitude during high dust storm. The estimated electron density in the clear atmosphere of Mars is compared with measurements of Earth's ionosphere at nearly the same geophysical condition.
KW - D region ionospheres of Earth and Mars
KW - dusty ionosphere of Mars
KW - modeling of dust density
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U2 - 10.1002/2015JA021630
DO - 10.1002/2015JA021630
M3 - Article
AN - SCOPUS:84954367255
SN - 2169-9380
VL - 120
SP - 8968
EP - 8977
JO - Journal of Geophysical Research: Space Physics
JF - Journal of Geophysical Research: Space Physics
IS - 10
ER -