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MAVEN and the total electron content of the Martian ionosphere
被引:13
|作者:
Mendillo, Michael
[1
]
Narvaez, Clara
[1
]
Vogt, Marissa F.
[1
]
Mayyasi, Majd
[1
]
Mahaffy, Paul
[2
]
Benna, Mehdi
[2
]
Andersson, Laila
[3
]
Campbell, Bruce
[4
]
Nemec, Frantisek
[5
]
Ma, Ying Juan
[6
]
Chaufray, Jean-Yves
[7
]
Leblanc, Francois
[7
]
Gonzalez-Galindo, Francisco
[8
]
Lopez-Valverde, Miguel Angel
[8
]
Forget, Francois
[9
]
Jakosky, Bruce
[3
]
机构:
[1] Boston Univ, Ctr Space Phys, Boston, MA 02215 USA
[2] NASA, Goddard Space Flight Ctr, Greenbelt, MD USA
[3] Univ Colorado, LASP, Boulder, CO 80309 USA
[4] Smithsonian Inst, Washington, DC 20560 USA
[5] Charles Univ Prague, Fac Math & Phys, Prague, Czech Republic
[6] Univ Calif Los Angeles, Dept Earth & Planetary Sci, Los Angeles, CA USA
[7] Univ Paris 06, Sorbonne Univ, CNRS, UVSQ,UPMC,LATMOS IPSL, Paris, France
[8] CSIC, Inst Astrofis Andalucia, Granada, Spain
[9] CNRS, Lab Meteorol, Dynam, Paris, France
关键词:
total electron content;
Mars;
MAVEN;
ionosphere;
MARS IONOSPHERE;
ION ESCAPE;
SUBSURFACE;
RADAR;
DENSITY;
MODEL;
D O I:
10.1002/2016JA023474
中图分类号:
P1 [天文学];
学科分类号:
0704 ;
摘要:
Model studies of the ionosphere of Mars under daytime conditions reveal that for solar zenith angles of 0 degrees-40 degrees, the shapes and magnitudes of the electron density profiles N-e(h) change by only small amounts. This suggests that midday observations made by MAVEN instruments along slanted orbit segments can be used to represent vertical profiles. The total electron content (TEC), defined as the height integral of N-e(h), is a measure of the cold plasma reservoir of the Martian ionosphere. During MAVEN's Deep-Dip-#2 campaign of April 2015, observations of total ion density by Neutral Gas and Ion Mass Spectrometer and electron density by Langmuir Probe and Waves from periapse (similar to 130km) to 400 km were used to form <TEC>(topside)-validated by independent diagnostics and models. Orbit-by-orbit changes in topside TEC were then used to assess the magnitudes of plasma escape associated with both large and small changes in the topside slope of N-e(h)-called an "ionopause episode." The TEC changes due to these episodes, generalized to a global change, resulted in an escape flux of similar to 3-6x10(24)ions/s, an escape rate consistent with prior observation by Phobos-2, Mars Express, and MAVEN's own in situ studies.
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页码:3526 / 3537
页数:12
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