Martian Clouds Observed by Mars Global Surveyor Mars Orbiter Camera from Ls 135 to 310
By Huiqun Wang, A. Ingersoll. 2002
173 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics
View Paper: https://www.semanticscholar.org/paper/ea19e0099da5a18f856a9a8423573dc9bacb0f81
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In Astronomy and Astrophysics
- Francois Forget
- F. Montmessin
- A. Spiga
- R. Haberle
- Robert J. Wilson
- Mark Richardson
- Michael D. Smith
- D. Hinson
Citations in the corpus
- Observations of the south seasonal cap of Mars during recession in 2004–2006 by the OMEGA visible/near‐infrared imaging spectrometer on board Mars Express (2007, methodology): “The last three spectra are nearly superimposed over a period of nearly one month, which is consistent with a relatively clear atmosphere after the southern summer solstice in early afternoon [ Wang and Ingersoll, 2002 ].”
- Observations of the initiation and evolution of the 2001 Mars global dust storm (2005, methodology): “[10] Daily Global Map (DGM) images are obtained by both WA cameras as continuous strips on the day-side portion of each orbit [Wang and Ingersoll, 2002].”
- Origin and role of water ice clouds in the Martian water cycle as inferred from a general circulation model (2004, methodology): “[81] In contrast, streaks observed in the southern Polar Hood feature much thinner clouds, and their numbers are substantially lower than their northern counterparts [Wang and Ingersoll, 2002].”
- Temperature inversions, thermal tides, and water ice clouds in the Martian tropics (2003, background): “A prominent band of water ice clouds appears at latitudes of about 10� S–30� N during spring and summer of the Northern Hemisphere [e.g., Clancy et al., 1996; Smith et al., 2001b; Wang and Ingersoll, 2002; Smith, 2004].”
- A new model to simulate the Martian mesoscale and microscale atmospheric circulation: Validation and first results (2009, methodology): “[ 2 ] The Mars Global Surveyor (MGS) mission yielded unprecedented observations of Martian meteorological phenomena at various horizontal scales below 100 km [e.g., Wang and Ingersoll , 2002].”
- Spacecraft Observations of the Martian Atmosphere (2008, background): “He also thanks Bruce Cantor for images of dust storms from the MGS MOC camera, Paul Withers for temperature profiles obtained by the MER Spirit and Opportunity rovers during their descent through the atmosphere, and John Wilson for Viking IRTM temperatures.”