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Robert M. Haberle

Researcher at Ames Research Center

Publications -  195
Citations -  13491

Robert M. Haberle is an academic researcher from Ames Research Center. The author has contributed to research in topics: Mars Exploration Program & Atmosphere of Mars. The author has an hindex of 58, co-authored 192 publications receiving 12240 citations. Previous affiliations of Robert M. Haberle include California Institute of Technology & University of Washington.

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Context Camera Investigation on board the Mars Reconnaissance Orbiter

TL;DR: The Context Camera (CTX) on the Mars Reconnaissance Orbiter (MRO) is a Facility Instrument (i.e., government-furnished equipment operated by a science team not responsible for design and fabrication) designed, built, and operated by Malin Space Science Systems and the MRO Mars Color Imager team (MARCI) as mentioned in this paper.
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The Mars Pathfinder atmospheric structure investigation/meteorology (ASI/MET) experiment

TL;DR: The Mars Pathfinder atmospheric structure investigation/meteorology (ASI/MET) experiment measured the vertical density, pressure, and temperature structure of the martian atmosphere from the surface to 160 km, and monitored surface meteorology and climate for 83 sols.
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Simulations of the Atmospheres of Synchronously Rotating Terrestrial Planets Orbiting M Dwarfs: Conditions for Atmospheric Collapse and the Implications for Habitability☆

TL;DR: In this article, the authors present results of three-dimensional simulations of the atmospheres of such planets, and comment on their possible habitability, concluding that these planets orbiting M stars can support atmospheres over a large range of conditions and, despite constraints such as stellar activity, are very likely to be habitable.
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Formation of Glaciers on Mars by Atmospheric Precipitation at High Obliquity

TL;DR: High-resolution climate simulations performed with a model designed to simulate the present-day Mars water cycle but assuming a 45° obliquity points to an atmospheric origin for the ice and reveals how precipitation could have formed glaciers on Mars.