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DOI | 10.1126/science.1080148 |
A sublimation model for Martian south polar ice features | |
Byrne S.; Ingersoll A.P. | |
发表日期 | 2003 |
ISSN | 0036-8075 |
起始页码 | 1051 |
结束页码 | 1053 |
卷号 | 299期号:5609 |
英文摘要 | In their pioneering work, Leighton and Murray argued that the Mars atmosphere, which at present is 95% carbon dioxide, is controlled by vapor equilibrium with a much larger polar reservoir of solid carbon dioxide. Here we argue that the polar reservoir is small and cannot function as a long-term buffer to the more massive atmosphere. Our work is based on modeling of the circular depressions commonly found on the south polar cap. We argue that a carbon dioxide ice layer about 8 meters thick is being etched away to reveal water ice underneath. This is consistent with thermal infrared data from the Mars Odyssey mission. |
英文关键词 | Carbon dioxide; Extraterrestrial atmospheres; Ice; Infrared radiation; Sublimation; Thermal effects; Vapors; Vapor equilibrium; Martian surface analysis; carbon dioxide; ice; water; carbon dioxide; ice; Mars; Martian atmosphere; polar region; arctic climate; article; atmosphere; experimental model; infrared radiation; priority journal; temperature; Atmosphere; Carbon Dioxide; Dry Ice; Ice; Mars; Models, Theoretical; Seasons; Temperature; Water |
语种 | 英语 |
来源期刊 | Science
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/243207 |
作者单位 | Division of Geological Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, United States |
推荐引用方式 GB/T 7714 | Byrne S.,Ingersoll A.P.. A sublimation model for Martian south polar ice features[J],2003,299(5609). |
APA | Byrne S.,&Ingersoll A.P..(2003).A sublimation model for Martian south polar ice features.Science,299(5609). |
MLA | Byrne S.,et al."A sublimation model for Martian south polar ice features".Science 299.5609(2003). |
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