火星探测计划
大气(单位)
天体生物学
火星大气层
极地的
大气科学
南半球
红外光谱学
光谱学
北半球
水蒸气
谱线
环境科学
红外线的
地质学
物理
天文
气象学
气候学
火星人
量子力学
作者
Rudolf Hanel,B. J. Conrath,W. A. Hovis,V. G. Kunde,Paul D. Lowman,J. C. Pearl,C. Prabhakara,B. Schlachman,G. V. Levin
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:1972-01-21
卷期号:175 (4019): 305-308
被引量:93
标识
DOI:10.1126/science.175.4019.305
摘要
The Mariner 9 infrared spectroscopy experiment has provided goodquality spectra of many areas of Mars, predominantly in the southern hemisphere. Large portions of the thermal emission spectra are significantly affected by dust with a silicon oxide content approximately corresponding to that of an intermediate igneous rock, thus implying that Mars has undergone substantial geochemical differentiation. Derived temperature profiles indicate a warm daytime upper atmosphere with a strong warming over the south polar cap. Atmospheric water vapor is clearly observed over the south polar area and less strongly over other regions.
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