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DOI10.1126/science.1159649
The global atmospheric circulation on moist isentropes
Pauluis O.; Czaja A.; Korty R.
发表日期2008
ISSN0036-8075
起始页码1075
结束页码1078
卷号321期号:5892
英文摘要The global atmospheric circulation transports energy from the equatorial regions to higher latitudes through a poleward flow of high-energy and -entropy parcels and an equatorward flow of air with lower energy and entropy content. Because of its turbulent nature, this circulation can only be described in some averaged sense. Here, we show that the total mass transport by the circulation is twice as large when averaged on moist isentropes than when averaged on dry isentropes. The additional mass transport on moist isentropes corresponds to a poleward flow of warm moist air near Earth's surface that rises into the upper troposphere within mid-latitudes and accounts for up to half of the air in the upper troposphere in polar regions.
英文关键词atmospheric circulation; atmospheric transport; energy; entropy; equatorial dynamics; polar region; troposphere; airflow; article; atmospheric pressure; energy transfer; entropy; moisture; priority journal; troposphere
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/245015
作者单位Courant Institute of Mathematical Sciences, New York University, 251 Mercer Street, New York, NY 10012, United States; Space and Atmospheric Physics Group, Department of Physics, Imperial College, London SW7 2AZ, United Kingdom; Department of Atmospheric Sciences, Texas A and M University, 3150 TAMU, College Station, TX 77843-3150, United States
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Pauluis O.,Czaja A.,Korty R.. The global atmospheric circulation on moist isentropes[J],2008,321(5892).
APA Pauluis O.,Czaja A.,&Korty R..(2008).The global atmospheric circulation on moist isentropes.Science,321(5892).
MLA Pauluis O.,et al."The global atmospheric circulation on moist isentropes".Science 321.5892(2008).
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