The global atmospheric circulation on moist isentropes

Science
Olivier PauluisRobert Korty

Abstract

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.

Citations

May 5, 2010·Proceedings of the National Academy of Sciences of the United States of America·Steven C Sherwood, Matthew Huber
Apr 7, 2010·Philosophical Transactions of the Royal Society of London. Series B, Biological Sciences·Wei Wu, Yangang Liu
Apr 9, 2009·Food and Chemical Toxicology : an International Journal Published for the British Industrial Biological Research Association·M MiragliaA Vespermann
Sep 13, 2016·Proceedings. Mathematical, Physical, and Engineering Sciences·Geoffrey K Vallis

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