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The thermal stratification of the extratropical troposphere

Schneider, Tapio (2007) The thermal stratification of the extratropical troposphere. In: The Global Circulation of the Atmosphere. Princeton University Press , Princeton, NJ, pp. 47-77. ISBN 9780691121819. https://resolver.caltech.edu/CaltechAUTHORS:20160929-131829928

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Abstract

This chapter discusses the dynamical mechanisms responsible for the maintenance and variability of the extratropical thermal stratification and tropopause in the zonal mean. Figure 3.1 shows the zonal-mean temperature lapse rate of Earth’s atmosphere for boreal winter and summer. The zonal-mean lapse rate in the free troposphere is relatively uniform (about 6.5 K km^(−1) ) and varies only weakly with season — observations that motivated the assumption of a fixed thermal stratification in quasigeostrophic theory. Regions of smaller lapse rate (statically more stable stratification) are seen near the surface in the subtropics and in high latitudes, particularly in winter. At the tropopause, the lapse rate decreases, in many regions to zero or less, marking the transition from the troposphere to the more stably stratified stratosphere.


Item Type:Book Section
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http://press.princeton.edu/titles/8591.htmlPublisherBook Catalog
ORCID:
AuthorORCID
Schneider, Tapio0000-0001-5687-2287
Additional Information:© 2007 Princeton University Press.
Record Number:CaltechAUTHORS:20160929-131829928
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20160929-131829928
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:70668
Collection:CaltechAUTHORS
Deposited By: George Porter
Deposited On:30 Sep 2016 20:42
Last Modified:03 Oct 2019 16:00

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