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A Model Study on the Influence of Overshooting Convection on Ttl Water Vapour : Volume 10, Issue 7 (09/07/2010)

By Hassim, M. E. E.

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Book Id: WPLBN0003995486
Format Type: PDF Article :
File Size: Pages 39
Reproduction Date: 2015

Title: A Model Study on the Influence of Overshooting Convection on Ttl Water Vapour : Volume 10, Issue 7 (09/07/2010)  
Author: Hassim, M. E. E.
Volume: Vol. 10, Issue 7
Language: English
Subject: Science, Atmospheric, Chemistry
Collections: Periodicals: Journal and Magazine Collection (Contemporary), Copernicus GmbH
Historic
Publication Date:
2010
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

Citation

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Lane, T. P., & E. Hassi, M. E. (2010). A Model Study on the Influence of Overshooting Convection on Ttl Water Vapour : Volume 10, Issue 7 (09/07/2010). Retrieved from http://community.ebooklibrary.org/


Description
Description: School of Earth Sciences, The University of Melbourne, Melbourne, Victoria 3010, Australia. Overshooting deep convection that penetrates into the Tropical Tropopause Layer (TTL) is thought to have an important role in regulating the water vapour content of this region. Yet, the net effect of such convection and the dominant mechanisms remain unclear. This study uses two idealised three-dimensional cloud-resolving model simulations to examine the influence of overshooting convection on water vapour when it penetrates into two different TTL environments, one supersaturated and the other subsaturated with respect to ice. These simulations show that the overshooting convection plays a direct role in driving the ambient environment towards ice saturation through either net moistening (subsaturated TTL) or net dehydration (supersaturated TTL). Moreover, in these cases the extent of dehydration in supersaturated conditions is greater than the moistening in subsaturated conditions. With the aid of modelled passive tracers, the relative roles of transport, mixing and ice microphysics are assessed; ultimately, ice sublimation and scavenging processes play the most important role in defining the different TTL relative humidity tendencies. In addition, significant moistening in both cases is modelled well into the subsaturated tropical lower stratosphere (up to 450 K), even though the overshooting turrets only reach approximately 420 K. It is shown that this moistening is the result of jumping cirrus, which is induced by the localised upward transport and mixing of TTL air following the collapse of the overshooting turret.

Summary
A model study on the influence of overshooting convection on TTL water vapour

Excerpt
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