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Tropical influences on southwest Asi...

Hoell, Andrew.

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Tropical influences on southwest Asia precipitation in a global atmospheric model.

Record Type:	Language materials, printed : Monograph/item
Title/Author:	Tropical influences on southwest Asia precipitation in a global atmospheric model./
Author:	Hoell, Andrew.
Description:	58 p.
Notes:	Adviser: Mathew Barlow.
Contained By:	Masters Abstracts International45-05.
Subject:	Atmospheric Sciences. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1442068

Tropical influences on southwest Asia precipitation in a global atmospheric model.
Hoell, Andrew.

Tropical influences on southwest Asia precipitation in a global atmospheric model. - 58 p.

Adviser: Mathew Barlow.

Thesis (M.S.)--University of Massachusetts Lowell, 2007.

The midlatitude dynamic and thermodynamic response to enhanced middle troposphere tropical diabatic heating over the eastern Indian Ocean during the northern hemisphere cold season (December--March) is investigated using the National Center for Atmospheric Research Community Atmosphere Model version 3.1 full global climate model. The dynamic response is similar to the idealized analytic Gill (1980) solution to steady diabatic heating and the thermodynamic response is consistent with theoretical works by Rodwell and Hoskins (1996, 2001) and observational analysis of Barlow et al. (2005). The thermodynamic response indicates that precipitation is suppressed by descending air over Iran, Afghanistan, and Pakistan due to cold temperature advection at middle and upper tropospheric levels. The sensitivity of the midlatitude response to diabatic heating is explored: the long-term steady state response, the short-term monthly response, and the response to variable magnitudes of diabatic heating.Subjects--Topical Terms:

1019179
Atmospheric Sciences.

Tropical influences on southwest Asia precipitation in a global atmospheric model.
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035 $a (UMI)AAI1442068
035 $a AAI1442068
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100 1 $a Hoell, Andrew. $3 1266314
245 1 0 $a Tropical influences on southwest Asia precipitation in a global atmospheric model.
300 $a 58 p.
500 $a Adviser: Mathew Barlow.
500 $a Source: Masters Abstracts International, Volume: 45-05, page: 2383.
502 $a Thesis (M.S.)--University of Massachusetts Lowell, 2007.
520 $a The midlatitude dynamic and thermodynamic response to enhanced middle troposphere tropical diabatic heating over the eastern Indian Ocean during the northern hemisphere cold season (December--March) is investigated using the National Center for Atmospheric Research Community Atmosphere Model version 3.1 full global climate model. The dynamic response is similar to the idealized analytic Gill (1980) solution to steady diabatic heating and the thermodynamic response is consistent with theoretical works by Rodwell and Hoskins (1996, 2001) and observational analysis of Barlow et al. (2005). The thermodynamic response indicates that precipitation is suppressed by descending air over Iran, Afghanistan, and Pakistan due to cold temperature advection at middle and upper tropospheric levels. The sensitivity of the midlatitude response to diabatic heating is explored: the long-term steady state response, the short-term monthly response, and the response to variable magnitudes of diabatic heating.
590 $a School code: 0111.
650 4 $a Atmospheric Sciences. $3 1019179
690 $a 0725
710 2 $a University of Massachusetts Lowell. $3 1017839
773 0 $t Masters Abstracts International $g 45-05.
790 $a 0111
790 1 0 $a Barlow, Mathew, $e advisor
791 $a M.S.
792 $a 2007
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1442068