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MM5 simulation of transport patterns...

Kasakseh, Shoukri J. S.

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MM5 simulation of transport patterns during a Middle-East summer ozone period.

Record Type:	Language materials, printed : Monograph/item
Title/Author:	MM5 simulation of transport patterns during a Middle-East summer ozone period./
Author:	Kasakseh, Shoukri J. S.
Description:	80 p.
Notes:	Adviser: Robert Bornstein.
Contained By:	Masters Abstracts International45-02.
Subject:	Atmospheric Sciences. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1438572
ISBN:	9780542919015

MM5 simulation of transport patterns during a Middle-East summer ozone period.
Kasakseh, Shoukri J. S.

MM5 simulation of transport patterns during a Middle-East summer ozone period. - 80 p.

Adviser: Robert Bornstein.

Thesis (M.S.)--San Jose State University, 2006.

Meteorological conditions over the West Bank, Gaza, and Israel were studied during average-summertime surface-O3 conditions. MM5 was run with three nested domains (min grid spacing of 1.67 km). Minimum biases resulted when MM5 input deep soil temperature was lowered by 9°C and its soil moisture content was capped at 10%. MM5 surface flow patterns correctly reproduced the observed diurnal variation of coastal and slope flows.

ISBN: 9780542919015Subjects--Topical Terms:

1019179
Atmospheric Sciences.

MM5 simulation of transport patterns during a Middle-East summer ozone period.
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020 $a 9780542919015
035 $a (UMI)AAI1438572
035 $a AAI1438572
040 $a UMI $c UMI
100 1 $a Kasakseh, Shoukri J. S. $3 1291339
245 1 0 $a MM5 simulation of transport patterns during a Middle-East summer ozone period.
300 $a 80 p.
500 $a Adviser: Robert Bornstein.
500 $a Source: Masters Abstracts International, Volume: 45-02, page: 0798.
502 $a Thesis (M.S.)--San Jose State University, 2006.
520 $a Meteorological conditions over the West Bank, Gaza, and Israel were studied during average-summertime surface-O3 conditions. MM5 was run with three nested domains (min grid spacing of 1.67 km). Minimum biases resulted when MM5 input deep soil temperature was lowered by 9°C and its soil moisture content was capped at 10%. MM5 surface flow patterns correctly reproduced the observed diurnal variation of coastal and slope flows.
520 $a The 700 hPa flow was dominated by the Azores High and a low-pressure center north of the area, while surface interactions involved the High and the Persian Low. As the Low was only north of the study area, surface O3 did not approach episode levels. The observed O 3 peak occurred at 1100 LST near the coast. While this peak is several hours earlier than at most other sites, simulations have shown a larger (and later) peak over Jordan due to emissions from a large coastal power plant.
590 $a School code: 6265.
650 4 $a Atmospheric Sciences. $3 1019179
650 4 $a Environmental Sciences. $3 676987
650 4 $a Geophysics. $3 535228
690 $a 0373
690 $a 0725
690 $a 0768
710 2 0 $a San Jose State University. $3 1020800
773 0 $t Masters Abstracts International $g 45-02.
790 $a 6265
790 1 0 $a Bornstein, Robert, $e advisor
791 $a M.S.
792 $a 2006
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1438572