Numerical weather simulation of the depression 23W over the Gulf of Thailand by the MM5

A numerical weather simulation of the depression 23W moving over the Gulf of Thailand during October 19-26, 2003 expressed in terms of meteorological variables including pressure, humidity, geopotential height, wind velocity, divergence, vertical velocity, vorticity and rain was performed by the fif...

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Main Authors: Jiemjai Kreasuwun, Chakrit Chotamonsak
Format: Article
Language:English
Published: Prince of Songkla University 2008-03-01
Series:Songklanakarin Journal of Science and Technology (SJST)
Subjects:
MM5
Online Access:http://rdo.psu.ac.th/sjst/ejournal/journal/30-2/0125-3395-30-2-257-267.pdf
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spelling doaj-fed9809562a546e58f62bd185297af882020-11-24T21:06:56ZengPrince of Songkla UniversitySongklanakarin Journal of Science and Technology (SJST)0125-33952008-03-01302257267Numerical weather simulation of the depression 23W over the Gulf of Thailand by the MM5Jiemjai KreasuwunChakrit ChotamonsakA numerical weather simulation of the depression 23W moving over the Gulf of Thailand during October 19-26, 2003 expressed in terms of meteorological variables including pressure, humidity, geopotential height, wind velocity, divergence, vertical velocity, vorticity and rain was performed by the fifth generation of PSN/NCAR mesoscale model, MM5 version 3.7. Favorable conditions for the storm development and storm center during its passage were indicated from the model simulation. The favorable weather conditions of the storm evolution were found to be high relative humidity of 90-100% and less than 1003 mb mean sea-level pressure. The central pressure of the storm decreased at the rate of at least 6 mb/24 hrs with the lowest value of 987 mb and the corresponding lowest geopotential height of 1326 m on October 22, 2003. Cyclonic flows were detected around the areas of negative horizontal divergence of -19.81 x 10-4 s-1 with gusts over 26 ms-1 and the positive vorticities of 128.4-234.1 x 10-4 s-1 along with moist air updrafts of 10-130 m/s. Continuous updrafts in an unstable atmosphere with adequate moisture supply enhanced the condensation process, and the cloud and rain formation, resulting in heavy rainfall in southern Thailand. Simulated rains are comparable with reported rains of 197-200 mm/24 hr at Prachuab Khiri Khan Province during October 24-25, 2003.http://rdo.psu.ac.th/sjst/ejournal/journal/30-2/0125-3395-30-2-257-267.pdfMM5numerical weather simulationdepressionthe Gulf of Thailand.
collection DOAJ
language English
format Article
sources DOAJ
author Jiemjai Kreasuwun
Chakrit Chotamonsak
spellingShingle Jiemjai Kreasuwun
Chakrit Chotamonsak
Numerical weather simulation of the depression 23W over the Gulf of Thailand by the MM5
Songklanakarin Journal of Science and Technology (SJST)
MM5
numerical weather simulation
depression
the Gulf of Thailand.
author_facet Jiemjai Kreasuwun
Chakrit Chotamonsak
author_sort Jiemjai Kreasuwun
title Numerical weather simulation of the depression 23W over the Gulf of Thailand by the MM5
title_short Numerical weather simulation of the depression 23W over the Gulf of Thailand by the MM5
title_full Numerical weather simulation of the depression 23W over the Gulf of Thailand by the MM5
title_fullStr Numerical weather simulation of the depression 23W over the Gulf of Thailand by the MM5
title_full_unstemmed Numerical weather simulation of the depression 23W over the Gulf of Thailand by the MM5
title_sort numerical weather simulation of the depression 23w over the gulf of thailand by the mm5
publisher Prince of Songkla University
series Songklanakarin Journal of Science and Technology (SJST)
issn 0125-3395
publishDate 2008-03-01
description A numerical weather simulation of the depression 23W moving over the Gulf of Thailand during October 19-26, 2003 expressed in terms of meteorological variables including pressure, humidity, geopotential height, wind velocity, divergence, vertical velocity, vorticity and rain was performed by the fifth generation of PSN/NCAR mesoscale model, MM5 version 3.7. Favorable conditions for the storm development and storm center during its passage were indicated from the model simulation. The favorable weather conditions of the storm evolution were found to be high relative humidity of 90-100% and less than 1003 mb mean sea-level pressure. The central pressure of the storm decreased at the rate of at least 6 mb/24 hrs with the lowest value of 987 mb and the corresponding lowest geopotential height of 1326 m on October 22, 2003. Cyclonic flows were detected around the areas of negative horizontal divergence of -19.81 x 10-4 s-1 with gusts over 26 ms-1 and the positive vorticities of 128.4-234.1 x 10-4 s-1 along with moist air updrafts of 10-130 m/s. Continuous updrafts in an unstable atmosphere with adequate moisture supply enhanced the condensation process, and the cloud and rain formation, resulting in heavy rainfall in southern Thailand. Simulated rains are comparable with reported rains of 197-200 mm/24 hr at Prachuab Khiri Khan Province during October 24-25, 2003.
topic MM5
numerical weather simulation
depression
the Gulf of Thailand.
url http://rdo.psu.ac.th/sjst/ejournal/journal/30-2/0125-3395-30-2-257-267.pdf
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