Sea breeze simulation over the Malay Peninsula in an intermonsoon period

This study presents a characteristic intermonsoon weather situation over the Malay Peninsula. The Coupled Ocean/Atmosphere Mesoscale Prediction System (COAMPS) is used to investigate the mesoscale details of the simulated sea breeze circulations over the Malay Peninsula on 23 April 2002. The occurre...

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Main Authors: Joseph, B., Koh, Tieh Yong., Chen, S., Bhatt, Bhuwan Chandra.
Format: Article
Language:English
Published: 2012
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Online Access:https://hdl.handle.net/10356/80111
http://hdl.handle.net/10220/8230
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-801112020-09-26T21:25:24Z Sea breeze simulation over the Malay Peninsula in an intermonsoon period Joseph, B. Koh, Tieh Yong. Chen, S. Bhatt, Bhuwan Chandra. DRNTU::Science::Geology This study presents a characteristic intermonsoon weather situation over the Malay Peninsula. The Coupled Ocean/Atmosphere Mesoscale Prediction System (COAMPS) is used to investigate the mesoscale details of the simulated sea breeze circulations over the Malay Peninsula on 23 April 2002. The occurrence of sea breeze collisions occurring in the inland region of the southern Malay Peninsula is noted. On the peninsulascale, convection was first initiated along the low-level convergence line that became established along the west coastal region of the Malay Peninsula in the early afternoon. Deep clouds that led to thunderstorms developed in the northwestern part of the Malay Peninsula after the sea breeze encountered the mountain wave induced under the ambient easterlies above the mountain ridge line. The convective activity was further enhanced over the central Malay Peninsula because of the interaction between sea breeze front and gap winds from the mountains. This case study suggests that the Malay Peninsula is a potentially fertile ground for many dynamically interesting case studies of land–sea breeze circulations. Published version 2012-06-21T03:10:14Z 2019-12-06T13:40:55Z 2012-06-21T03:10:14Z 2019-12-06T13:40:55Z 2008 2008 Journal Article Joseph, B., Bhatt, B. C., Koh, T. Y., & Chen, S. (2008). Sea breeze simulation over Malay Peninsula over an intermonsoon period. Journal of Geophysical Research, 113. https://hdl.handle.net/10356/80111 http://hdl.handle.net/10220/8230 10.1029/2008JD010319 en Journal of geophysical research © 2008 American Geophysical Union.This paper was published in Journal of Geophysical Research and is made available as an electronic reprint (preprint) with permission of American Geophysical Union. The paper can be found at the following official URL: [http://dx.doi.org/10.1029/2008JD010319]. One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law. 8 p. application/pdf
institution Nanyang Technological University
building NTU Library
country Singapore
collection DR-NTU
language English
topic DRNTU::Science::Geology
spellingShingle DRNTU::Science::Geology
Joseph, B.
Koh, Tieh Yong.
Chen, S.
Bhatt, Bhuwan Chandra.
Sea breeze simulation over the Malay Peninsula in an intermonsoon period
description This study presents a characteristic intermonsoon weather situation over the Malay Peninsula. The Coupled Ocean/Atmosphere Mesoscale Prediction System (COAMPS) is used to investigate the mesoscale details of the simulated sea breeze circulations over the Malay Peninsula on 23 April 2002. The occurrence of sea breeze collisions occurring in the inland region of the southern Malay Peninsula is noted. On the peninsulascale, convection was first initiated along the low-level convergence line that became established along the west coastal region of the Malay Peninsula in the early afternoon. Deep clouds that led to thunderstorms developed in the northwestern part of the Malay Peninsula after the sea breeze encountered the mountain wave induced under the ambient easterlies above the mountain ridge line. The convective activity was further enhanced over the central Malay Peninsula because of the interaction between sea breeze front and gap winds from the mountains. This case study suggests that the Malay Peninsula is a potentially fertile ground for many dynamically interesting case studies of land–sea breeze circulations.
format Article
author Joseph, B.
Koh, Tieh Yong.
Chen, S.
Bhatt, Bhuwan Chandra.
author_facet Joseph, B.
Koh, Tieh Yong.
Chen, S.
Bhatt, Bhuwan Chandra.
author_sort Joseph, B.
title Sea breeze simulation over the Malay Peninsula in an intermonsoon period
title_short Sea breeze simulation over the Malay Peninsula in an intermonsoon period
title_full Sea breeze simulation over the Malay Peninsula in an intermonsoon period
title_fullStr Sea breeze simulation over the Malay Peninsula in an intermonsoon period
title_full_unstemmed Sea breeze simulation over the Malay Peninsula in an intermonsoon period
title_sort sea breeze simulation over the malay peninsula in an intermonsoon period
publishDate 2012
url https://hdl.handle.net/10356/80111
http://hdl.handle.net/10220/8230
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