Climatology Definition of the Myanmar Southwest Monsoon (MSwM): Change Point Index (CPI)

Myanmar’s climate is heavily influenced by its geographic location and relief. Located between the Indian summer monsoon (ISM) and the East Asian summer monsoon (EASM), Myanmar’s climate is distinguished by the alternation of seasons known as the monsoon. The north-south direction of peaks and valle...

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Main Author: Kyaw Than Oo
Format: Article
Language:English
Published: Hindawi Limited 2023-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2023/2346975
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author Kyaw Than Oo
author_facet Kyaw Than Oo
author_sort Kyaw Than Oo
collection DOAJ
description Myanmar’s climate is heavily influenced by its geographic location and relief. Located between the Indian summer monsoon (ISM) and the East Asian summer monsoon (EASM), Myanmar’s climate is distinguished by the alternation of seasons known as the monsoon. The north-south direction of peaks and valleys creates a pattern of alternate zones of heavy and scanty precipitation during both the northeast and southwest monsoons. The majority of the rainfall has come from Myanmar’s southwest monsoon (MSwM), which is Myanmar’s rainy season (summer in global terms, June–September). This study explained both threshold-based and nonthreshold-based objective definitions of the onset and withdrawal of large-scale MSwM. The seasonal transitions in MSwM circulation and precipitation are convincingly represented by the new index, which is based on change point detection of the atmospheric moisture flow converging in the MSwM region (10–28 N, 92–102 E). A transition in vertically integrated moisture transport (VIMT), the reversal of surface winds, and an increase in precipitation may also be considered when defining MSwM onset objectively. We also define a change point of the MSwM (CPI) index for MSwM onset and withdrawal dates. The climatological mean onset of MSwM is day 135 (May 14), withdrawal is day 278 (October 4), and the total season length is 144 days. We are investigating spatial patterns of rainfall progression at and after the start of the monsoon, rather than transitions within a single region of the MSwM. The local southwest monsoon duration is well correlated with the CPI duration on interannual timescales, particularly in the peak rainfall regions, with a delay (advance) in large-scale onset or withdrawal associated with a delay (advance) of onset or withdrawal by local index. Hence, the next phase of this research is to study the maintenance and break of the monsoon to understand the underlying physical processes governing the monsoon circulation. The results of this study provide a possibility to reconstruct Myanmar’s monsoon climate dynamics, and the findings of this study can help unravel many remaining questions regarding the greater Asian monsoon system’s variability.
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spelling doaj.art-b91d4843fa964590b9d3d848a19e9fbf2023-02-06T01:40:48ZengHindawi LimitedAdvances in Meteorology1687-93172023-01-01202310.1155/2023/2346975Climatology Definition of the Myanmar Southwest Monsoon (MSwM): Change Point Index (CPI)Kyaw Than Oo0Nanjing University of Information Science and TechnologyMyanmar’s climate is heavily influenced by its geographic location and relief. Located between the Indian summer monsoon (ISM) and the East Asian summer monsoon (EASM), Myanmar’s climate is distinguished by the alternation of seasons known as the monsoon. The north-south direction of peaks and valleys creates a pattern of alternate zones of heavy and scanty precipitation during both the northeast and southwest monsoons. The majority of the rainfall has come from Myanmar’s southwest monsoon (MSwM), which is Myanmar’s rainy season (summer in global terms, June–September). This study explained both threshold-based and nonthreshold-based objective definitions of the onset and withdrawal of large-scale MSwM. The seasonal transitions in MSwM circulation and precipitation are convincingly represented by the new index, which is based on change point detection of the atmospheric moisture flow converging in the MSwM region (10–28 N, 92–102 E). A transition in vertically integrated moisture transport (VIMT), the reversal of surface winds, and an increase in precipitation may also be considered when defining MSwM onset objectively. We also define a change point of the MSwM (CPI) index for MSwM onset and withdrawal dates. The climatological mean onset of MSwM is day 135 (May 14), withdrawal is day 278 (October 4), and the total season length is 144 days. We are investigating spatial patterns of rainfall progression at and after the start of the monsoon, rather than transitions within a single region of the MSwM. The local southwest monsoon duration is well correlated with the CPI duration on interannual timescales, particularly in the peak rainfall regions, with a delay (advance) in large-scale onset or withdrawal associated with a delay (advance) of onset or withdrawal by local index. Hence, the next phase of this research is to study the maintenance and break of the monsoon to understand the underlying physical processes governing the monsoon circulation. The results of this study provide a possibility to reconstruct Myanmar’s monsoon climate dynamics, and the findings of this study can help unravel many remaining questions regarding the greater Asian monsoon system’s variability.http://dx.doi.org/10.1155/2023/2346975
spellingShingle Kyaw Than Oo
Climatology Definition of the Myanmar Southwest Monsoon (MSwM): Change Point Index (CPI)
Advances in Meteorology
title Climatology Definition of the Myanmar Southwest Monsoon (MSwM): Change Point Index (CPI)
title_full Climatology Definition of the Myanmar Southwest Monsoon (MSwM): Change Point Index (CPI)
title_fullStr Climatology Definition of the Myanmar Southwest Monsoon (MSwM): Change Point Index (CPI)
title_full_unstemmed Climatology Definition of the Myanmar Southwest Monsoon (MSwM): Change Point Index (CPI)
title_short Climatology Definition of the Myanmar Southwest Monsoon (MSwM): Change Point Index (CPI)
title_sort climatology definition of the myanmar southwest monsoon mswm change point index cpi
url http://dx.doi.org/10.1155/2023/2346975
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