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Massachusetts Institute of Technology

Evaluating the trend and impact factors of Southeast Asian monsoon

Abstract

dc:description.abstract

As a global leading agricultural producer, Southeast Asian (SEA) economy and livelihood rely on water supply from the monsoon precipitation during the rainy season. However, SEA monsoon system is still understudied. Here, we focus on the Mainland SEA monsoon because of its geographical simplicity. We find that the total precipitation of the Mainland SEA monsoon has experienced a reversing trend from a four-decade-long drying by 0.18 mm day-1 decade-1 to increasing by 0.13 day-1 decade-1 starting from 1989. The increased energy and moisture post-reversal comes from the strengthened Hadley and Walker cell due to the increasing meridional equivalent potential temperature ([theta]e) gradient. The meridional [theta]e gradient shows significant correlation with the precipitation time-series at r = 0.52 (p = 0.0015), despite [theta]e gradient has reversed ahead of precipitation for 4-5 years. Even though the overall precipitation trend of Mainland SEA in recent decades is increasing, the north of Myanmar and the south of China shows a decreasing trend. The surface wind analysis shows that surface southwesterly is weakening in the Northern Hemisphere, so the north of Mainland SEA receives less moisture, but also allow more moisture from the South China Sea to access the south of Mainland SEA. The surface wind change also corresponds with the rising branch of Hadley cell shifting southward. Lastly, we find that the Mainland SEA monsoon is a mixed convection system, composing of deep, moist convection directly over the region at 10-20°N, and a shallow, dry convection just north of the region at 35°, aligning with further assessment using zonal-mean precipitation, [theta], and [theta]e,. The deep, moist convection coincides with the zonal-mean [theta]e peak. The shallow, dry convection coincides with the zonal-mean [theta] peak.

Degree

thesis:*
Department dc:contributor.department
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences.
Grantor dc:publisher
Massachusetts Institute of Technology
Year dc:date.issued
2018

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Panasawatwong, Warittha
Advisor dc:contributor.advisor
  • Chien Wang.

Subjects

dc:subject × 1

Rights

dc:rights
Statement dc:rights
  • MIT theses are protected by copyright. They may be viewed, downloaded, or printed from this source but further reproduction or distribution in any format is prohibited without written permission.
Language dc:language.iso
eng

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/1721.1/119993
OAI identifier oai:identifier
oai:dspace.mit.edu:1721.1/119993

Chain of custody

source
Harvested from
MIT
Base URL
dspace.mit.edu/oai/request
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
citation

Panasawatwong, Warittha. Evaluating the trend and impact factors of Southeast Asian monsoon. Massachusetts Institute of Technology, 2018. http://hdl.handle.net/1721.1/119993