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DOI | 10.1007/s00382-019-04951-6 |
Roles of land-surface properties and terrains on Maritime Continent rainfall and its seasonal evolution | |
Zhang T.; Tam C.-Y.; Jiang X.; Yang S.; Lau N.-C.; Chen J.; Laohalertchai C. | |
发表日期 | 2019 |
ISSN | 0930-7575 |
起始页码 | 6681 |
结束页码 | 6697 |
卷号 | 53期号:11 |
英文摘要 | The Maritime Continent (MC) is characterized by a seasonal evolution of rainfall distinct from other regions, due to its unique land–sea distribution and topography. In this study, the roles of surface properties and terrains in controlling the regional climatological rainfall were investigated, based on general circulation model experiments. Results show that the existence of terrain can increase the MC land (MCL) rainfall mainly through its dynamical lifting effect, but otherwise has only moderate influence on rainfall over the MC ocean (MCO). On the other hand, the impact of MC land–sea distribution on the regional rainfall is more seasonally dependent. When replacing the MC flat-land with ocean, rainfall is significantly increased over both MCL and MCO during boreal summer-to-fall, but not in the winter-to-spring season. Further inspection showed that by eliminating the MC flat-land, there is enhanced atmospheric water vapor and convective instability in the summer-to-fall period, contributing to a dramatic increase in precipitation. On the other hand, changes in convective instability and atmospheric water vapor over the MCL act to counteract each other, leading to an only moderate change in rainfall during boreal winter-to-spring. The model-based results suggest that this seasonally dependent influence of the MC flat-land on regional climate mean rainfall is not determined by its modulation on the diurnal cycle. Our results also suggest a larger sensitivity of model bias in representing land–sea distribution/fraction over the MC region during the dry season (i.e. boreal summer) than in the wet season (i.e. boreal winter). © 2019, Springer-Verlag GmbH Germany, part of Springer Nature. |
英文关键词 | Maritime Continent; Roles of land–sea distribution and terrains; Seasonally dependent features |
语种 | 英语 |
scopus关键词 | atmospheric convection; general circulation model; land surface; land-sea interaction; rainfall; seasonal variation; terrain; water vapor |
来源期刊 | Climate Dynamics |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/145810 |
作者单位 | Institute of Environment, Energy and Sustainability, The Chinese University of Hong Kong, Hong Kong; Earth System Science Programme, The Chinese University of Hong Kong, Hong Kong; Institute of Plateau Meteorology, China Meteorological Administration, 20 Guanghua Village Street, Qingyang District, Chengdu, Sichuan 610072, China; School of Atmospheric Sciences, Sun Yat-sen University, Guangzhou, Guangdong 510275, China; Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Sun Yat-sen University, Guangzhou, Guangdong 510275, China; Southern Laboratory of Ocean Science and Engineering (Guangdong, Zhuhai), Zhuhai, Guangdong 519000, China; Department of Geography and Resource Management, The Chinese University of Hong Kong, Sha Tin, Hong Kong; Thai Meteorological Department, Bangna, Bangkok, 10260, Thailand |
推荐引用方式 GB/T 7714 | Zhang T.,Tam C.-Y.,Jiang X.,et al. Roles of land-surface properties and terrains on Maritime Continent rainfall and its seasonal evolution[J],2019,53(11). |
APA | Zhang T..,Tam C.-Y..,Jiang X..,Yang S..,Lau N.-C..,...&Laohalertchai C..(2019).Roles of land-surface properties and terrains on Maritime Continent rainfall and its seasonal evolution.Climate Dynamics,53(11). |
MLA | Zhang T.,et al."Roles of land-surface properties and terrains on Maritime Continent rainfall and its seasonal evolution".Climate Dynamics 53.11(2019). |
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