Climate Variability in Monsoon and Arid Regions Attributable to Dynamic Vegetation in a Global Climate Model | |
Wang, Hongli2,3; Qiu, Linjing4; Xie, Xiaoning3; Wang, Zhiyuan1,5; Liu, Xiaodong3,4 | |
刊名 | JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN |
2018 | |
卷号 | 96期号:4页码:391-403 |
关键词 | dynamic vegetation monsoon region arid region climate variability East Asian monsoon |
ISSN号 | 0026-1165 |
DOI | 10.2151/jmsj.2018-047 |
通讯作者 | Qiu, Linjing(qiulinjing@mail.xjtu.edu.cn) |
英文摘要 | The climate variability in monsoon and arid regions attributable to dynamic vegetation is investigated using NCAR's Community Earth System Model with the Dynamic Global Vegetation Model. Two present climate simulations, one using dynamics and the other using fixed vegetation cover, are carried out. A comparative analysis of the two simulations reveals that the climate in monsoon and arid regions exhibits different responses to dynamic vegetation. On the hemispheric scale, precipitation mainly increases in the Northern hemisphere and decreases in the Southern Hemisphere in response to dynamic vegetation, while the surface temperature exhibits a consistent decrease. On the regional scale, precipitation decreases caused by dynamic vegetation are the main trend in monsoon regions except for the Asian monsoon region, while precipitation responses to vegetation change are weak in arid regions relative to monsoon regions. The surface temperature increases significantly because of dynamic vegetation only in the boreal winter Asian monsoon region, while the rest of the monsoon and arid regions mainly exhibit reduced surface temperatures. Therefore, the climate variability in the Asian monsoon region is clearly different from the other regions. Further analysis shows that dynamic vegetation can modulate variations in the east-west sea-level pressure gradient and lower-level meridional winds in East Asia, and it can strengthen (weaken) the Fast Asian summer (winter) monsoon. Mechanistic analysis reveals that the difference in hemispheric and regional climate variations may be due to changes in the dynamic vegetation-induced moisture flux and net surface radiative forcing. |
资助项目 | National Natural Science Foundation of China[31741020] ; National Natural Science Foundation of China[41301223] ; National Natural Science Foundation of China[41690115] ; Natural Science Basic Research Plan of Shaanxi Province[2015JQ4109] ; Science Research Project of Shaanxi Radio and TV University[15D-08-A01] |
WOS关键词 | INTERANNUAL VARIABILITY ; PRECIPITATION ; FEEDBACKS ; CO2 ; TERRESTRIAL ; IMPACTS ; SYSTEM |
WOS研究方向 | Meteorology & Atmospheric Sciences |
语种 | 英语 |
出版者 | METEOROLOGICAL SOC JAPAN |
WOS记录号 | WOS:000451216100001 |
资助机构 | National Natural Science Foundation of China ; Natural Science Basic Research Plan of Shaanxi Province ; Science Research Project of Shaanxi Radio and TV University |
内容类型 | 期刊论文 |
源URL | [http://ir.ieecas.cn/handle/361006/14546] |
专题 | 地球环境研究所_古环境研究室 |
通讯作者 | Qiu, Linjing |
作者单位 | 1.Nanjing Univ Informat Sci & Technol, Climate Dynam Res Ctr, Nanjing, Jiangsu, Peoples R China 2.Shaanxi Radio & TV Univ, Xian, Shaanxi, Peoples R China 3.Chinese Acad Sci, Inst Earth Environm, SKLLQG, Beijing, Peoples R China 4.Xi An Jiao Tong Univ, Sch Human Settlements & Civil Engn, 99 Yanxiang Rd, Xian 710049, Shaanxi, Peoples R China 5.Nanjing Univ Informat Sci & Technol, Earth Syst Modeling Ctr, Nanjing, Jiangsu, Peoples R China |
推荐引用方式 GB/T 7714 | Wang, Hongli,Qiu, Linjing,Xie, Xiaoning,et al. Climate Variability in Monsoon and Arid Regions Attributable to Dynamic Vegetation in a Global Climate Model[J]. JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN,2018,96(4):391-403. |
APA | Wang, Hongli,Qiu, Linjing,Xie, Xiaoning,Wang, Zhiyuan,&Liu, Xiaodong.(2018).Climate Variability in Monsoon and Arid Regions Attributable to Dynamic Vegetation in a Global Climate Model.JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN,96(4),391-403. |
MLA | Wang, Hongli,et al."Climate Variability in Monsoon and Arid Regions Attributable to Dynamic Vegetation in a Global Climate Model".JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN 96.4(2018):391-403. |
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