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Global NDVI Patterns in Response to Atmospheric Water Vapor Anomalies over the Indo-Pacific Warm Pool during April-June
Wang, Zhaosheng1; Huang, Mei1; Wang, Rong2; Wang, Shaoqiang1,3; Liu, Xiaodong4; Xie, Xiaoning4; Liu, Zhengjia5; Gong, He1; Hao, Man6
通讯作者Huang, Mei(huangm@igsnrr.ac.cn)
2019-02-01
发表期刊JOURNAL OF CLIMATE
ISSN0894-8755
卷号32期号:4页码:1167-1180
摘要Vertically integrated atmospheric water vapor (VIWV) over the Indo-Pacific warm pool (IPWP) indirectly affects terrestrial vegetation growth (TVG) patterns through atmospheric water vapor transmission. However, their linkages and mechanisms are poorly understood. This study intends to understand the contributions of VIWVIPWP to TVG and the mechanisms by which VIWVIPWP impacts TVG. Combining monthly SST, VIWV, and NDVI data from 1982 to 2015, the linkage between VIWVIPWP and NDVI is investigated during April-June (AMJ). A strong correlation between VIWVIPWP and NDVI suggests that VIWVIPWP is an important factor affecting TVG. A composite analysis of VIWVIPWP anomalies and their relation to NDVI patterns shows that VIWVIPWP positively influences the NDVI of 68.1% of global green land during high-VIWVIPWP years but negatively influences 74.7% in low years. Corresponding to these results, during high-VIWVIPWP years, the warm and humid terrestrial climate conditions improved TVG by 9% and 2% in the Northern and Southern Hemispheres, respectively, but cold and dry conditions inhibited TVG for both hemispheres during the low years. Additionally, strong spatial correlations between VIWVIPWP and precipitation imply that VIWVIPWP affects the spatial-temporal pattern of precipitation. There is a stronger interaction between the Pacific north-south ridge and the two land troughs during high-VIWVIPWP years than during low-VIWVIPWP years. The zonally averaged wind at 850 hPa and VIWV results indicate that, during high-VIWVIPWP years, the enhanced wind from the ocean brings more atmospheric water vapor to land, increasing the probability of precipitation and resulting in moist climate conditions that promote AMJ vegetation growth. In brief, VIWVIPWP indirectly induces vegetation growth by affecting the distributions of terrestrial VIWV and precipitation.
关键词Atmosphere-land interaction Biosphere-atmosphere interaction Ecosystem effects Geographic information systems (GIS) Vegetation-atmosphere interactions
DOI10.1175/JCLI-D-18-0381.1
关键词[WOS]VEGETATION ACTIVITY ; WESTERN PACIFIC ; TEMPERATURE ; HYDROCLIMATE ; IMPACTS ; SCALE ; CHINA ; CLOUD
收录类别SCI ; SCI
语种英语
资助项目National Key R&D Program of China[2017YFC0503905] ; National Natural Science Foundation of China[41801082]
WOS研究方向Meteorology & Atmospheric Sciences
项目资助者National Key R&D Program of China ; National Natural Science Foundation of China
WOS类目Meteorology & Atmospheric Sciences
WOS记录号WOS:000457325500006
出版者AMER METEOROLOGICAL SOC
引用统计
被引频次:4[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.ieecas.cn/handle/361006/14359
专题古环境研究室
通讯作者Huang, Mei
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing, Peoples R China
2.Tianshui Normal Univ, Coll Resources & Environm Engn, Tianshui, Gansu, Peoples R China
3.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing, Peoples R China
4.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Shaanxi, Peoples R China
5.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing, Peoples R China
6.Jinan Environm Res Inst, Jinan, Shangdong, Peoples R China
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Wang, Zhaosheng,Huang, Mei,Wang, Rong,et al. Global NDVI Patterns in Response to Atmospheric Water Vapor Anomalies over the Indo-Pacific Warm Pool during April-June[J]. JOURNAL OF CLIMATE,2019,32(4):1167-1180.
APA Wang, Zhaosheng.,Huang, Mei.,Wang, Rong.,Wang, Shaoqiang.,Liu, Xiaodong.,...&Hao, Man.(2019).Global NDVI Patterns in Response to Atmospheric Water Vapor Anomalies over the Indo-Pacific Warm Pool during April-June.JOURNAL OF CLIMATE,32(4),1167-1180.
MLA Wang, Zhaosheng,et al."Global NDVI Patterns in Response to Atmospheric Water Vapor Anomalies over the Indo-Pacific Warm Pool during April-June".JOURNAL OF CLIMATE 32.4(2019):1167-1180.
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