Drought and spring cooling induced recent decrease in vegetation growth in Inner Asia

被引:164
作者
Mohammat, Anwar [1 ]
Wang, Xuhui [2 ]
Xu, Xiangtao [2 ]
Peng, Liqing [2 ]
Yang, Yan [2 ]
Zhang, Xinping [2 ]
Myneni, Ranga B. [3 ]
Piao, Shilong [2 ,4 ]
机构
[1] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Key Lab Biogeog & Bioresources Arid Land, Urumqi 830011, Xinjiang, Peoples R China
[2] Peking Univ, Sino French Inst Earth Syst Sci, Coll Urban & Environm Sci, Beijing 100871, Peoples R China
[3] Boston Univ, Dept Geog & Environm, Boston, MA 02215 USA
[4] Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100085, Peoples R China
基金
中国国家自然科学基金;
关键词
Drought; Global warming; Spring cooling; NDVI; Vegetation growth; Inner Asia; PHOTOSYNTHETIC TRENDS; NORTH-AMERICA; CLIMATE; HEAT; RESPONSES; DATASET; BOREAL; INDEX;
D O I
10.1016/j.agrformet.2012.09.014
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
The response of vegetation growth to current climate change in Inner Asia (35-55 degrees N, 45-120 degrees E) was investigated by analyzing time series of the Normalized Difference Vegetation Index (NDVI) data from the Advanced Very High Resolution Radiometer (AVHRR) from 1982 to 2009. We found that at the regional scale, the greening trend observed during the 1980s was stalled in the 1990s. Different seasons, however, show different changes and mechanisms. Among the three seasons (spring, summer and autumn), summer has the earliest turning point (from greening to non-greening) in the early 1990s, as a result of summertime droughts, as indicated by Palmer Drought Severity Index (PDSI). Consistent with the change in summer NDVI, summer PDSI and precipitation significantly increased in the 1980s, but strongly decreased since the early 1990s at the regional scale. The negative effect of summer drought is particularly significant over dry regions such as eastern Kazakhstan, Mongolia and Inner Mongolia. However, in high altitude or high latitude regions (>50 degrees N), summer vegetation growth is more strongly correlated with summer temperature rather than with summer PDSI. In spring, changes in vegetation growth are closely linked with temperature changes rather than droughts. Both spring temperature and spring NDVI, for instance, increased until the late 1990s and then decreased. Statistical analyses also show that spring NDVI is significantly correlated with spring temperature at the regional scale (P < 0.05), implying that temperature is the dominant limiting factor for spring vegetation growth in most regions of Inner Asia except Turkmenistan and Uzbekistan, where spring PDSI shows significant positive correlation with spring NDVI. Further analyses of the response of vegetation to extreme high spring temperature in 1997 and extreme summer drought in 2001 exhibit a highly heterogeneous pattern. (c) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:21 / 30
页数:10
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