Arid
DOI10.1088/1748-9326/8/3/035033
Vegetation response to extreme climate events on the Mongolian Plateau from 2000 to 2010
John, Ranjeet1; Chen, Jiquan1,2; Ou-Yang, Zu-Tao1; Xiao, Jingfeng3; Becker, Richard1; Samanta, Arindam4; Ganguly, Sangram5,6; Yuan, Wenping7; Batkhishig, Ochirbat8
通讯作者John, Ranjeet
来源期刊ENVIRONMENTAL RESEARCH LETTERS
ISSN1748-9326
出版年2013
卷号8期号:3
英文摘要

Climate change has led to more frequent extreme winters (aka, dzud) and summer droughts on the Mongolian Plateau during the last decade. Among these events, the 2000-2002 combined summer drought-dzud and 2010 dzud were the most severe on vegetation. We examined the vegetation response to these extremes through the past decade across the Mongolian Plateau as compared to decadal means. We first assessed the severity and extent of drought using the Tropical Rainfall Measuring Mission (TRMM) precipitation data and the Palmer drought severity index (PDSI). We then examined the effects of drought by mapping anomalies in vegetation indices (EVI, EVI2) and land surface temperature derived from MODIS and AVHRR for the period of 2000-2010. We found that the standardized anomalies of vegetation indices exhibited positively skewed frequency distributions in dry years, which were more common for the desert biome than for grasslands. For the desert biome, the dry years (2000-2001, 2005 and 2009) were characterized by negative anomalies with peak values between -1.5 and -0.5 and were statistically different (P < 0.001) from relatively wet years (2003, 2004 and 2007). Conversely, the frequency distributions of the dry years were not statistically different (p < 0.001) from those of the relatively wet years for the grassland biome, showing that they were less responsive to drought and more resilient than the desert biome. We found that the desert biome is more vulnerable to drought than the grassland biome. Spatially averaged EVI was strongly correlated with the proportion of land area affected by drought (PDSI < -1) in Inner Mongolia (IM) and Outer Mongolia (OM), showing that droughts substantially reduced vegetation activity. The correlation was stronger for the desert biome (R-2 = 65 and 60, p < 0.05) than for the IM grassland biome (R-2 = 53, p < 0.05). Our results showed significant differences in the responses to extreme climatic events (summer drought and dzud) between the desert and grassland biomes on the Plateau.


英文关键词Mongolian Plateau vegetation indices extreme climate drought land surface temperature MODIS EVI EVI2 dzud
类型Article
语种英语
国家USA ; Peoples R China ; Mongolia
收录类别SCI-E
WOS记录号WOS:000325247100078
WOS关键词ATMOSPHERIC CIRCULATION ; INNER-MONGOLIA ; LAND-USE ; DROUGHT ; VARIABILITY ; CHINA ; INDEX ; TRENDS ; PRECIPITATION ; SENSITIVITY
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
来源机构北京师范大学 ; 中国科学院植物研究所
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/176999
作者单位1.Univ Toledo, Dept Environm Sci, Toledo, OH 43606 USA;
2.Chinese Acad Sci, Inst Bot, Beijing 100093, Peoples R China;
3.Univ New Hampshire, Inst Study Earth Oceans & Space, Earth Syst Res Ctr, Durham, NH 03824 USA;
4.Atmospher & Environm Res Inc, Boston, MA USA;
5.Bay Area Environm Res Inst, Moffett Field, CA 94035 USA;
6.NASA, Ames Res Ctr, Moffett Field, CA 94035 USA;
7.Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing 100875, Peoples R China;
8.Mongolian Acad Sci, Inst Geog, Ulaanbaatar 210620, Mongolia
推荐引用方式
GB/T 7714
John, Ranjeet,Chen, Jiquan,Ou-Yang, Zu-Tao,et al. Vegetation response to extreme climate events on the Mongolian Plateau from 2000 to 2010[J]. 北京师范大学, 中国科学院植物研究所,2013,8(3).
APA John, Ranjeet.,Chen, Jiquan.,Ou-Yang, Zu-Tao.,Xiao, Jingfeng.,Becker, Richard.,...&Batkhishig, Ochirbat.(2013).Vegetation response to extreme climate events on the Mongolian Plateau from 2000 to 2010.ENVIRONMENTAL RESEARCH LETTERS,8(3).
MLA John, Ranjeet,et al."Vegetation response to extreme climate events on the Mongolian Plateau from 2000 to 2010".ENVIRONMENTAL RESEARCH LETTERS 8.3(2013).
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