Response of vegetation NDVI to climatic extremes in the arid region of Central Asia: a case study in Xinjiang, China

被引:73
作者
Yao, Junqiang [1 ]
Chen, Yaning [2 ]
Zhao, Yong [3 ]
Mao, Weiyi [1 ]
Xu, Xinbing [4 ,5 ]
Liu, Yang [6 ]
Yang, Qing [1 ]
机构
[1] China Meteorol Adm, Inst Desert Meteorol, Urumqi 830002, Peoples R China
[2] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, Urumqi 830011, Peoples R China
[3] Chengdu Univ Informat Technol, Sch Atmospher Sci, 24 Xuefu Rd, Chengdu 610225, Sichuan, Peoples R China
[4] Xinjiang Normal Univ, Urumqi 830054, Peoples R China
[5] Lanzhou Univ, Coll Earth & Environm Sci, Lanzhou 734000, Gansu, Peoples R China
[6] Xinjiang Univ, Coll Resources & Environm Sci, Key Lab Oasis Ecol, Minist Educ, Urumqi 830046, Peoples R China
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
WATER-RESOURCES; INDEX NDVI3G; TRENDS; DYNAMICS; GROWTH; GIMMS; TEMPERATURE; IMPACTS; HYDROLOGY; INCREASE;
D O I
10.1007/s00704-017-2058-0
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Observed data showed the climatic transition from warm-dry to warm-wet in Xinjiang during the past 30 years and will probably affect vegetation dynamics. Here, we analyze the interannual change of vegetation index based on the satellite-derived normalized difference vegetation index (NDVI) with temperature and precipitation extreme over the Xinjiang, using the 8-km NDVI third-generation (NDVI3g) from the Global Inventory Modelling and Mapping Studies (GIMMS) from 1982 to 2010. Few previous studies analyzed the link between climate extremes and vegetation response. From the satellite-based results, annual NDVI significantly increased in the first two decades (1981-1998) and then decreased after 1998. We show that the NDVI decrease over the past decade may conjointly be triggered by the increases of temperature and precipitation extremes. The correlation analyses demonstrated that the trends of NDVI was close to the trend of extreme precipitation; that is, consecutive dry days (CDD) and torrential rainfall days (R24) positively correlated with NDVI during 1998-2010. For the temperature extreme, while the decreases of NDVI correlate positively with warmer mean minimum temperature (Tnav), it correlates negatively with the number of warmest night days (Rwn). The results suggest that the climatic extremes have possible negative effects on the ecosystem.
引用
收藏
页码:1503 / 1515
页数:13
相关论文
共 67 条
[11]   Global Trends in Seasonality of Normalized Difference Vegetation Index (NDVI), 1982-2011 [J].
Eastman, J. Ronald ;
Sangermano, Florencia ;
Machado, Elia A. ;
Rogan, John ;
Anyamba, Assaf .
REMOTE SENSING, 2013, 5 (10) :4799-4818
[12]   Climate change and the ecological responses in Xinjiang, China: Model. simulations and data analyses [J].
Fang, Shifeng ;
Yan, Jianwu ;
Che, Mingliang ;
Zhu, Yunqiang ;
Liu, Zhihui ;
Pei, Huan ;
Zhang, Huifang ;
Xu, Guang ;
Lin, Xiaofeng .
QUATERNARY INTERNATIONAL, 2013, 311 :108-116
[13]   Greenness in semi-arid areas across the globe 1981-2007 - an Earth Observing Satellite based analysis of trends and drivers [J].
Fensholt, Rasmus ;
Langanke, Tobias ;
Rasmussen, Kjeld ;
Reenberg, Anette ;
Prince, Stephen D. ;
Tucker, Compton ;
Scholes, Robert J. ;
Le, Quang Bao ;
Bondeau, Alberte ;
Eastman, Ron ;
Epstein, Howard ;
Gaughan, Andrea E. ;
Hellden, Ulf ;
Mbow, Cheikh ;
Olsson, Lennart ;
Paruelo, Jose ;
Schweitzer, Christian ;
Seaquist, Jonathan ;
Wessels, Konrad .
REMOTE SENSING OF ENVIRONMENT, 2012, 121 :144-158
[14]   Evaluation of earth observation based long term vegetation trends - Intercomparing NDVI time series trend analysis consistency of Sahel from AVHRR GIMMS, Terra MODIS and SPOT VGT data [J].
Fensholt, Rasmus ;
Rasmussen, Kjeld ;
Nielsen, Thomas Theis ;
Mbow, Cheikh .
REMOTE SENSING OF ENVIRONMENT, 2009, 113 (09) :1886-1898
[15]   Anthropogenic contribution to global occurrence of heavy-precipitation and high-temperature extremes [J].
Fischer, E. M. ;
Knutti, R. .
NATURE CLIMATE CHANGE, 2015, 5 (06) :560-564
[16]   Assessing onset and length of greening period in six vegetation types in Oaxaca, Mexico, using NDVI-precipitation relationships [J].
Gomez-Mendoza, L. ;
Galicia, L. ;
Cuevas-Fernandez, M. L. ;
Magana, V. ;
Gomez, G. ;
Palacio-Prieto, J. L. .
INTERNATIONAL JOURNAL OF BIOMETEOROLOGY, 2008, 52 (06) :511-520
[17]   Leaf respiration is differentially affected by leaf vs. stand-level night-time warming [J].
Griffin, KL ;
Turnbull, M ;
Murthy, R ;
Lin, GH ;
Adams, J ;
Farnsworth, B ;
Mahato, T ;
Bazin, G ;
Potasnak, M ;
Berry, JA .
GLOBAL CHANGE BIOLOGY, 2002, 8 (05) :479-485
[18]   The 2007 eastern US spring freezes: Increased cold damage in a warming world? [J].
Gu, Lianhong ;
Hanson, Paul J. ;
Mac Post, W. ;
Kaiser, Dale P. ;
Yang, Bai ;
Nemani, Ramakrishna ;
Pallardy, Stephen G. ;
Meyers, Tilden .
BIOSCIENCE, 2008, 58 (03) :253-262
[19]  
Guo Ni, 2008, Zhiwu Shengtai Xuebao, V32, P319, DOI 10.3773/j.issn.1005-264x.2008.02.008
[20]   Perception of climate change [J].
Hansen, James ;
Sato, Makiko ;
Ruedy, Reto .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2012, 109 (37) :E2415-E2423