Spatial and temporal trends of climate change in Xinjiang, China

Temperature and precipitation time series datasets from 1961 to 2005 at 65 meteorological stations were used to reveal the spatial and temporal trends of climate change in Xinjiang, China. Annual and seasonal mean air temperature and total precipitation were analyzed using Mann-Kendall (MK) test, inverse distance weighted (IDW) interpolation, and R/S methods. The results indicate that: (1) both temperature and precipitation increased in the past 45 years, but the increase in temperature is more obvious than that of precipitation; (2) for temperature increase, the higher the latitude and the higher the elevation the faster the increase, though the latitude has greater influence on the increase. Northern Xinjiang shows a faster warming than southern Xinjiang, especially in summer; (3) increase of precipitation occurs mainly in winter in northern Xinjiang and in summer in southern Xinjiang. Ili, which has the most precipitation in Xinjiang, shows a weak increase of precipitation; (4) although both temperature and precipitation increased in general, the increase is different inside Xinjiang; (5) Hurst index (H) analysis indicates that climate change will continue the current trends.

[1]  Comparison of pan evaporation and actual evaporation estimated by land surface model in Xinjiang from 1960 to 2005 , 2009 .

[2]  Jianhua Xu,et al.  Climate change and its effects on runoff of Kaidu River, Xinjiang, China: A multiple time-scale analysis , 2008 .

[3]  Wei Gao,et al.  Sensitivity analysis of response of land cover change to climate change from 1992 to 2000 across Xinjiang , 2003, SPIE Optics + Photonics.

[4]  B. Burchfiel,et al.  Crustal shortening on the margins of the Tien Shan , 1999 .

[5]  W. Ye,et al.  Climate instability in the Yili region, Xinjiang during the last glaciation , 2000 .

[6]  Wei Zhong,et al.  Climatic change during the last 4000 years in the southern Tarim Basin, Xinjiang, northwest China , 2007 .

[7]  Jun Li.  Variations of potential evapotranspiration from 1961-2000 in Xinjiang, China , 2007, Geoinformatics.

[8]  Fengqing Jiang,et al.  Observed trends of heating and cooling degree-days in Xinjiang Province, China , 2009 .

[9]  Yaonan Zhang,et al.  Response of runoff in the source region of the Yellow River to climate warming , 2010 .

[10]  Yan Zeng,et al.  Change in pan evaporation over the past 50 years in the arid region of China , 2009 .

[11]  E. Kahya,et al.  Trend analysis of streamflow in Turkey , 2004 .

[12]  Guobin Fu,et al.  Trends of major hydroclimatic variables in the Tarim River basin during the past 50 years , 2010 .

[13]  A. H. Siddiqi,et al.  Wavelet based hurst exponent and fractal dimensional analysis of Saudi climatic dynamics , 2009 .

[14]  Zhang Hong,et al.  A preliminary study of oasis evolution in the Tarim Basin, Xinjiang, China , 2003 .

[15]  Edward R. Cook,et al.  Climate change over the past 2000 years in Western China , 2009 .

[16]  Huajun Xu,et al.  A Holocene climatic record denoted by geochemical indicators from Barkol Lake in the northeastern Xinjiang, NW China , 2010 .

[17]  Zhu Chenggang,et al.  Fifty-year climate change and its effect on annual runoff in the Tarim River Basin, China , 2009 .

[18]  Yaning Chen,et al.  Effects of climate change on water resources in Tarim River Basin, Northwest China. , 2007, Journal of environmental sciences.

[19]  Minhe Ji,et al.  Wavelet analysis and nonparametric test for climate change in Tarim River Basin of Xinjiang during 1959–2006 , 2009 .

[20]  Yongping Shen,et al.  Hydrology and water resources variation and its response to regional climate change in Xinjiang , 2010 .

[21]  Hideaki Shibata,et al.  Potential effects of climate change and variability on watershed biogeochemical processes and water quality in Northeast Asia. , 2010, Environment international.

[22]  Shafiqur Rehman,et al.  Study of Saudi Arabian climatic conditions using Hurst exponent and climatic predictability index , 2009 .

[23]  G. Mu,et al.  Magnification of Flood Disasters and its Relation to Regional Precipitation and Local Human Activities since the 1980s in Xinjiang, Northwestern China , 2005 .

[24]  N. Cobb,et al.  Climate change and human activities: a case study in Xinjiang, China , 2010 .

[25]  Jiabao Zhang,et al.  The primary research of climate change features and their causes for the recent 40 years in Xinjiang , 2003, SPIE Asia-Pacific Remote Sensing.

[26]  Xiaoling Pan,et al.  Preliminary study on the relationship between temporal and spatial evolution of ecological landscape pattern and climate change in Xinjiang, China , 2003, SPIE Asia-Pacific Remote Sensing.

[27]  E. Cook,et al.  An extreme drought event in the central Tien Shan area in the year 1945. , 2010 .

[28]  Yaning Chen,et al.  Global perspective on hydrology, water balance, and water resources management in arid basins , 2009 .

[29]  Quanlin Ma,et al.  Effects of precipitation, soil water content and soil crust on artificial Haloxylon ammodendron forest , 2007 .

[30]  Yan Zeng,et al.  Trend in pan evaporation and its attribution over the past 50 years in China , 2010 .

[31]  Zhou Kefa,et al.  Ecological response to the climate change on the northern slope of the Tianshan Mountains in Xinjiang , 2005 .

[32]  Corinne Le Quéré,et al.  Climate Change 2013: The Physical Science Basis , 2013 .

[33]  Denis Ruelland,et al.  Sensitivity of a lumped and semi-distributed hydrological model to several methods of rainfall interpolation on a large basin in West Africa , 2008 .

[34]  Yaning Chen,et al.  Periodicity of plant yield and its response to precipitation in the steppe desert of the Tianshan Mountains region , 2010 .

[35]  Shunde Wang,et al.  The effects of human activities on oasis climate and hydrologic environment in the Aksu River Basin, Xinjiang, China , 2010 .

[36]  E. Kang,et al.  Recent and Future Climate Change in Northwest China , 2007 .