TY - JOUR
T1 - Climate change and human activities
T2 - A case study in Xinjiang, China
AU - Wu, Zhuoting
AU - Zhang, Hongjun
AU - Krause, Crystal M.
AU - Cobb, Neil S.
N1 - Funding Information:
Acknowledgements We thank Xinshi Zhang, Borong Pan and Wencui Feng for providing weather data used in this study. We also thank Paul Dijkstra for providing references for calculating greenhouse gas emissions and many valuable suggestions to the paper, and Steven Sesnie for providing support for processing MODIS images. This work is supported by Major Academician Consulting Project of Chinese Academy of Sciences and the Cheung Kong Scholar’s Program and the Promotion Project for Creative Teams of Ministry of Education of the People’s Republic of China (IRT0412), and the Science Foundation Arizona (GRF 0001-07).
PY - 2010/4
Y1 - 2010/4
N2 - We examined both long-term climate variability and anthropogenic contributions to current climate change for Xinjiang province of northwest China. Xinjiang encompasses several mountain ranges and inter-mountain basins and is comprised of a northern semiarid region and a more arid southern region. Climate over the last three centuries was reconstructed from tree rings and temperature series were calculated for the past 50 years using weather station data. Three major conclusions from these analyses are: (1) Although temperature varied considerably in Xinjiang over the last 200 years, it was non-directional until the last 50 years when a substantial warming trend occurred; (2) The semiarid North Xinjiang was representative of the northern hemisphere climate, while the more arid South Xinjiang resembled the southern hemisphere climate, meanwhile, (3) The entire Xinjiang province captured the global-scale climate signal. We also compared human contributions to global change between North and South Xinjiang, including land cover/land use, population, and greenhouse gas production. For both regions, urban areas acted as heat islands; and large areas of grassland and forest were converted to barren land, especially in North Xinjiang. Additionally, North Xinjiang also showed larger increase in population and greenhouse gas emissions mainly associated with animal production than those in South Xinjiang. Although Xinjiang province is a geographically coupled mountain-basin system, the two regions have distinct climate patterns and anthropogenic activities related to land cover conversion and greenhouse gas production.
AB - We examined both long-term climate variability and anthropogenic contributions to current climate change for Xinjiang province of northwest China. Xinjiang encompasses several mountain ranges and inter-mountain basins and is comprised of a northern semiarid region and a more arid southern region. Climate over the last three centuries was reconstructed from tree rings and temperature series were calculated for the past 50 years using weather station data. Three major conclusions from these analyses are: (1) Although temperature varied considerably in Xinjiang over the last 200 years, it was non-directional until the last 50 years when a substantial warming trend occurred; (2) The semiarid North Xinjiang was representative of the northern hemisphere climate, while the more arid South Xinjiang resembled the southern hemisphere climate, meanwhile, (3) The entire Xinjiang province captured the global-scale climate signal. We also compared human contributions to global change between North and South Xinjiang, including land cover/land use, population, and greenhouse gas production. For both regions, urban areas acted as heat islands; and large areas of grassland and forest were converted to barren land, especially in North Xinjiang. Additionally, North Xinjiang also showed larger increase in population and greenhouse gas emissions mainly associated with animal production than those in South Xinjiang. Although Xinjiang province is a geographically coupled mountain-basin system, the two regions have distinct climate patterns and anthropogenic activities related to land cover conversion and greenhouse gas production.
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U2 - 10.1007/s10584-009-9760-6
DO - 10.1007/s10584-009-9760-6
M3 - Article
AN - SCOPUS:77950460733
SN - 0165-0009
VL - 99
SP - 457
EP - 472
JO - Climatic Change
JF - Climatic Change
IS - 3
ER -