Would the 'real' observed dataset stand up? A critical examination of eight observed gridded climate datasets for China

被引:85
作者
Sun, Qiaohong [1 ]
Miao, Chiyuan [1 ]
Duan, Qingyun [1 ]
Kong, Dongxian [1 ]
Ye, Aizhong [1 ]
Di, Zhenhua [1 ]
Gong, Wei [1 ]
机构
[1] Beijing Normal Univ, Coll Global Change & Earth Syst Sci, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China
基金
中国国家自然科学基金;
关键词
gridded dataset; climate change; precipitation; temperature; China; SURFACE AIR-TEMPERATURE; SPACE-TIME CLIMATE; GLOBAL PRECIPITATION; WATER-RESOURCES; VARIABILITY; PROJECTION; EXTREMES; IMPACTS; TRENDS;
D O I
10.1088/1748-9326/9/1/015001
中图分类号
X [环境科学、安全科学];
学科分类号
083001 [环境科学];
摘要
This research compared and evaluated the spatio-temporal similarities and differences of eight widely used gridded datasets. The datasets include daily precipitation over East Asia (EA), the Climate Research Unit (CRU) product, the Global Precipitation Climatology Centre (GPCC) product, the University of Delaware (UDEL) product, Precipitation Reconstruction over Land (PREC/L), the Asian Precipitation Highly Resolved Observational (APHRO) product, the Institute of Atmospheric Physics (IAP) dataset from the Chinese Academy of Sciences, and the National Meteorological Information Center dataset from the China Meteorological Administration (CN05). The meteorological variables focus on surface air temperature (SAT) or precipitation (PR) in China. All datasets presented general agreement on the whole spatio-temporal scale, but some differences appeared for specific periods and regions. On a temporal scale, EA shows the highest amount of PR, while APHRO shows the lowest. CRU and UDEL show higher SAT than IAP or CN05. On a spatial scale, the most significant differences occur in western China for PR and SAT. For PR, the difference between EA and CRU is the largest. When compared with CN05, CRU shows higher SAT in the central and southern Northwest river drainage basin, UDEL exhibits higher SAT over the Southwest river drainage system, and IAP has lower SAT in the Tibetan Plateau. The differences in annual mean PR and SAT primarily come from summer and winter, respectively. Finally, potential factors impacting agreement among gridded climate datasets are discussed, including raw data sources, quality control (QC) schemes, orographic correction, and interpolation techniques. The implications and challenges of these results for climate research are also briefly addressed.
引用
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页数:15
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