Spatial Interpolation of Daily Precipitation in China: 1951-2005

被引:100
作者
Chen, Deliang [1 ]
Ou, Tinghai [1 ,2 ]
Gong, Lebing [3 ]
Xu, Chong-Yu [3 ,4 ]
Li Weijing [5 ]
Ho, Chang-Hoi [6 ]
Qian Weihong [7 ]
机构
[1] Univ Gothenburg, Dept Earth Sci, Gothenburg, Sweden
[2] Beijing Normal Univ, Sch Geog, Beijing 100875, Peoples R China
[3] Uppsala Univ, Dept Earth Sci, Uppsala, Sweden
[4] Univ Oslo, Dept Geosci, N-0316 Oslo, Norway
[5] China Meteorol Adm, Natl Climate Ctr, Lab Climate Studies, Beijing 100029, Peoples R China
[6] Seoul Natl Univ, Sch Earth & Environm Sci, Seoul 151, South Korea
[7] Peking Univ, Sch Phys, Beijing 100871, Peoples R China
关键词
daily precipitation; spatial interpolation; ordinary kriging; gridded data; China; STOCHASTIC INTERPOLATION; CLIMATE VARIABILITY; RAINFALL DATA; MODEL; TEMPERATURE; NORMALS; SWEDEN; GAUGES; TRENDS; WIND;
D O I
10.1007/s00376-010-9151-y
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Climate research relies heavily on good quality instrumental data; for modeling efforts gridded data are needed. So far, relatively little effort has been made to create gridded climate data for China. This is especially true for high-resolution daily data. This work, focuses on identifying an accurate method to produce gridded daily precipitation in China based on the observed data at 753 stations for the period 1951-2005. Five interpolation methods, including ordinary nearest neighbor, local polynomial, radial basis function, inverse distance weighting, and ordinary kriging, have been used and compared. Cross-validation shows that the ordinary kriging based on seasonal semi-variograms gives the best performance, closely followed by the inverse distance weighting with a power of 2. Finally the ordinary kriging is chosen to interpolate the station data to a 18 kmx 18 km grid system covering the whole country. Precipitation for each 0.5A degrees x 0.5A degrees latitude-longitude block is then obtained by averaging the values at the grid nodes within the block. Owing to the higher station density in the eastern part of the country, the interpolation errors are much smaller than those in the west (west of 100A degrees E). Excluding 145 stations in the western region, the daily, monthly, and annual relative mean absolute errors of the interpolation for the remaining 608 stations are 74%, 29%, and 16%, respectively. The interpolated daily precipitation has been made available on the internet for the scientific community.
引用
收藏
页码:1221 / 1232
页数:12
相关论文
共 56 条
[1]   Performance of the Rossby Centre regional atmospheric model in Southern Sweden: comparison of simulated and observed precipitation [J].
Achberger, C ;
Linderson, ML ;
Chen, D .
THEORETICAL AND APPLIED CLIMATOLOGY, 2003, 76 (3-4) :219-234
[2]  
[Anonymous], 1987, Map Projections-A Working Manual
[3]  
[Anonymous], 2002, Trans GIS, DOI DOI 10.1111/1467-9671.00101
[4]   Spatio-temporal interpolation of climatic variables over large region of complex terrain using neural networks [J].
Antonic, O ;
Krizan, J ;
Marki, A ;
Bukovec, D .
ECOLOGICAL MODELLING, 2001, 138 (1-3) :255-263
[5]  
[蔡福 CAI Fu], 2006, [资源科学, Resources science], V28, P73
[6]   THE PARAMETER R2 IN MULTIQUADRIC INTERPOLATION [J].
CARLSON, RE ;
FOLEY, TA .
COMPUTERS & MATHEMATICS WITH APPLICATIONS, 1991, 21 (09) :29-42
[7]  
CHEN D, 2004, J LAKE SCI, V15, P105
[8]   A high-resolution, gridded dataset for monthly temperature normals (1971-2000) in Sweden [J].
Chen, Deliang ;
Gong, Lebing ;
Xu, Chong-Yu ;
Halldin, Sven .
GEOGRAFISKA ANNALER SERIES A-PHYSICAL GEOGRAPHY, 2007, 89A (04) :249-261
[9]   Comparison of the Thornthwaite method and pan data with the standard Penman-Monteith estimates of reference evapotranspiration in China [J].
Chen, DL ;
Gao, G ;
Xu, CY ;
Guo, J ;
Ren, GY .
CLIMATE RESEARCH, 2005, 28 (02) :123-132
[10]  
[朱华忠 Zhu Huazhong], 2003, [地理研究, Geographical Research], V22, P349