喜马拉雅地区气温的空间插值

S. Krishna kumar, M. Shashikumar, E. Sivasankar
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引用次数: 0

摘要

在Sutlej流域的几个站点测量的日气温需要在空间上跨流域插值,以解释所提出的融雪径流模型的空间变异性。GIDS算法结合了多元回归和距离平方反比方法,其中输入包括站点的位置和高程细节,参考每个站点之间的距离平方反比。该模型在GIS环境下创建,并在4月和5月每天执行,通过改变MATLAB软件生成的系数,分辨率为30m。该模型包含两个模块,以卡扎和拉克舍姆为检查站。统计分析结果表明,根据Kaza站,误差百分比为+/ - 5%。这两个月份的标准差分别为0.60和0.44。对于Racksham,误差百分比在+/ - 20%以内。这两个月的标准差分别为3.4和1.12。通过分析,GIDS模型受空间距离、海拔和温度等输入范围的控制。将计算的温度与递减率法(LRM)计算的温度进行了比较。相比之下,GIDS比LRM效果更好。研究表明,在一定的边界条件下,GIDS可以用于插值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spatial interpolation of air temperature in Himalayas
The daily air temperature measured at few stations in Sutlej basin need to be interpolated spatially across the basin to account for spatial variability in the proposed snowmelt runoff model. GIDS algorithm combines the multiple regression and inverse-distance-squared approaches in which the inputs includes location and elevation details of the stations with reference to inverse squared distance between each station. The model was created in GIS environment and executed daily for April and May by varying the coefficients generated using MATLAB software with 30m resolution. The model contains two modules, with Kaza and Racksham as check stations. Statistical analysis result shows, according to Kaza station the percentage of error is +/− 5%. The standard deviation for both the months is 0.60 and 0.44. In case of Racksham, the percentage of error is within +/− 20%. The standard deviation for both the months is 3.4 and 1.12. Based on analysis, GIDS model was governed by the range of inputs like spatial distance, elevations and temperatures.The computed temperatures were compared with those derived using lapse rate method (LRM). On comparison GIDS produced better results than LRM. Thus the study concludes that GIDS can be used for interpolation with certain boundary conditions.
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