Study on applicability of remote sensing precipitation products in hilly-plain-wetland complex area of northeast China

被引:0
|
作者
Wang, Zhu-Xian [1 ]
Wang, Zi-Yang [2 ]
Feng, Peng [1 ]
Dong, Yang [1 ]
Zhang, Zhao-Wei [1 ]
Yang, Ying-Kui [1 ]
机构
[1] Heilongjiang Prov Meteorol Data Ctr, Harbin 150030, Peoples R China
[2] Heilongjiang Prov Meteorol Serv Ctr, Harbin 150036, Peoples R China
关键词
hilly-plain-wetland; Naoli River; remote sensing precipitation; spatial scale; time scale; HIGH-RESOLUTION SATELLITE; BASIN; TMPA; REGION; MODEL;
D O I
10.2166/ws.2021.387
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
For the hilly-plain-wetland complex ecosystem in the cold region of Northeast China, in order to solve the problems which include the scarcity of surface rainfall stations and the inability to provide accurate surface precipitation for hydrological process simulation, based on the observed precipitation of rainfall stations, three remote sensing precipitation products are taken as objects of evaluation. They include TRMM(Tropical Rainfall Measuring Mission) 3B42V7,3B42RT and CHIRPS (Climate Hazards Group InfraRed Precipitation with Station data,CHIP). In this paper, the observation data of rainfall stations and IDWP precipitation data interpolated by IDW(Inverse Distance Weighted) are used as true value of precision comparison, and the detection accuracy of remote sensing precipitation products from 2001 to 2010 is evaluated on the time scale (day, month and quarter) and spatial scale in Naoli River Basin.The results of the study indicated that 3B42V7 and CHIP have a high detection accuracy for precipitation, and their CC(correlation coefficient) values are 0.47 and 0.49 respectively in daily time scale. The accuracy of their observationfor monthly precipitation is better than that of daily precipitation, and the CC are 0.85 and 0.87 respectively. The multi-year average precipitation at different grid positions in the basin is overestimated by 3B42RT, and its evaluation results are poor at different time scales.For the precipitation intensity range of (0,20], the observed results of 3B42V7 and rainfall station are close to each other. For the precipitation intensity ranges of (0,1) and (50,+infinity), 3B42RT and CHIP have overestimated or underestimated the precipitation in different degrees. Based on the above analysis results, 3B42RT can be considered as data that can detect whether precipitation occurs on different spatial positions in the basin. 3B42V7 and CHIP can be applied to flood forecasting and non-point source pollution control in cold regions.
引用
收藏
页码:3498 / 3507
页数:10
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