Abstract
Although the Tropical Rainfall Measurement Mission (TRMM) has come to an end, the evaluation of TRMM satellite precipitation is still of great significance for the improvement of the Global Precipitation Measurement (GPM). In this paper, the hydrological utility of TRMM Multi-satellite Precipitation Analysis (TMPA) 3B42 RTV7/V7 precipitation products was evaluated using the variable infiltration capacity (VIC) hydrological model in the upper Yangtze River basin. The main results show that (1) TMPA 3B42V7 had a reliable performance in precipitation estimation compared with the gauged precipitation on both spatial and temporal scales over the upper Yangtze River basin. Although TMPA 3B42V7 slightly underestimated precipitation, TMPA 3B42RTV7 significantly overestimated precipitation at daily and monthly time scales; (2) the simulated runoff by the VIC hydrological model showed a high correlation with the gauged runoff and lower bias at daily and monthly time scales. The Nash–Sutcliffe coefficient of efficiency (NSCE) value was as high as 0.85, the relative bias (RB) was −6.36% and the correlation coefficient (CC) was 0.93 at the daily scale; (3) the accuracy of the 3B42RTV7-driven runoff simulation had been greatly improved by using the hydrological calibration parameters obtained from 3B42RTV7 compared with that of gauged precipitation. A lower RB (14.38% vs. 66.58%) and a higher CC (0.87 vs. 0.85) and NSCE (0.71 vs. −0.92) can be found at daily time scales when we use satellite data instead of gauged precipitation data to calibrate the VIC model. However, the performance of the 3B42V7-driven runoff simulation did not improve in the same operation accordingly. The cause might be that the 3B42V7 satellite products have been adjusted by gauged precipitation. This study suggests that it might be better to calibrate the parameters using satellite data in hydrological simulations, especially for unadjusted satellite data. This study is not only helpful for understanding the assessment of multi-satellite precipitation products in large-scale and complex areas in the upper reaches of the Yangtze River, but also can provide a reference for the hydrological utility of the satellite precipitation products in other river basins of the world.
Highlights
Precipitation is a fundamental part of the hydrological cycle, which is of great significance in meteorology, hydrology, ecology and other scientific research areas [1,2]
It can be found that the precipitation relative bias fluctuation of the 3B42V7 product was slight with a range between −30% and 10%, and over 66% parts of the spatial distribution of precipitation were underestimated in the whole basin
This study evaluated the hydrological utilities of TRMM Multi-satellite Precipitation Analysis (TMPA) 3B42RTV7/V7 products against gauge observations using the variable infiltration capacity (VIC) hydrological model over the upper Yangtze River basin from 2003 to 2010
Summary
Precipitation is a fundamental part of the hydrological cycle, which is of great significance in meteorology, hydrology, ecology and other scientific research areas [1,2]. Precipitation is a complex natural phenomenon which is characterized by a significant variability both in time and space [3,4,5]. Accurate precipitation data are extremely important for water resource-related research. The main methods of obtaining precipitation data are the ground rain gauge, ground radar and space-borne passive radiometer [6,7,8]. The rain gauge is considered to be the standard for measuring precipitation, the gauge networks are sparse or nonexistent in many remote areas of the world. Satellite-based precipitation products will hopefully be an alternative to ground-based precipitation estimates for the current and foreseeable future [9]
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