Assessment of Satellite-Based Precipitation Products Performance over the Hyperarid Climate of Kuwait

被引:0
作者
AlMutairi, Bandar S. [1 ]
机构
[1] Kuwait Univ, Civil Engn Dept, Kuwait, Kuwait
关键词
Precipitation; Remote sensing; Hydrometeorology; Model evaluation/performance; Model output statistics; HIGH-RESOLUTION SATELLITE; RAINFALL DATA; ANALYSIS TMPA; GPM IMERG; BASIN; 3B42;
D O I
10.1175/JHM-D-20-0300.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Precipitation is a complex natural parameter that is essential for water and environmental systems. Due to its variability on the spatial and temporal scales, satellite-based precipitation products (SPPs) have arisen interest in hydrology and meteorology applications. This study measures the performance of six high-resolution SPPs [GPM IMERG products (IMERG-E, IMERG-L, and IMERG-F), TMPA products (3B42 V7, 3B42RT V7), and PERSIANN product] in producing the observed precipitation over a hyperarid climate, water-scarce region for the period 2013-18. It also evaluates their performance dependency on the aggregation time step and topographic elevations. According to a number of continuous and categorical evaluation metrics: (i) SPPs overestimate the observed daily annual and seasonal precipitation, particularly with near-real-time products; (ii) all SPPs estimates depict correlation ranging from 0.68 to 0.84 with the annual and seasonal precipitation and weak correlations in dry season; and (iii) their ability to detect rain/no-rain events is measured by Peirce's skill score (PSS), ranging from 0.73 to 0.92 across annual and seasonal scales, whereas 3B42RT V7 reproduces lower PSSs. Furthermore, the study finds that aggregation to a monthly time step improves only SPP correlations. The performance of near-real-time products shows significant dependency on elevations, especially with 3B42RT V7, which shows low skills at coastlands. The TMPA products' ability to detect rain/no-rain events dramatically drops from highlands to coastlands, with low skills to generate observed no/tiny and light precipitation classes. The study addresses an adequate ability of IMERG-F and PERSIANN to be utilized in water and environmental studies over hyperarid climate regions, with highlighting for the superiority of IMERG-F.
引用
收藏
页码:2489 / 2501
页数:13
相关论文
共 51 条
[1]   Evaluation of TRMM 3B42V7 and CHIRPS Satellite Precipitation Products as an Input for Hydrological Model over Eastern Nile Basin [J].
Abdelmoneim, Hadir ;
Soliman, Mohamed Reda ;
Moghazy, Hossam Mohamed .
EARTH SYSTEMS AND ENVIRONMENT, 2020, 4 (04) :685-698
[2]   Accounting for Uncertainties of the TRMM Satellite Estimates [J].
AghaKouchak, Amir ;
Nasrollahi, Nasrin ;
Habib, Emad .
REMOTE SENSING, 2009, 1 (03) :606-619
[3]   Calibration of TRMM rainfall climatology over Saudi Arabia during 1998-2009 [J].
Almazroui, Mansour .
ATMOSPHERIC RESEARCH, 2011, 99 (3-4) :400-414
[4]   PERSIANN-CDR Daily Precipitation Climate Data Record from Multisatellite Observations for Hydrological and Climate Studies [J].
Ashouri, Hamed ;
Hsu, Kuo-Lin ;
Sorooshian, Soroosh ;
Braithwaite, Dan K. ;
Knapp, Kenneth R. ;
Cecil, L. Dewayne ;
Nelson, Brian R. ;
Prat, Olivier P. .
BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, 2015, 96 (01) :69-+
[5]   Validation of new satellite rainfall products over the Upper Blue Nile Basin, Ethiopia [J].
Ayehu, Getachew Tesfaye ;
Tadesse, Tsegaye ;
Gessesse, Berhan ;
Dinku, Tufa .
ATMOSPHERIC MEASUREMENT TECHNIQUES, 2018, 11 (04) :1921-1936
[6]  
Bolvin D. T., ALGORITHM THEORETICA
[7]   Towards a roadmap for use of radar rainfall data in urban drainage [J].
Einfalt, T ;
Arnbjerg-Nielsen, K ;
Golz, C ;
Jensen, NE ;
Quirmbach, M ;
Vaes, G ;
Vieux, B .
JOURNAL OF HYDROLOGY, 2004, 299 (3-4) :186-202
[8]  
Eris E., 2012, Journal of Water Resource and Protection, V4, P99, DOI 10.4236/jwarp.2012.42012
[9]   Evaluation and Hydrological Application of CMADS against TRMM 3B42V7, PERSIANN-CDR, NCEP-CFSR, and Gauge-Based Datasets in Xiang River Basin of China [J].
Gao, Xichao ;
Zhu, Qian ;
Yang, Zhiyong ;
Wang, Hao .
WATER, 2018, 10 (09)
[10]  
Hsu KL, 1997, J APPL METEOROL, V36, P1176, DOI 10.1175/1520-0450(1997)036<1176:PEFRSI>2.0.CO