Utilization of Google Earth Engine for Assessment of Daily and Seasonal Variations of TRMM3B43-v7, GPM-v6 and PERSIANN-CDR Data Over the Coastline of Pahang State, Malaysia

被引:1
作者
Akbari, Abolghasem [1 ]
Jaghargh, Majid Rajabi [2 ]
Samah, Azizan Abu
Cox, Jonathan [3 ]
机构
[1] Binaloud Inst Higher Educ, Dept Civil Engn, Mashhad, Iran
[2] Ferdowsi Univ Mashhad, Dept Water Sci & Engn, Mashhad, Iran
[3] Caribbean Inst Meteorol & Hydrol, POB 130, Bridgetown, Barbados
基金
美国国家航空航天局;
关键词
GPM; PERSIANN-CDR; Kuantan; Malaysia; Google Earth Engine; SATELLITE PRECIPITATION; MODEL; VARIABILITY; PRODUCTS; BASIN; IMERG; 3B42;
D O I
10.1007/s12524-022-01657-x
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Precipitation is one of the main components of the hydrological cycle, and its accurate measurement has been a long-term objective of scientists, water resources industries, and earth observation technology. The Tropical Rainfall Measurement Mission (TRMM) launched in 1997 opened a new era for precipitation estimation from space. Since then, several other satellite-based precipitation products (SPPs) have been released. Examining the suitability and validity of these SPPs has become a proactive line of research in recent years. This study uses the Google Earth Engine platform to daily and seasonal variations of TRMM3B43-v7, GPM-v6 and PERSIANN-CDR data over the coastline of Pahang State in Malaysia using seven rain gauges located in the vicinity of the South China Sea. An initial comparison of three SPPs was performed with the ground truth monthly data for the period of 10 years (2002-2011) in four recognizable time periods through the year known as; northeast monsoon (NEM) (Nov-Feb), southwest monsoon (SEM) (May-Aug), intermonsoon 1 (IM1) (Mar- Apr) and intermonsoon 2 (IM2) (Sep-Oct). This study found that TRMM3B43-v7 data satisfactorily explained the rainfall characteristics in the NEM period followed by GPM based on the applied statistical metrics CC (0.76, 0.72), NSE (0.73, 0.70) and KGE (0.72, 0.67). However, a relatively weak and unstable correlation was observed for PERSIANN-CDR in all four investigated time periods. It was also revealed that SPPs could only explain the monthly precipitation well on the NEM and relatively well for the IM2 period. The poorest results were obtained for the SWM period with CC (0.35,0.26,0.17), KGE (0.24,0.16,0.06) and NSE (0.29, 0.24, 0.00) for TRMM3B43-v7, GPM-v6 and PERSIANN-CDR, respectively. In addition, this study enhances the weakness of SPPs in daily timescales specifically when it comes to hydrological applications such as real-time flood forecasting.
引用
收藏
页码:601 / 611
页数:11
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