Application of TRMM for Spatio-Temporal Analysis of Precipitation in the Taiwan Strait and Its Adjacent Regions

Author:

Zhong Yaozhao1ORCID,Li Da2,Wang Lei3,Zhang Caiyun4ORCID,Zhang Feng1

Affiliation:

1. Fuzhou Institute of Oceanography, Minjiang University, Fuzhou 350108, China

2. International College, Fujian Agriculture and Forestry University, Fuzhou 350002, China

3. College of Mathematics and Statistics, Sichuan University of Science & Engineering, Yibin 644000, China

4. College of Ocean and Earth Sciences, Xiamen University, Xiamen 361104, China

Abstract

Precipitation patterns are highly valued in the fields of weather forecasting, water resource management, and estuary environment research. In this study, daily and monthly precipitation TRMM data from 1998 to 2019 were selected, and EOF analysis was employed to analyze the precipitation patterns of the Taiwan Strait and its neighboring regions. We obtained the following results: (1) The rainy season (May–June) is the main contributor to precipitation in the study area. The EOF first mode reflected the overall consistency of the precipitation spatial distribution. However, within each river basin, the magnitude of precipitation variation is spatially different. The magnitude of precipitation variation is significant in the northwestern part of the Minjiang River basin, the southwestern part of the Jiulong River basin, and the southwestern corner of the Hanjiang River basin. These areas happen to correspond to the mountain areas, revealing that topographic precipitation plays a role in the spatial distribution of precipitation in the three river basins. (2) The spatial distributions of the EOF first mode and of precipitation during El Niño in the Minjiang River basin are consistent. This reveals that ENSO is probably the dominant factor in precipitation in the Minjiang River basin. The significant increase in precipitation during El Niño compared with a normal year in the Minjiang River basin confirms this point. (3) In all three strong El Niño years, 1998, 2010, and 2016, the Minjiang River basin experienced significant heavy precipitation in the fall and winter, whereas the Jiulong River and Hanjiang River basins did not (except in 2016). In other words, the Minjiang River basin is more affected by ENSO, while the Jiulong River and Hanjiang River basins are only limitedly impacted by ENSO.

Funder

Joint Funds of the National Natural Science Foundation of China

Fujian Province Natural Science Foundation

Fuzhou Institute of Oceanography Science and Technology Project

Minjiang University Talent Introduction Pre-Research Project

Fujian Marine Economic Development Special Fund Project

Fujian Science and Technology Major Special Project

Fujian Young and Middle-aged Teacher Education Research Project

Opening Project of Sichuan Province University Key Laboratory of Bridge Non-destruction Detecting and Engineering Computing

Publisher

MDPI AG

Subject

Ocean Engineering,Water Science and Technology,Civil and Structural Engineering

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