Use of Indices on Daily Timescales to Study Changes in Extreme Precipitation Across Nepal Over 40 Years (1976-2015)

被引:5
|
作者
Maharjan, Manisha [1 ]
Yoneda, Minoru [1 ]
Talchabhadel, Rocky [2 ,3 ]
Thapa, Bhesh Raj [3 ,4 ,5 ]
Aryal, Anil [6 ]
机构
[1] Kyoto Univ, Dept Environm Engn, Kyoto, Japan
[2] Texas A&M Univ, Texas A&M AgriLife Res, El Paso, TX USA
[3] Smartphones Water Nepal, Lalitpur, Nepal
[4] Universal Engn & Sci Coll, Lalitpur, Nepal
[5] Nepal Acad Sci & Technol, Lalitpur, Nepal
[6] Asian Inst Technol, Water Engn & Management, Pathum Thani, Thailand
关键词
extreme precipitation; precipitation indices; Nepal; trend; spatiotemporal change; nonparametric test; KENDALL TREND TEST; MANN-KENDALL; HIMALAYAN REGION; CLIMATE-CHANGE; MONSOON; TEMPERATURE; VARIABILITY; PATTERN; EVENTS; TESTS;
D O I
10.1029/2020EA001509
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
This paper presents a comprehensive picture of extreme precipitation across Nepal from 1976 to 2015 based on high-quality daily precipitation observations from 28 precipitation stations spatially distributed across the country. We computed 11 extreme precipitation indices. The selected indices allow the analysis of extreme events (such as flood/inundation) related to heavy precipitation and evaluate the linkage with indications of agricultural production and drought (such as consecutive dry and wet days). Using a simple daily intensity index (SDII) and the number of days with daily precipitation >= 10 mm (R10), along with the total amount of annual precipitation (PRCPTOT), we summarized the distribution of the wet periods of the year at different locations. We divided the study period into two halves (T1: 1976-1995 and T2: 1996-2015) to examine the temporal mean, trends, and their shift. We emphasized the changes in those indices between these two periods across the country. Our results show that although the amount of precipitation (in terms of PRCPTOT and SDII) did not change significantly between the two periods (i.e., T1 and T2), there exists a clearly increasing trend of extreme precipitation indices in T2 compared to T1. In addition, the consecutive dry days show the rising tendency of elongated dry spells that can adversely affect plant/crop growth in the future. Our study recommends the need for effective management of both precipitation extremes (i.e., drier and wetter), for instance, by introducing irrigation facilities and flood mitigation measures.
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页数:18
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