論文

2021年2月

Evaluation of precipitation elasticity using precipitation data from ground and satellite-based estimates and watershed modeling in Western Nepal

JOURNAL OF HYDROLOGY-REGIONAL STUDIES
  • Rocky Talchabhadel
  • ,
  • Anil Aryal
  • ,
  • Kenji Kawaike
  • ,
  • Kazuki Yamanoi
  • ,
  • Hajime Nakagawa
  • ,
  • Binod Bhatta
  • ,
  • Saroj Karki
  • ,
  • Bhesh Raj Thapa

33
記述言語
英語
掲載種別
研究論文(学術雑誌)
DOI
10.1016/j.ejrh.2020.100768
出版者・発行元
ELSEVIER

Study Region: West Rapti River (WRR) basin, Western Nepal.Study Focus: Hydrologic modeling requires an accurate precipitation data at a high spatial resolution, which is often limited in many regions of the globe. As a complement to the ground (gauge) precipitation data, satellite-based precipitation estimates (SPEs) appear useful. At first, this study evaluated performance of three different SPEs, namely i) CHIRPS, ii) PERSIANN-CCS, and iii) IMERG, with respect to gauge data using different event detection and quantification indices. Soil Water Assessment Tool (SWAT), a semi-distributed hydrologic model, was used to simulate the river discharge. We then analysed precipitation elasticity, as a first kind of such study in Nepalese river basin, by scaling the precipitation input in both positive and negative directions (ranging from -20 % to +20 %) in order to explore basin response on likely alteration of precipitation. A non-parametric precipitation elasticity was finally computed for three different cases: 1) observed river discharge, 2) gauge-based simulated river discharge, and 3) SPEs-based simulated river discharge.New Hydrologic Insights for the Region: IMERG proved to be superior among three SPEs. All SPEs showed improved results after implementation of different levels of bias-correction where daily precipitation data were corrected using linear correction factors computed at a mean monthly scale. Computed correction factors are replicable to nearby basins. Precipitation elasticity of the study area ranged from +1.3 to +2.0 (approximately +1.5) which indicates that a 1.0 % change in precipitation will result in 1.5 % change in river discharge.

リンク情報
DOI
https://doi.org/10.1016/j.ejrh.2020.100768
Web of Science
https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=JSTA_CEL&SrcApp=J_Gate_JST&DestLinkType=FullRecord&KeyUT=WOS:000612991900002&DestApp=WOS_CPL
ID情報
  • DOI : 10.1016/j.ejrh.2020.100768
  • eISSN : 2214-5818
  • Web of Science ID : WOS:000612991900002

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