日本地球惑星科学連合2025年大会

講演情報

[E] ポスター発表

セッション記号 A (大気水圏科学) » A-HW 水文・陸水・地下水学・水環境

[A-HW28] 水循環・水環境

2025年5月28日(水) 17:15 〜 19:15 ポスター会場 (幕張メッセ国際展示場 7・8ホール)

コンビーナ:濱 侃(千葉大学大学院園芸学研究院)、榊原 厚一(信州大学理学部理学科)、林 武司(秋田大学教育文化学部)、福士 圭介(金沢大学環日本海域環境研究センター)

17:15 〜 19:15

[AHW28-P03] Synthesizing the predictive regression model for low flow in river basins

*Antonio Machava Junior1Andrew Charles Whitaker2 (1.Graduate School of Science and Technology, Niigata University, Japan、2.Institute of Science and Technology, Niigata University, Japan)

キーワード:Recession constant, Low flow, Regression model, River basin, Basin characteristics

In the evaluation of low flow hydrology, low flow indices are crucial when considering water supply, water quality, and water resources planning in river basins. To evaluate a basin's low flow characteristics, the synthetic master recession curve (MRC), which is typically represented as an exponential function, has been used globally. Hydrologists have taken interest in predicting the baseflow recession rate or recession constant and the Q710flow (seven-day, 10-year low flow), and numerous regional studies have developed models to estimate baseflow recession characteristics from various catchment characteristics. However, accurately and easily deriving the MRC from streamflow records remains a challenge. This research aims to propose the synthetic regression model which can be widely applied for predicting low flow (Q710) (seven-day 10-year low flow) in order to evaluate sustainable water resources of river basin units.
The given locations (around 45 study basins) in Japan are adopted to use hydrological records for headwater catchments upstream of reservoirs, with the restriction that there are no regulations or diversion structures in the upstream reaches. Secondly, the results of regression analysis for each river basin will be compared, and parameters of the model generalized by means of using information on the dominant geology of the basins.
Ongoing results from 34 river systems indicate recession constants ranging from 0.0130 to 0.0746, showing considerable variability across basins. The results suggest how much baseflow recession rates might be influenced by basin characteristics, especially geology. The recession constants results provide initial insights into recession characteristics and their variability across basins. The ongoing research aims to finalize a synthetic regression model, which is expected to apply to other regions, such as Africa, for evaluating sustainable water resources.