Japan Geoscience Union Meeting 2021

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-HW Hydrology & Water Environment

[A-HW20] Hydrology & Water Environment

Sat. Jun 5, 2021 9:00 AM - 10:30 AM Ch.12 (Zoom Room 12)

convener:Takeshi Hayashi(Faculty of Education and Human Studies, Akita University), Keisuke Fukushi(Institute of Nature & Environmental Technology, Kanazawa University), Koichi Sakakibara(Department of Environmental Sciences, Faculty of Science, Shinshu University), Dai Yamazaki(Institute of Industrial Sciences, The University of Tokyo), Chairperson:Takeshi Hayashi(Faculty of Education and Human Studies, Akita University), Keisuke Fukushi(Institute of Nature & Environmental Technology, Kanazawa University), Koichi Sakakibara(Department of Environmental Sciences, Faculty of Science, Shinshu University), Dai Yamazaki(Institute of Industrial Sciences, The University of Tokyo)

9:35 AM - 9:50 AM

[AHW20-04] Investigating the validity of a meso scale constitutive equation using micro scale water dynamics simulations for hillslope rainfall-runoff processes

*Yutaka Ichikawa1, Yuusuke Mori1, Yasuto Tachikawa1 (1.Graduate School of Engineering, Kyoto University)

Keywords:rainfall-runoff, hillslope, depth-discharge relationship, constitutive equation

A number of rainfall-runoff models have been developed in the field of hydraulic and hydrologic engineering, with a special attention on simulating temporal patterns of river discharge in order to meet practical demands such as discharge predictions. Conceptual rainfall-runoff models were initially developed, followed by physical-based models. The physical-based models have achieved a certain level of success, which was partly due to the considerable advancement of computers and the increasing availability of a variety of datasets. It is pointed out, however, that recent important findings based on field studies are not incorporated into rainfall-runoff models, especially used for engineering purposes. To examine the raised issue, this study conducted detailed simulations coupling surface flow and saturated-unsaturated flow for hillslope rainfall-runoff dynamics, and investigated the validity of a constitutive equation used in a rainfall-runoff model. The results revealed that the constitutive equation was capable of describing depth-discharge relationships for hillslopes with relatively shallow soil layers but not for those with thick soil layers.