Japan Geoscience Union Meeting 2021

Presentation information

[E] Oral

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

[A-HW22] Material transportation and cycling in watershed ecosystems; from headwaters to coastal areas

Fri. Jun 4, 2021 1:45 PM - 3:15 PM Ch.12 (Zoom Room 12)

convener:Morihiro Maeda(Okayama University), Tomohisa Irino(Faculty of Environmental Earth Science, Hokkaido University), Shin-ichi Onodera(Graduate School of Advanced Science and Engineering, , Hiroshima University), Adina Paytan(University of California Santa Cruz), Chairperson:Tomohisa Irino(Faculty of Environmental Earth Science, Hokkaido University)

2:30 PM - 2:45 PM

[AHW22-15] Water discharge at forested watersheds throughout Japan by using SWAT

*Naohiro Imamura1, Kunyang Wang2, Shin-ichi Onodera2, Yuta Shimizu3, Masahiro Kobayashi1, Takanori Shimizu1, Naoyuki Yamashita1, Yoshiki Shinomiya1, Koji Tamai1, Shinji Sawano1, Shin'ichi Iida1, Naoki Kabeya1, Akira Shimizu1, Yoshio Tsuboyama1 (1.Forestry and Forest Products Research Institute, 2.Hiroshima University, 3.National Agriculture and Food Research Organization)

Keywords:Water discharge, SWAT, Forested watersheds

Predicting the impact of forest operations and/or climate change on water and nutrient cycle in forest watershed are more important for planning future forest management in Japan. This study estimated daily water discharge at different sizes and different climate watersheds in Japanese forested areas by using SWAT. We calculated discharge at Jyozankei (1.9 ha) in snowfall area (Abe et al., 2010; 2011; 2014; Nobuhiro et al., 2020), Katsura (60 ha) and Tsukuba (3.8 ha) in a temperate area, and Kahoku (3.7 ha) and Takatoriyama (19 ha) in heavy rainfall area. As a result, daily hydrographs showed relatively high reproduction for observed values at all watersheds (Nash-Sutcliffe efficiency (NSE) showed over 0.65 value). This means SWAT can calculate water discharge at various size forested watersheds in the Japanese climate. However, the calculated peak water values were a little low compared to the observed value. This indicated discharge in stormflow periods did not reproduce effectively. Setting distribution of soil depth in the watershed may be more important for improving water discharge in small forested watersheds.