Journal of Japan Society for Natural Disaster Science
Online ISSN : 2434-1037
Print ISSN : 0286-6021
The 2022 Heavy Rainfall Disaster Caused by Stagnated Linear Rainbands in the Kaetsu Region, Niigata
Ryoko NishiiKatsuhisa KawashimaTakane MatsumotoKyoko S. KataokaShun WatabeHiroshi Kurita
Author information
JOURNAL FREE ACCESS

2024 Volume 43 Issue 2 Pages 207-228

Details
Abstract
The Kaetsu region, Niigata Prefecture, experienced record-breaking heavy rainfall between the 3rd to 4th August 2022 that originated from stagnated linear rainbands. Intense rainfall up to 150 mm h-1 resulted in numerous shallow landslides on mountain slopes, with a landslide area rate( normalized cumulative area of landslides per unit area of landform) of 8.3%. In addition, hyperconcentrated flow with large woody debris in the Osawa River reached the hamlet of Koiwauchi, Murakami city, late at night. Fortunately, there were no fatalities caused by the event. However, damming of the channel by large woody debris resulted in the destruction of several houses along the river and inundation of the surrounding area. Evacuation of residents in Koiwauchi was initiated by the local government, based on flood alert information rather than landslide alert information. This was key to obtaining sufficient lead time for a successful evacuation. In Koiwauchi, the lessons learned from the 1967 Uetsu flood disaster and the training program for disaster prevention expert facilitated by Murakami city were instrumental in bringing about effective and appropriate evacuation behavior.
Content from these authors
© 2024 Japan Society for Natural Disaster Science
Previous article Next article
feedback
Top