日本地球惑星科学連合2022年大会

講演情報

[E] ポスター発表

セッション記号 H (地球人間圏科学) » H-GM 地形学

[H-GM02] Geomorphology

2022年5月30日(月) 11:00 〜 13:00 オンラインポスターZoom会場 (10) (Ch.10)

コンビーナ:齋藤 仁(関東学院大学 経済学部)、コンビーナ:八反地 剛(筑波大学生命環境系)、Parkner Thomas(University of Tsukuba, Graduate School of Life and Environmental Sciences)、コンビーナ:南雲 直子(土木研究所 水災害・リスクマネジメント国際センター)、座長:Parkner Thomas(University of Tsukuba, Graduate School of Life and Environmental Sciences)、齋藤 仁(関東学院大学 経済学部)


11:00 〜 13:00

[HGM02-P03] Preliminary detection of thermokarst landforms and vegetation succession using multitemporal satellite and UAV images

*齋藤 仁1飯島 慈裕2桐村 喬3、Fedorov Alexander N.4 (1.関東学院大、2.三重大、3.皇學館大、4.Melnikov Permafrost Inst.)

キーワード:サーモカルスト、永久凍土、UAVs、衛星コンステレーション

Eastern Siberia is characterized by widespread permafrost thawing and subsequent thermokarst development in open natural and anthropogenic landscapes. The thermokarst development affects the hydrological processes, ecosystems, and human society accompanied by vegetation succession and degradation. Presently we lack quantitative knowledge on the progression of thermokarst distribution in eastern Siberia. This study preliminary detects the early-stage thermokarst landforms and vegetation succession using multitemporal satellite images of Planet and Landsat and UAV-based high-definition images. Especially, we focus on the changes in normalized difference vegetation index (NDVI) of grasslands around the Churapcha area in eastern Siberia. The results showed that the NDVI of grasslands with early-stage thermokarst landforms was higher than that of grasslands without thermokarst development. The differences in NDVI was large during the growing season from June to August. Analysis of the time series NDVI over the past 20 years showed an increasing tendency in NDVI in early-stage thermokarst grasslands with a history of anthropogenic land use. These results indicate that increases in soil moisture and soil temperature may affect rapid vegetation growth and succession at the early-stage thermokarst landforms. Further study is necessary to verify the results using field observation over a wide area of eastern Siberia.