Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Ching-Ying Tsou"'
Autor:
Joaquin V. Ferrer, Guilherme Samprogna Mohor, Olivier Dewitte, Tomáš Pánek, Cristina Reyes‐Carmona, Alexander L. Handwerger, Marcel Hürlimann, Lisa Köhler, Kanayim Teshebaeva, Annegret H. Thieken, Ching‐Ying Tsou, Alexandra Urgilez Vinueza, Valentino Demurtas, Yi Zhang, Chaoying Zhao, Norbert Marwan, Jürgen Kurths, Oliver Korup
Publikováno v:
Earth's Future, Vol 12, Iss 9, Pp n/a-n/a (2024)
Abstract A rapidly growing population across mountain regions is pressuring expansion onto steeper slopes, leading to increased exposure of people and their assets to slow‐moving landslides. These moving hillslopes can inflict damage to buildings a
Externí odkaz:
https://doaj.org/article/bd9a6759484445e6b67f40122550dcae
Autor:
Thi Cam Nhung Tran, Maximo Larry Lopez Caceres, Sergi Garcia i Riera, Marco Conciatori, Yoshiki Kuwabara, Ching-Ying Tsou, Yago Diez
Publikováno v:
Remote Sensing, Vol 16, Iss 20, p 3831 (2024)
Vegetation biodiversity in mountainous regions is controlled by altitudinal gradients and their corresponding microclimate. Higher temperatures, shorter snow cover periods, and high variability in the precipitation regime might lead to changes in veg
Externí odkaz:
https://doaj.org/article/9b24e62ce5f84a839975f62cf8639c50
Publikováno v:
Water, Vol 13, Iss 9, p 1185 (2021)
The N-Ohkawa landslide, and the southern section of the Ohkawa landslide, occurred during the snow-melt seasons of 1999 and 2006, respectively, in the Shirakami Mountains, Japan. This paper examines the response of trees in the Shirakami Mountains to
Externí odkaz:
https://doaj.org/article/0da764048591491d909a0642365968ad
Autor:
Ching-Ying Tsou, 鄒青穎
93
Step-pools are fundamental components of channel morphology in mountain streams. Knowing the formation of step-pools will contribute to increasing the understanding of mountain streams morphology. Because of attention to river restoration mor
Step-pools are fundamental components of channel morphology in mountain streams. Knowing the formation of step-pools will contribute to increasing the understanding of mountain streams morphology. Because of attention to river restoration mor
Externí odkaz:
http://ndltd.ncl.edu.tw/handle/14947284053002581704
Autor:
Toshiyuki KON, Ching-Ying TSOU, Takashi KOI, Yusuke YAMAMOTO, Naoto KOIWA, Ryu NODA, Michiya IRASAWA, Kiyokazu KATO, Hiroshi TSUSHIMA, Hiroshi MORI, Hideya IWATA, Tatsuya SATO, Hajime IKEDA, Yushi KUDO, Motoshiko KOBAYASHI, Kenichi ARAI, Chie KUROIWA, Yuki KOGA, Takeaki ISHIKAWA, Misa TSUSHIMA, Eiji NAGANO, Jun MIURA, Haruka SAITO, Reona KAWAKAMI
Publikováno v:
International Journal of Erosion Control Engineering. 15:22-30
Autor:
Syushi MATSUSHIMA, Michiya IRASAWA, Ching-Ying TSOU, Kazunori HAYASHI, Tatsuya OCHIAI, Taro SUZUKI
Publikováno v:
Journal of the Japan Landslide Society. 59:92-98
Autor:
Hisako Furukawa, Ching-Ying Tsou, Takayoshi Sasagawa, Kousei Yamabe, Shuhei Numata, Daisuke Higaki, Tomo Kiriu, Mutsumi S. Odagiri
Publikováno v:
Journal of the Japan Landslide Society. 58:109-117
Publikováno v:
Landslides. 18:619-627
The number of natural disasters induced by rainfall events in Taiwan has soared, with typhoons and torrential rains invariably inducing major landslides. In this study, data on major rainfall-generated landslides (605 in total) which occurred between
Autor:
Manabu Koubu, Mio Kasai, Shinjiro Matsuo, Nobuaki Kato, Michiya Irasawa, Hiroyuki Matsusaka, Kenichi Arai, Shinji Hirose, Kazuhiro Sugawara, Ching-Ying Tsou, Masahiro Kaibori, Taeko Wakahara, Daisuke Higaki, Yoshiharu Ishikawa, Takashi Yamada, Satoshi Niwa, Takashi Koi, Mizuho Arai, Hajime Ikeda, Nobuyuki Tada, Hideki Kawabata, Toshiyuki Kon, Tatsuya Sato
Publikováno v:
International Journal of Erosion Control Engineering. 13:48-55
Autor:
Ching-Ying Tsou, Masahiro Chigira, Marc-Henri Derron, Benjamin Rudaz, Michel Jaboyedoff, Noriyuki Arai
Publikováno v:
Earth Surface Dynamics, Vol 7, Pp 439-458 (2019)
Reconstructions of failure surfaces (prior to potential landslides or after their release), landslide deposits, or other palaeotopographic features are important for hazard and erosion assessment. The volumes involved in landslide and failure surface