Zobrazeno 1 - 10
of 29
pro vyhledávání: '"Toshihiro Ozeki"'
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
The infiltration of melted snow water and rainwater into snow can drastically change the form of snow layers. This process is an important factor affecting wet snow avalanches. Accordingly, numerous field surveys and cold room experiments have been c
Externí odkaz:
https://doaj.org/article/e8f7b9a9565b460593135d16650ed8ac
Publikováno v:
Journal of the Japanese Society of Snow and Ice. 84:341-358
Publikováno v:
Bulletin of Glaciological Research. :43-51
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
The infiltration of melted snow water and rainwater into snow can drastically change the form of snow layers. This process is an important factor affecting wet snow avalanches. Accordingly, numerous field surveys and cold room experiments have been c
The Tenth Symposium on Polar Science/Ordinary sessions: [OM] Polar Meteorology and Glaciology, Wed. 4 Dec. / Entrance Hall (1st floor) , National Institute of Polar Research
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::b17f6c9e88ecbe8d426718edba9416e8
http://id.nii.ac.jp/1291/00015654/
http://id.nii.ac.jp/1291/00015654/
Publikováno v:
Journal of the Japanese Society of Snow and Ice. 79:497-509
The Ninth Symposium on Polar Science/Ordinary sessions: [OM] Polar meteorology and glaciology, Wed. 5 Dec. / Entrance Hall (1st floor), National Institute of Polar Research
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::bfd84f80cb01ec5f1439baf0fc6fad19
http://id.nii.ac.jp/1291/00015313/
http://id.nii.ac.jp/1291/00015313/
Autor:
Toshihiro Ozeki, Shotaro Uto, Takeshi Tamura, Daisuke Simizu, Shuki Ushio, Seita Hoshino, Haruhito Shimoda, Kazutaka Tateyama, Yasushi Fukamachi, Fuko Sugimoto, Kay I. Ohshima
Publikováno v:
Polar Science. 10:43-51
Under the Japanese Antarctic Research Expedition (JARE) program, sea-ice thickness has been routinely monitored off Lutzow–Holm Bay (East Antarctica) during the summer (mid-December to early January) since 2000/01, using an electromagnetic inductio
Publikováno v:
Cold Regions Science and Technology. 170:102956
Flow fingers develop due to the infiltration of snow meltwater or rain water into a dry snowpack. The width, spacing, and areal coverage of the flow finger path and occurrence of capillary barriers have been demonstrated using dye tracer experiments
Publikováno v:
Cold Regions Science and Technology. 169:102889
The surface hoar layer is known to be one of the most typical types of weak layers in dry slab avalanches. To investigate the features of snow cover, including the surface hoar layer, we developed apparatuses that make surface hoar artificially. Two