Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Gorow Wakahama"'
Autor:
Gorow WAKAHAMA
Publikováno v:
Journal of the Japanese Society of Snow and Ice. 79:581-600
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3fe2c0a735b0ad720ddf7de7dfba6839
https://doi.org/10.5331/seppyo.79.6_581
https://doi.org/10.5331/seppyo.79.6_581
Publikováno v:
Tellus B; Vol 38, No 5 (1986)
Oxygen isotopic composition, crystal types and the degree of riming of falling snow particles were simultaneously observed in order to determine the possible causes of short-term variation of the δ l8 O value together with the formation process of s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f2fd76fe5d9171331340125af1f0201e
http://www.tellusb.net/index.php/tellusb/article/view/15143
http://www.tellusb.net/index.php/tellusb/article/view/15143
Publikováno v:
Annals of Glaciology. 18:117-122
To investigate the internal structure and transformational processes from firn to ice of the Hisago snow patch on Daisetsu Mountain, Hokkaido, Japan, many drillings were made during the ablation period in 1986 and 1987. The ice cores were analyzed fo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8aacc6ab5485a1a6df1fe144d224cc6c
https://doi.org/10.1017/s0260305500011368
https://doi.org/10.1017/s0260305500011368
Publikováno v:
Annals of Glaciology. 18:107-112
In Hokkaido we have often experienced hazardous accidents, such as tower collapses and conductor breakage, caused by wet-snow accretion on transmission lines, and over many years have developed countermeasures for wet-snow accretion. Recently we have
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a6c6a9d4740e15f840d116a72ffacdf4
https://doi.org/10.1017/s0260305500011344
https://doi.org/10.1017/s0260305500011344
Autor:
Gorow Wakahama, Kazuhisa Tsuboki
Publikováno v:
Journal of the Meteorological Society of Japan. Ser. II. 70:77-93
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61b82c9fcc8476b4c77a76fbd76cc565
https://doi.org/10.2151/jmsj1965.70.1_77
https://doi.org/10.2151/jmsj1965.70.1_77
Publikováno v:
Journal of the Meteorological Society of Japan. Ser. II. 70:11-24
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::25e25e1b511278f1cde5e81c8ccaac56
https://doi.org/10.2151/jmsj1965.70.1_11
https://doi.org/10.2151/jmsj1965.70.1_11
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 8:869-872
We present three-dimensional (3D) displays of meteorological radar echoes. We made surfaces of precipitating clouds specified by some echo intensity (dBZ) by the marching cubes method, which is a high-resolution 3D surface construction algorithm. Sur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e049cfd56b70ed6e4fd0c94a6c05601
https://doi.org/10.1175/1520-0426(1991)008<0869:tddore>2.0.co
https://doi.org/10.1175/1520-0426(1991)008<0869:tddore>2.0.co
Publikováno v:
Journal of the Meteorological Society of Japan. Ser. II. 69:15-30
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::646ac87680cbf07e93cceeaae63c010b
https://doi.org/10.2151/jmsj1965.69.1_15
https://doi.org/10.2151/jmsj1965.69.1_15
Autor:
Yoshihiro Tachibana, Kazuhisa Tsuboki, Tatsuo Endoh, Gorow Wakahama, Tomomi Yamada, Yasushi Fujiyoshi
Publikováno v:
Journal of Applied Meteorology. 29:147-152
A best-fit power-law relationship (Z = 427 R1.09) between 1-minute integrated averages of snowfall rate (R) and radar reflectivity factor (Z) was determined on the basis of observations made by using high sensitivity snow gauges (accuracy 0.03 mm h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1889649a11214a76fe5c73597f18de8
https://doi.org/10.1175/1520-0450(1990)029<0147:doarfs>2.0.co
https://doi.org/10.1175/1520-0450(1990)029<0147:doarfs>2.0.co
Autor:
Hisashi, OZAWA, Gorow, WAKAHAMA
Publikováno v:
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology. 6:157
Glacier surge is a catastrophic glacier advance which can't be explained by variation in climate. We propose a "hydro-thermal instability" model which is capable of explaining surges of an inversion type glacier. An inversion type glacier has a cold
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::a9b8e394da87cb2df14db091db6a3665
http://id.nii.ac.jp/1291/00003760/
http://id.nii.ac.jp/1291/00003760/