Zobrazeno 1 - 10
of 85
pro vyhledávání: '"M. Nakawo"'
Publikováno v:
Geophysical Research Letters. 31
[1] An extended deuterium excess (d or d-excess) record covering the last three glacial-interglacial cycles (ca. 340,000 years) was obtained from the Dome Fuji ice core, Antarctica. In order to interpret the Antarctic d record as a climatic history o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::218f86b67e805dfccf4a26f8009ccd34
https://doi.org/10.1029/2004gl019954
https://doi.org/10.1029/2004gl019954
Autor:
M. Nakawo, N.K. Sinha
Publikováno v:
Atmosphere-Ocean. 22:193-206
Brine layer spacing has been measured in a core sample taken 19 January 1978 from Eclipse Sound, Baffin Island, Canada. Observations on snow and ice conditions and a record of air temperatures for the entire growth season allowed correlation of the b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::32c6ee7817e00e10eaa18bd1a7edfc04
https://doi.org/10.1080/07055900.1984.9649193
https://doi.org/10.1080/07055900.1984.9649193
Autor:
M. Nakawo, N. K. Sinha
Publikováno v:
Journal of Glaciology. 27:315-330
This paper describes the growth of sea ice and the salinity profiles observed in Eclipse Sound near Pond Inlet, Baffin Island, Canada, during the winter of 1977–78. A numerical method of calculation has been developed to incorporate the variations
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::462f05f81f9e1fe6dcae504badddcf80
https://doi.org/10.1017/s0022143000015409
https://doi.org/10.1017/s0022143000015409
Autor:
N. K. Sinha, M. Nakawo
Publikováno v:
Canadian Geotechnical Journal. 18:17-23
A simple numerical integration method has been developed for predicting growth of ice under snow cover where solar radiation does not play a dominant role. The method is capable of incorporating variations in snow conditions and physical properties o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bfb7b7d6fb86b3a9e2c0ad3be1346a19
https://doi.org/10.1139/t81-003
https://doi.org/10.1139/t81-003
Autor:
M. Nakawo
Publikováno v:
Journal of Glaciology. 22:273-283
Field investigations of supraglacial debris were carried out during the monsoon season in 1974 on G2 glacier near Tukche Peak in Hidden Valley, Mukut Himal, Nepal. The thickness of the debris layer was observed to increase down-glacier. Laboratory an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2a3ebe13075d36b3240c5bda5c49f06a
https://doi.org/10.3189/s002214300001426x
https://doi.org/10.3189/s002214300001426x
Autor:
G.J. Young, M. Nakawo
Publikováno v:
Journal of Glaciology. 28:29-34
A simple model suggests that th e a bl ati on under a debris la yer could be estimated from meteorological variables if th e surface temperat ure data of the layer are available. This method was tested by a nal yz in g the data o btained from ex peri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::24665a98388a76cb42c5c28e8f400f4b
https://doi.org/10.3189/s002214300001176x
https://doi.org/10.3189/s002214300001176x
Autor:
G.J. Young, M. Nakawo
Publikováno v:
Annals of Glaciology. 2:85-91
Ablation of glacier ice has been observed with artificial debris layers prepared with Ottawa sand (ASTM C-109) ranging from 0.01 to 0.1 m thick. Data on external variables observed during the experiments and determination of physical constants of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8ec85069146b28556c96725b72ce7a4a
https://doi.org/10.3189/172756481794352432
https://doi.org/10.3189/172756481794352432
Publikováno v:
Memoirs of National Institute of Polar Research. Special issue. 7:235-244
The flow velocity of about 2500m/year was obtained for the Shirase Glacier (70°S; 39°E), East Antarctica, by the analyses of aerophotographs taken in 1969 and 1975. Thicknesses of icebergs near the termini of the glaciers located along the Soya Coa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::6fe54a834bb89355fa2d79efb705e5f2
http://id.nii.ac.jp/1291/00000867/
http://id.nii.ac.jp/1291/00000867/
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Publikováno v:
Annals of Glaciology. 8:129-131
The thickness of supraglacial debris on the Khumbu Glacier, Nepal Himalaya, has been mapped by a combination of direct measurements and morphological and lithological studies. All three processes, englacial, supraglacial, and subglacial, must be cons
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::397c741a65f7856a73a0c180972410b4
https://doi.org/10.3189/s0260305500001294
https://doi.org/10.3189/s0260305500001294