Zobrazeno 1 - 10
of 390
pro vyhledávání: '"Stamukha"'
Autor:
K. A. Kornishin, P. A. Tarasov, Ya. O. Yefimov, Yu. P. Gudoshnikov, S. M. Kovalev, Ye. U. Mironov, Ye. I. Makarov, A. V. Nesterov
Publikováno v:
Лëд и снег, Vol 58, Iss 3, Pp 396-404 (2018)
The study was carried out to reveal characteristics of the ice regime of poorly explored water area of the Khatanga Bay in the South-Western part of the Laptev Sea. Actuality of the research is due to the high potential of hydrocarbon reserves in the
Externí odkaz:
https://doaj.org/article/2d12ba39fecc43ec853e1432e44c9686
Autor:
Valeria Selyuzhenok, Denis Demchev
Publikováno v:
Remote Sensing, Vol 13, Iss 18, p 3783 (2021)
For regional environmental studies it is important to know the location of the fast ice edge which affects the coastal processes in the Arctic. The aim of this study is to develop a new automated method for fast ice delineation from SAR imagery. The
Externí odkaz:
https://doaj.org/article/274c40fb0d734bdfb845964a97f7b1bf
Akademický článek
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Publikováno v:
Polar Research, Vol 36, Iss 1 (2017)
Accurate representation of fast ice in numerical models is important for realistic simulation of numerous sea-ice and ocean variables. In order to simulate seasonal and interannual variability of fast-ice extent, the mechanisms controlling fast-ice d
Externí odkaz:
https://doaj.org/article/872636e4420b44f4be60221c3da0e109
Autor:
Sergey M. Kovalev, Petr A. Tarasov, A. V. Nesterov, Ye. I. Makarov, Konstantin A. Kornishin, Ye. U. Mironov, Yu. P. Gudoshnikov, Ya. O. Yefimov
Publikováno v:
Lëd i Sneg, Vol 58, Iss 3, Pp 396-404 (2018)
The study was carried out to reveal characteristics of the ice regime of poorly explored water area of the Khatanga Bay in the South-Western part of the Laptev Sea. Actuality of the research is due to the high potential of hydrocarbon reserves in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cd58caf65afb23ce2729f9e41ba1d0a7
https://ice-snow.igras.ru/jour/article/view/490
https://ice-snow.igras.ru/jour/article/view/490
Publikováno v:
The Cryosphere, Vol 12, Pp 1699-1713 (2018)
GPS measurements reveal strong modulation of horizontal ice shelf and ice stream flow at a variety of tidal frequencies, most notably a fortnightly (Msf) frequency not present in the vertical tides themselves. Current theories largely fail to explain
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::853e8ddb9e678a7649c0c1166bc30597
https://www.the-cryosphere.net/12/1699/2018/tc-12-1699-2018.pdf
https://www.the-cryosphere.net/12/1699/2018/tc-12-1699-2018.pdf
Conference
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Publikováno v:
Ocean Engineering. 140:334-351
Massive ice pile-ups have been frequently observed in the conductor array of offshore jacket platforms in Bohai Sea. Once formed, such rubble piles were very difficult to clear manually and therefore studies on the ice rubble piles and their forming
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9c95b3141f5056abb660aae7aed977eb
https://doi.org/10.1016/j.oceaneng.2017.05.036
https://doi.org/10.1016/j.oceaneng.2017.05.036
Publikováno v:
Journal of Quaternary Science. 32:463-474
This is the peer reviewed version of the following article: Ruther, D.C., Winsborrow, M., Andreassen, K. & Forwick, M. (2017). Grounding line proximal sediment characteristics at a marine-based, late-stage ice stream margin. Journal of Quaternary Sci
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b151cc150ddf261987ada2a839d65f83
https://doi.org/10.1002/jqs.2939
https://doi.org/10.1002/jqs.2939
Autor:
Bradley P. Lipovsky, Eric M. Dunham
Publikováno v:
Journal of Geophysical Research: Earth Surface. 122:973-1003
The Whillans Ice Plain (WIP), Antarctica, experiences twice-daily tidally modulated stick-slip cycles. Slip events last about 30 minutes, have sliding velocities as high as ∼0.5 mm/s (15 km/yr), and have total slip ∼0.5 m. Slip events tend to occ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53980e127cd486207be734b0a7fedde9
https://doi.org/10.1002/2016jf004183
https://doi.org/10.1002/2016jf004183