Standard
Morphometry and internal structure of ice ridges in the kara and laptev seas. / Guzenko, Roman B.; Mironov, Yevgeny U.; Kharitonov, Victor V.; May, Ruslan I.; Porubaev, Viktor S.; Khotchenkov, Stepan V.; Kornishin, Konstantin A.; Efimov, Yaroslav O.; Tarasov, Petr A.
In:
International Journal of Offshore and Polar Engineering, Vol. 30, No. 2, 06.2020, p. 194-201.
Research output: Contribution to journal › Article › peer-review
Harvard
Guzenko, RB, Mironov, YU, Kharitonov, VV
, May, RI, Porubaev, VS, Khotchenkov, SV, Kornishin, KA, Efimov, YO & Tarasov, PA 2020, '
Morphometry and internal structure of ice ridges in the kara and laptev seas',
International Journal of Offshore and Polar Engineering, vol. 30, no. 2, pp. 194-201.
https://doi.org/10.17736/ijope.2020.jc784APA
Guzenko, R. B., Mironov, Y. U., Kharitonov, V. V.
, May, R. I., Porubaev, V. S., Khotchenkov, S. V., Kornishin, K. A., Efimov, Y. O., & Tarasov, P. A. (2020).
Morphometry and internal structure of ice ridges in the kara and laptev seas.
International Journal of Offshore and Polar Engineering,
30(2), 194-201.
https://doi.org/10.17736/ijope.2020.jc784Vancouver
Author
Guzenko, Roman B. ; Mironov, Yevgeny U. ; Kharitonov, Victor V.
; May, Ruslan I. ; Porubaev, Viktor S. ; Khotchenkov, Stepan V. ; Kornishin, Konstantin A. ; Efimov, Yaroslav O. ; Tarasov, Petr A. /
Morphometry and internal structure of ice ridges in the kara and laptev seas. In:
International Journal of Offshore and Polar Engineering. 2020 ; Vol. 30, No. 2. pp. 194-201.
BibTeX
@article{dfa14022b4a446b39bad164ca80f3e97,
title = "Morphometry and internal structure of ice ridges in the kara and laptev seas",
abstract = "The article presents an analysis of the expedition results on morphometry and the internal structure of ice ridges. A regression equation connecting the consolidated layer (CL) thickness of ice ridges with the sum of degree-days of frost is proposed. The issue of the CL distribution inside the ice ridge is considered. It is shown that the largest CL thickness is observed in the zone, combining the maximum sail and keel. The averaged porosity distribution by vertical is derived, and the main regularities of its change inside the ice ridge are shown.",
keywords = "Consolidated layer, Ice ridge, Internal structure, Keel, Porosity, Sail, Thermal drilling",
author = "Guzenko, {Roman B.} and Mironov, {Yevgeny U.} and Kharitonov, {Victor V.} and May, {Ruslan I.} and Porubaev, {Viktor S.} and Khotchenkov, {Stepan V.} and Kornishin, {Konstantin A.} and Efimov, {Yaroslav O.} and Tarasov, {Petr A.}",
note = "Funding Information: This study is supported by the Russian Foundation for Basic Research (Grant 18-05-60109). Studies were carried out in the framework of the innovation activity of the Rosneft Oil Company. Publisher Copyright: {\textcopyright} by The International Society of Offshore and Polar Engineers. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.",
year = "2020",
month = jun,
doi = "10.17736/ijope.2020.jc784",
language = "English",
volume = "30",
pages = "194--201",
journal = "International Journal of Offshore and Polar Engineering",
issn = "1053-5381",
publisher = "International Society of Offshore and Polar Engineers",
number = "2",
}
RIS
TY - JOUR
T1 - Morphometry and internal structure of ice ridges in the kara and laptev seas
AU - Guzenko, Roman B.
AU - Mironov, Yevgeny U.
AU - Kharitonov, Victor V.
AU - May, Ruslan I.
AU - Porubaev, Viktor S.
AU - Khotchenkov, Stepan V.
AU - Kornishin, Konstantin A.
AU - Efimov, Yaroslav O.
AU - Tarasov, Petr A.
N1 - Funding Information:
This study is supported by the Russian Foundation for Basic Research (Grant 18-05-60109). Studies were carried out in the framework of the innovation activity of the Rosneft Oil Company.
Publisher Copyright:
© by The International Society of Offshore and Polar Engineers.
Copyright:
Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2020/6
Y1 - 2020/6
N2 - The article presents an analysis of the expedition results on morphometry and the internal structure of ice ridges. A regression equation connecting the consolidated layer (CL) thickness of ice ridges with the sum of degree-days of frost is proposed. The issue of the CL distribution inside the ice ridge is considered. It is shown that the largest CL thickness is observed in the zone, combining the maximum sail and keel. The averaged porosity distribution by vertical is derived, and the main regularities of its change inside the ice ridge are shown.
AB - The article presents an analysis of the expedition results on morphometry and the internal structure of ice ridges. A regression equation connecting the consolidated layer (CL) thickness of ice ridges with the sum of degree-days of frost is proposed. The issue of the CL distribution inside the ice ridge is considered. It is shown that the largest CL thickness is observed in the zone, combining the maximum sail and keel. The averaged porosity distribution by vertical is derived, and the main regularities of its change inside the ice ridge are shown.
KW - Consolidated layer
KW - Ice ridge
KW - Internal structure
KW - Keel
KW - Porosity
KW - Sail
KW - Thermal drilling
UR - http://www.scopus.com/inward/record.url?scp=85086763424&partnerID=8YFLogxK
U2 - 10.17736/ijope.2020.jc784
DO - 10.17736/ijope.2020.jc784
M3 - Article
AN - SCOPUS:85086763424
VL - 30
SP - 194
EP - 201
JO - International Journal of Offshore and Polar Engineering
JF - International Journal of Offshore and Polar Engineering
SN - 1053-5381
IS - 2
ER -
