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Landscapes of the Kara Sea. / Bobkov, A.A.; Drabkin, V.V.; Karklin, V.P.

Proceedings of the 24th International Symposium on Okhotsk Sea and Sea Ice. Mombetsu, 15-19 February, 2009. The Okhotsk Sea & Cold Ocean Research Association (OSCORA), 2009. p. 199-204.

Research output: Chapter in Book/Report/Conference proceeding › Article in an anthology › Research

Harvard

Bobkov, AA, Drabkin, VV & Karklin, VP 2009, Landscapes of the Kara Sea. in Proceedings of the 24th International Symposium on Okhotsk Sea and Sea Ice. Mombetsu, 15-19 February, 2009. The Okhotsk Sea & Cold Ocean Research Association (OSCORA), pp. 199-204.

APA

Bobkov, A. A., Drabkin, V. V., & Karklin, V. P. (2009). Landscapes of the Kara Sea. In Proceedings of the 24th International Symposium on Okhotsk Sea and Sea Ice. Mombetsu, 15-19 February, 2009 (pp. 199-204). The Okhotsk Sea & Cold Ocean Research Association (OSCORA).

Vancouver

Bobkov AA, Drabkin VV, Karklin VP. Landscapes of the Kara Sea. In Proceedings of the 24th International Symposium on Okhotsk Sea and Sea Ice. Mombetsu, 15-19 February, 2009. The Okhotsk Sea & Cold Ocean Research Association (OSCORA). 2009. p. 199-204

Author

Bobkov, A.A. ; Drabkin, V.V. ; Karklin, V.P. / Landscapes of the Kara Sea. Proceedings of the 24th International Symposium on Okhotsk Sea and Sea Ice. Mombetsu, 15-19 February, 2009. The Okhotsk Sea & Cold Ocean Research Association (OSCORA), 2009. pp. 199-204

BibTeX

@inbook{f324a9e999d64f59ba0e5c423e4a7c62,
title = "Landscapes of the Kara Sea",
abstract = "Ice cover of the Kara Sea is main functional link in physico-geographical processes determining many features of its hydrological, meteorological and biological regimes. Its forming is usually determined by two principal stages in seasonal development: 1) autumnal-wintry period, during which the ice formation and growth of ice occur, and, 2) spring-summer one, when melting and destruction of ice occur. Common viewpoint shows that landscapes of the Kara Sea could be divided into: 1) water-ice item characterizing by covering of total sea area less than 50%, and, 2) ice-water, taken up to 50 and more percentages of sea surfaces. Both types of landscapes belong to non-stable system in which correlation between the open water and ice surface continuously vary. However, few relatively stable structures are very well observed in such distribution, namely: 1) fast ice, 2) flaw polynyas, 3) ice massive, and, 4) because of the considerable flow into Kara Sea with Ob` and Enisey rivers, it is reasonably to distinguish",
author = "A.A. Bobkov and V.V. Drabkin and V.P. Karklin",
year = "2009",
language = "English",
pages = "199--204",
booktitle = "Proceedings of the 24th International Symposium on Okhotsk Sea and Sea Ice. Mombetsu, 15-19 February, 2009",
publisher = "The Okhotsk Sea & Cold Ocean Research Association (OSCORA)",
address = "International organisation",

}

RIS

TY - CHAP

T1 - Landscapes of the Kara Sea

AU - Bobkov, A.A.

AU - Drabkin, V.V.

AU - Karklin, V.P.

PY - 2009

Y1 - 2009

N2 - Ice cover of the Kara Sea is main functional link in physico-geographical processes determining many features of its hydrological, meteorological and biological regimes. Its forming is usually determined by two principal stages in seasonal development: 1) autumnal-wintry period, during which the ice formation and growth of ice occur, and, 2) spring-summer one, when melting and destruction of ice occur. Common viewpoint shows that landscapes of the Kara Sea could be divided into: 1) water-ice item characterizing by covering of total sea area less than 50%, and, 2) ice-water, taken up to 50 and more percentages of sea surfaces. Both types of landscapes belong to non-stable system in which correlation between the open water and ice surface continuously vary. However, few relatively stable structures are very well observed in such distribution, namely: 1) fast ice, 2) flaw polynyas, 3) ice massive, and, 4) because of the considerable flow into Kara Sea with Ob` and Enisey rivers, it is reasonably to distinguish

AB - Ice cover of the Kara Sea is main functional link in physico-geographical processes determining many features of its hydrological, meteorological and biological regimes. Its forming is usually determined by two principal stages in seasonal development: 1) autumnal-wintry period, during which the ice formation and growth of ice occur, and, 2) spring-summer one, when melting and destruction of ice occur. Common viewpoint shows that landscapes of the Kara Sea could be divided into: 1) water-ice item characterizing by covering of total sea area less than 50%, and, 2) ice-water, taken up to 50 and more percentages of sea surfaces. Both types of landscapes belong to non-stable system in which correlation between the open water and ice surface continuously vary. However, few relatively stable structures are very well observed in such distribution, namely: 1) fast ice, 2) flaw polynyas, 3) ice massive, and, 4) because of the considerable flow into Kara Sea with Ob` and Enisey rivers, it is reasonably to distinguish

M3 - Article in an anthology

SP - 199

EP - 204

BT - Proceedings of the 24th International Symposium on Okhotsk Sea and Sea Ice. Mombetsu, 15-19 February, 2009

PB - The Okhotsk Sea & Cold Ocean Research Association (OSCORA)

ER -

ID: 4486370