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Albedo dependence on low clouds amount. / Vasilyeva, D. A.; Svyashchennikov, P. N.

In: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, Vol. 2003, No. 3, 2003, p. 129-131.

Research output: Contribution to journalArticlepeer-review

Harvard

Vasilyeva, DA & Svyashchennikov, PN 2003, 'Albedo dependence on low clouds amount', ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, vol. 2003, no. 3, pp. 129-131.

APA

Vasilyeva, D. A., & Svyashchennikov, P. N. (2003). Albedo dependence on low clouds amount. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, 2003(3), 129-131.

Vancouver

Vasilyeva DA, Svyashchennikov PN. Albedo dependence on low clouds amount. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2003;2003(3):129-131.

Author

Vasilyeva, D. A. ; Svyashchennikov, P. N. / Albedo dependence on low clouds amount. In: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2003 ; Vol. 2003, No. 3. pp. 129-131.

BibTeX

@article{4a855af586a34ef69cc0d8b9a27428d7,
title = "Albedo dependence on low clouds amount",
abstract = "Snow albedo dependence on low clouds amount is estimated in the Arctic Basin, including surface changes and different sun altitudes. Data of 6-hour observations of drifting stations {"}North Pole{"} were used. Albedo of snow depends on clouds amount, especially on skies, with 3-5 tenths cloud cover, but sun altitude has an influence too. Sun altitude and cloud amount influence on albedo is complex and requires joint investigations.",
author = "Vasilyeva, {D. A.} and Svyashchennikov, {P. N.}",
year = "2003",
language = "English",
volume = "2003",
pages = "129--131",
journal = "Вестник Санкт-Петербургского университета. Науки о Земле",
issn = "2541-9668",
publisher = "Издательство Санкт-Петербургского университета",
number = "3",

}

RIS

TY - JOUR

T1 - Albedo dependence on low clouds amount

AU - Vasilyeva, D. A.

AU - Svyashchennikov, P. N.

PY - 2003

Y1 - 2003

N2 - Snow albedo dependence on low clouds amount is estimated in the Arctic Basin, including surface changes and different sun altitudes. Data of 6-hour observations of drifting stations "North Pole" were used. Albedo of snow depends on clouds amount, especially on skies, with 3-5 tenths cloud cover, but sun altitude has an influence too. Sun altitude and cloud amount influence on albedo is complex and requires joint investigations.

AB - Snow albedo dependence on low clouds amount is estimated in the Arctic Basin, including surface changes and different sun altitudes. Data of 6-hour observations of drifting stations "North Pole" were used. Albedo of snow depends on clouds amount, especially on skies, with 3-5 tenths cloud cover, but sun altitude has an influence too. Sun altitude and cloud amount influence on albedo is complex and requires joint investigations.

UR - http://www.scopus.com/inward/record.url?scp=18444371470&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:18444371470

VL - 2003

SP - 129

EP - 131

JO - Вестник Санкт-Петербургского университета. Науки о Земле

JF - Вестник Санкт-Петербургского университета. Науки о Земле

SN - 2541-9668

IS - 3

ER -

ID: 95475156