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МЕЗОКЛИМАТ ПОЛИГОНА КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ И СОВРЕМЕННЫЕ ТЕНДЕНЦИИ ЕГО ИЗМЕНЕНИЯ. / Каюкова, Е.П.

In: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, Vol. 2010, No. 4, 01.12.2010, p. 32-46.

Research output: Contribution to journal › Article › peer-review

Harvard

Каюкова, ЕП 2010, 'МЕЗОКЛИМАТ ПОЛИГОНА КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ И СОВРЕМЕННЫЕ ТЕНДЕНЦИИ ЕГО ИЗМЕНЕНИЯ', ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, vol. 2010, no. 4, pp. 32-46.

APA

Каюкова, Е. П. (2010). МЕЗОКЛИМАТ ПОЛИГОНА КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ И СОВРЕМЕННЫЕ ТЕНДЕНЦИИ ЕГО ИЗМЕНЕНИЯ. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, 2010(4), 32-46.

Vancouver

Каюкова ЕП. МЕЗОКЛИМАТ ПОЛИГОНА КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ И СОВРЕМЕННЫЕ ТЕНДЕНЦИИ ЕГО ИЗМЕНЕНИЯ. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2010 Dec 1;2010(4):32-46.

Author

Каюкова, Е.П. / МЕЗОКЛИМАТ ПОЛИГОНА КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ И СОВРЕМЕННЫЕ ТЕНДЕНЦИИ ЕГО ИЗМЕНЕНИЯ. In: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2010 ; Vol. 2010, No. 4. pp. 32-46.

BibTeX

@article{2bebd5311cd14456a559e74512232710,
title = "МЕЗОКЛИМАТ ПОЛИГОНА КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ И СОВРЕМЕННЫЕ ТЕНДЕНЦИИ ЕГО ИЗМЕНЕНИЯ",
abstract = "Due to global warming the climate within the Second ridge of the Crimean mountains changes. The site of Crimean geological field training of St. Petersburg University is situated here. The past twelve years (1998-2009) were the warmest for the entire observation period (from 1929). Comparison of average annual temperatures of two periods (1998-2009 and 1929-1965) indicates the rise of temperature at 1,27° C. At present, there is a temperature increase of 0,37° C/10 years, mainly through August, and to a lesser extent through March and June. The mean value of the annual precipitation during the observation period from 1998 till 2009 is 560 mm (116% of the rate in 1939-1965). From 1998 up to present time, there is a negative trend in rainfall (with the dynamics of about 1 mm/year) mainly through June. The area belongs to the zone of insufficient humidity. The climate is semi-continental with the trend to decrease.",
keywords = "Climate change, Crimean mountains, Precipitation, Temperature",
author = "Е.П. Каюкова",
year = "2010",
month = dec,
day = "1",
language = "русский",
volume = "2010",
pages = "32--46",
journal = "Вестник Санкт-Петербургского университета. Науки о Земле",
issn = "2541-9668",
publisher = "Издательство Санкт-Петербургского университета",
number = "4",

}

RIS

TY - JOUR

T1 - МЕЗОКЛИМАТ ПОЛИГОНА КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ И СОВРЕМЕННЫЕ ТЕНДЕНЦИИ ЕГО ИЗМЕНЕНИЯ

AU - Каюкова, Е.П.

PY - 2010/12/1

Y1 - 2010/12/1

N2 - Due to global warming the climate within the Second ridge of the Crimean mountains changes. The site of Crimean geological field training of St. Petersburg University is situated here. The past twelve years (1998-2009) were the warmest for the entire observation period (from 1929). Comparison of average annual temperatures of two periods (1998-2009 and 1929-1965) indicates the rise of temperature at 1,27° C. At present, there is a temperature increase of 0,37° C/10 years, mainly through August, and to a lesser extent through March and June. The mean value of the annual precipitation during the observation period from 1998 till 2009 is 560 mm (116% of the rate in 1939-1965). From 1998 up to present time, there is a negative trend in rainfall (with the dynamics of about 1 mm/year) mainly through June. The area belongs to the zone of insufficient humidity. The climate is semi-continental with the trend to decrease.

AB - Due to global warming the climate within the Second ridge of the Crimean mountains changes. The site of Crimean geological field training of St. Petersburg University is situated here. The past twelve years (1998-2009) were the warmest for the entire observation period (from 1929). Comparison of average annual temperatures of two periods (1998-2009 and 1929-1965) indicates the rise of temperature at 1,27° C. At present, there is a temperature increase of 0,37° C/10 years, mainly through August, and to a lesser extent through March and June. The mean value of the annual precipitation during the observation period from 1998 till 2009 is 560 mm (116% of the rate in 1939-1965). From 1998 up to present time, there is a negative trend in rainfall (with the dynamics of about 1 mm/year) mainly through June. The area belongs to the zone of insufficient humidity. The climate is semi-continental with the trend to decrease.

KW - Climate change

KW - Crimean mountains

KW - Precipitation

KW - Temperature

UR - http://www.scopus.com/inward/record.url?scp=79952177516&partnerID=8YFLogxK

M3 - статья

VL - 2010

SP - 32

EP - 46

JO - Вестник Санкт-Петербургского университета. Науки о Земле

JF - Вестник Санкт-Петербургского университета. Науки о Земле

SN - 2541-9668

IS - 4

ER -

ID: 5182264