Standard

Soil moisture content and runoff in the extratropical part of the Northern Hemisphere under global warming. / Vinnikov, K. Y.; Lemeshko, N. A.; Speranskaya, N. A.

In: Meteorologiya i Gidrologiya, Vol. 3, 01.01.1990, p. 5-10.

Research output: Contribution to journalArticlepeer-review

Harvard

Vinnikov, KY, Lemeshko, NA & Speranskaya, NA 1990, 'Soil moisture content and runoff in the extratropical part of the Northern Hemisphere under global warming', Meteorologiya i Gidrologiya, vol. 3, pp. 5-10.

APA

Vinnikov, K. Y., Lemeshko, N. A., & Speranskaya, N. A. (1990). Soil moisture content and runoff in the extratropical part of the Northern Hemisphere under global warming. Meteorologiya i Gidrologiya, 3, 5-10.

Vancouver

Author

Vinnikov, K. Y. ; Lemeshko, N. A. ; Speranskaya, N. A. / Soil moisture content and runoff in the extratropical part of the Northern Hemisphere under global warming. In: Meteorologiya i Gidrologiya. 1990 ; Vol. 3. pp. 5-10.

BibTeX

@article{cc6060e6008b470e958bc469cde68e35,
title = "Soil moisture content and runoff in the extratropical part of the Northern Hemisphere under global warming",
abstract = "Estimation is made of the summer moisture content in the 1 m soil layer and the annual runoff under the global warming to 1° and 2°C. Calculations are based on a comprehensive method of determination of evaporation from the land surface and on analyzing paleoclimatic data for two past warm periods: 1) the Holocene optimum with the mean global air temperature higher by 1°C than the present one; and 2) the Mikulinsky interglacial epoch when the mean global air temperature was higher by 2°C. -English summary",
author = "Vinnikov, {K. Y.} and Lemeshko, {N. A.} and Speranskaya, {N. A.}",
year = "1990",
month = jan,
day = "1",
language = "русский",
volume = "3",
pages = "5--10",
journal = "Meteorologiya i Gidrologiya",
issn = "0130-2906",
publisher = "Научно-исследовательский центр космической гидрометеорологии Планета",

}

RIS

TY - JOUR

T1 - Soil moisture content and runoff in the extratropical part of the Northern Hemisphere under global warming

AU - Vinnikov, K. Y.

AU - Lemeshko, N. A.

AU - Speranskaya, N. A.

PY - 1990/1/1

Y1 - 1990/1/1

N2 - Estimation is made of the summer moisture content in the 1 m soil layer and the annual runoff under the global warming to 1° and 2°C. Calculations are based on a comprehensive method of determination of evaporation from the land surface and on analyzing paleoclimatic data for two past warm periods: 1) the Holocene optimum with the mean global air temperature higher by 1°C than the present one; and 2) the Mikulinsky interglacial epoch when the mean global air temperature was higher by 2°C. -English summary

AB - Estimation is made of the summer moisture content in the 1 m soil layer and the annual runoff under the global warming to 1° and 2°C. Calculations are based on a comprehensive method of determination of evaporation from the land surface and on analyzing paleoclimatic data for two past warm periods: 1) the Holocene optimum with the mean global air temperature higher by 1°C than the present one; and 2) the Mikulinsky interglacial epoch when the mean global air temperature was higher by 2°C. -English summary

UR - http://www.scopus.com/inward/record.url?scp=0025247464&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0025247464

VL - 3

SP - 5

EP - 10

JO - Meteorologiya i Gidrologiya

JF - Meteorologiya i Gidrologiya

SN - 0130-2906

ER -

ID: 52206864