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Comparison of climate changes in 1981-2000 with paleoclimate anaologues of global warming. / Efimova, N. A.; Zhiltsova, E. L.; Lemeshko, N. A.; Strokina, L. A.

In: Russian Meteorology and Hydrology, No. 8, 01.12.2004, p. 11-15.

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Harvard

Efimova, NA, Zhiltsova, EL, Lemeshko, NA & Strokina, LA 2004, 'Comparison of climate changes in 1981-2000 with paleoclimate anaologues of global warming', Russian Meteorology and Hydrology, no. 8, pp. 11-15.

APA

Efimova, N. A., Zhiltsova, E. L., Lemeshko, N. A., & Strokina, L. A. (2004). Comparison of climate changes in 1981-2000 with paleoclimate anaologues of global warming. Russian Meteorology and Hydrology, (8), 11-15.

Vancouver

Efimova NA, Zhiltsova EL, Lemeshko NA, Strokina LA. Comparison of climate changes in 1981-2000 with paleoclimate anaologues of global warming. Russian Meteorology and Hydrology. 2004 Dec 1;(8):11-15.

Author

Efimova, N. A. ; Zhiltsova, E. L. ; Lemeshko, N. A. ; Strokina, L. A. / Comparison of climate changes in 1981-2000 with paleoclimate anaologues of global warming. In: Russian Meteorology and Hydrology. 2004 ; No. 8. pp. 11-15.

BibTeX

@article{1690ba8b27824b18953fa9d4184b1dd9,
title = "Comparison of climate changes in 1981-2000 with paleoclimate anaologues of global warming",
abstract = "Characteristic features of regional climate changes in all seasons of the 1990s with a record rise of annual mean global air temperature are considered. The results obtained are compared with estimates of the regional climate changes in the winter, spring, summer, and fall seasons of the 1980s. It is shown that the most substantial temperature changes over the 20-year period were observed in the same regions. Positive temperature anomalies and the area they cover increased in the 1990s in comparison to the 1980s. The estimates of climate changes for 1981-2000 are compared with paleoclimate analogues of global warming for the winter and summer seasons. It is concluded that, according to two independent empirical methods, quantitative estimates of the winter air temperature rise agree over large regions in Eurasia and North America.",
author = "Efimova, {N. A.} and Zhiltsova, {E. L.} and Lemeshko, {N. A.} and Strokina, {L. A.}",
year = "2004",
month = dec,
day = "1",
language = "English",
pages = "11--15",
journal = "Russian Meteorology and Hydrology",
issn = "1068-3739",
publisher = "Allerton Press, Inc.",
number = "8",

}

RIS

TY - JOUR

T1 - Comparison of climate changes in 1981-2000 with paleoclimate anaologues of global warming

AU - Efimova, N. A.

AU - Zhiltsova, E. L.

AU - Lemeshko, N. A.

AU - Strokina, L. A.

PY - 2004/12/1

Y1 - 2004/12/1

N2 - Characteristic features of regional climate changes in all seasons of the 1990s with a record rise of annual mean global air temperature are considered. The results obtained are compared with estimates of the regional climate changes in the winter, spring, summer, and fall seasons of the 1980s. It is shown that the most substantial temperature changes over the 20-year period were observed in the same regions. Positive temperature anomalies and the area they cover increased in the 1990s in comparison to the 1980s. The estimates of climate changes for 1981-2000 are compared with paleoclimate analogues of global warming for the winter and summer seasons. It is concluded that, according to two independent empirical methods, quantitative estimates of the winter air temperature rise agree over large regions in Eurasia and North America.

AB - Characteristic features of regional climate changes in all seasons of the 1990s with a record rise of annual mean global air temperature are considered. The results obtained are compared with estimates of the regional climate changes in the winter, spring, summer, and fall seasons of the 1980s. It is shown that the most substantial temperature changes over the 20-year period were observed in the same regions. Positive temperature anomalies and the area they cover increased in the 1990s in comparison to the 1980s. The estimates of climate changes for 1981-2000 are compared with paleoclimate analogues of global warming for the winter and summer seasons. It is concluded that, according to two independent empirical methods, quantitative estimates of the winter air temperature rise agree over large regions in Eurasia and North America.

UR - http://www.scopus.com/inward/record.url?scp=27644512932&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:27644512932

SP - 11

EP - 15

JO - Russian Meteorology and Hydrology

JF - Russian Meteorology and Hydrology

SN - 1068-3739

IS - 8

ER -

ID: 52206766