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Advection and outgoing radiation-induced fluctuations of climate. / Alekseyev, G. V.; Podgornyy, I. A.; Svyashchennikov, P. N.

In: Doklady. Earth science sections, Vol. 315, No. 6, 11.1990, p. 46-49.

Research output: Contribution to journalArticlepeer-review

Harvard

Alekseyev, GV, Podgornyy, IA & Svyashchennikov, PN 1990, 'Advection and outgoing radiation-induced fluctuations of climate', Doklady. Earth science sections, vol. 315, no. 6, pp. 46-49.

APA

Alekseyev, G. V., Podgornyy, I. A., & Svyashchennikov, P. N. (1990). Advection and outgoing radiation-induced fluctuations of climate. Doklady. Earth science sections, 315(6), 46-49.

Vancouver

Alekseyev GV, Podgornyy IA, Svyashchennikov PN. Advection and outgoing radiation-induced fluctuations of climate. Doklady. Earth science sections. 1990 Nov;315(6):46-49.

Author

Alekseyev, G. V. ; Podgornyy, I. A. ; Svyashchennikov, P. N. / Advection and outgoing radiation-induced fluctuations of climate. In: Doklady. Earth science sections. 1990 ; Vol. 315, No. 6. pp. 46-49.

BibTeX

@article{e73b774aee774f46b24989570d756c7d,
title = "Advection and outgoing radiation-induced fluctuations of climate",
abstract = "Analysis of variations in the monthly-average air temperature of the Northern Hemisphere in the nodes of a regular grid (5° of latitude by 10° of longitude) for the period from 1891 to 1986 (based on data from the All-Union Meteorological Information Institute's data base (VNIIGMIMTsD)) revealed a strong inverse correlation between deviations of the average temperatures and anomalies of their lateral temperature distribution during the cold half of the year in nontropical latitudes of the Northern Hemisphere (85° to 25° N). This analysis of the relationship between the atmospheric temperature and its lateral variation reveals that advection and outgoing radiation-induced fluctuations in the average temperature represent the main components of its year-to-year climatic variation during the cold half of the year, and contribute a significant part of the variation for the year as a whole. These fluctuations provide a key to understanding the mechanism governing the natural year-to-year variation of temperature in the atmosphere produced by free and forced fluctuations of the atmospheric and oceanic circulations. Our data suggest that a more critical approach to interpretations that find a human influence in the time series of air temperatures is in order.",
author = "Alekseyev, {G. V.} and Podgornyy, {I. A.} and Svyashchennikov, {P. N.}",
year = "1990",
month = nov,
language = "English",
volume = "315",
pages = "46--49",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "6",

}

RIS

TY - JOUR

T1 - Advection and outgoing radiation-induced fluctuations of climate

AU - Alekseyev, G. V.

AU - Podgornyy, I. A.

AU - Svyashchennikov, P. N.

PY - 1990/11

Y1 - 1990/11

N2 - Analysis of variations in the monthly-average air temperature of the Northern Hemisphere in the nodes of a regular grid (5° of latitude by 10° of longitude) for the period from 1891 to 1986 (based on data from the All-Union Meteorological Information Institute's data base (VNIIGMIMTsD)) revealed a strong inverse correlation between deviations of the average temperatures and anomalies of their lateral temperature distribution during the cold half of the year in nontropical latitudes of the Northern Hemisphere (85° to 25° N). This analysis of the relationship between the atmospheric temperature and its lateral variation reveals that advection and outgoing radiation-induced fluctuations in the average temperature represent the main components of its year-to-year climatic variation during the cold half of the year, and contribute a significant part of the variation for the year as a whole. These fluctuations provide a key to understanding the mechanism governing the natural year-to-year variation of temperature in the atmosphere produced by free and forced fluctuations of the atmospheric and oceanic circulations. Our data suggest that a more critical approach to interpretations that find a human influence in the time series of air temperatures is in order.

AB - Analysis of variations in the monthly-average air temperature of the Northern Hemisphere in the nodes of a regular grid (5° of latitude by 10° of longitude) for the period from 1891 to 1986 (based on data from the All-Union Meteorological Information Institute's data base (VNIIGMIMTsD)) revealed a strong inverse correlation between deviations of the average temperatures and anomalies of their lateral temperature distribution during the cold half of the year in nontropical latitudes of the Northern Hemisphere (85° to 25° N). This analysis of the relationship between the atmospheric temperature and its lateral variation reveals that advection and outgoing radiation-induced fluctuations in the average temperature represent the main components of its year-to-year climatic variation during the cold half of the year, and contribute a significant part of the variation for the year as a whole. These fluctuations provide a key to understanding the mechanism governing the natural year-to-year variation of temperature in the atmosphere produced by free and forced fluctuations of the atmospheric and oceanic circulations. Our data suggest that a more critical approach to interpretations that find a human influence in the time series of air temperatures is in order.

UR - http://www.scopus.com/inward/record.url?scp=0025508997&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0025508997

VL - 315

SP - 46

EP - 49

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 6

ER -

ID: 95475459