Standard

Interrelation between climate variation in the arctic and at middle and low latitudes. / Alekseev, G. V.; Aleksandrov, E. I.; Svyashchennikov, P. N.; Kharlanenkova, N. E.

в: Russian Meteorology and Hydrology, № 6, 2000, стр. 1-11.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Alekseev, GV, Aleksandrov, EI, Svyashchennikov, PN & Kharlanenkova, NE 2000, 'Interrelation between climate variation in the arctic and at middle and low latitudes', Russian Meteorology and Hydrology, № 6, стр. 1-11.

APA

Alekseev, G. V., Aleksandrov, E. I., Svyashchennikov, P. N., & Kharlanenkova, N. E. (2000). Interrelation between climate variation in the arctic and at middle and low latitudes. Russian Meteorology and Hydrology, (6), 1-11.

Vancouver

Alekseev GV, Aleksandrov EI, Svyashchennikov PN, Kharlanenkova NE. Interrelation between climate variation in the arctic and at middle and low latitudes. Russian Meteorology and Hydrology. 2000;(6):1-11.

Author

Alekseev, G. V. ; Aleksandrov, E. I. ; Svyashchennikov, P. N. ; Kharlanenkova, N. E. / Interrelation between climate variation in the arctic and at middle and low latitudes. в: Russian Meteorology and Hydrology. 2000 ; № 6. стр. 1-11.

BibTeX

@article{06b9048dc5ec4c499593a134265bedb2,
title = "Interrelation between climate variation in the arctic and at middle and low latitudes",
abstract = "The temperature anomalies in the Arctic and at the extra-Arctic latitudes in winter are generally correlated negatively over periods shorter than ten years and positively for longer periods. A spatial distribution of air temperature anomalies at the arctic and adjacent latitudes at significant deviations of mean air temperature from the norms is characterized in winter by two opposite-sign anomalies. More than that, it is obvious that the pressure difference between the centers of the Azores high and the Icelandic low (the North Atlantic Oscillation index) increases in winter warming and decreases in cooling. The reaction of the Arctic to the climatic characteristics at middle and low latitudes is connected first of all with the variations in the area of sea ice and in the freshwater content in the Arctic Ocean and with their outflow into the North Atlantic.",
author = "Alekseev, {G. V.} and Aleksandrov, {E. I.} and Svyashchennikov, {P. N.} and Kharlanenkova, {N. E.}",
year = "2000",
language = "English",
pages = "1--11",
journal = "Russian Meteorology and Hydrology",
issn = "1068-3739",
publisher = "Allerton Press, Inc.",
number = "6",

}

RIS

TY - JOUR

T1 - Interrelation between climate variation in the arctic and at middle and low latitudes

AU - Alekseev, G. V.

AU - Aleksandrov, E. I.

AU - Svyashchennikov, P. N.

AU - Kharlanenkova, N. E.

PY - 2000

Y1 - 2000

N2 - The temperature anomalies in the Arctic and at the extra-Arctic latitudes in winter are generally correlated negatively over periods shorter than ten years and positively for longer periods. A spatial distribution of air temperature anomalies at the arctic and adjacent latitudes at significant deviations of mean air temperature from the norms is characterized in winter by two opposite-sign anomalies. More than that, it is obvious that the pressure difference between the centers of the Azores high and the Icelandic low (the North Atlantic Oscillation index) increases in winter warming and decreases in cooling. The reaction of the Arctic to the climatic characteristics at middle and low latitudes is connected first of all with the variations in the area of sea ice and in the freshwater content in the Arctic Ocean and with their outflow into the North Atlantic.

AB - The temperature anomalies in the Arctic and at the extra-Arctic latitudes in winter are generally correlated negatively over periods shorter than ten years and positively for longer periods. A spatial distribution of air temperature anomalies at the arctic and adjacent latitudes at significant deviations of mean air temperature from the norms is characterized in winter by two opposite-sign anomalies. More than that, it is obvious that the pressure difference between the centers of the Azores high and the Icelandic low (the North Atlantic Oscillation index) increases in winter warming and decreases in cooling. The reaction of the Arctic to the climatic characteristics at middle and low latitudes is connected first of all with the variations in the area of sea ice and in the freshwater content in the Arctic Ocean and with their outflow into the North Atlantic.

UR - http://www.scopus.com/inward/record.url?scp=0034437869&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0034437869

SP - 1

EP - 11

JO - Russian Meteorology and Hydrology

JF - Russian Meteorology and Hydrology

SN - 1068-3739

IS - 6

ER -

ID: 95474903