Tropospheric temperature anomalies in the Northern Hemisphere 1977–1986

Abstract Tropospheric temperatures for the Northern Hemisphere (NH) during the period 1977–1986 are analysed on the basis of 300/1000 mbar thickness data between latitudes 10 °N and 80 °N. The departures from the mean 1951–1960 are determined on a 10 ° by 10° grid. Averages and trends are calculated...

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Published in:International Journal of Climatology
Main Author: Weber, Gerd‐Rainer
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1990
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.3370100103
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spelling crwiley:10.1002/joc.3370100103 2024-06-02T08:02:31+00:00 Tropospheric temperature anomalies in the Northern Hemisphere 1977–1986 Weber, Gerd‐Rainer 1990 http://dx.doi.org/10.1002/joc.3370100103 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.3370100103 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.3370100103 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 10, issue 1, page 3-19 ISSN 0899-8418 1097-0088 journal-article 1990 crwiley https://doi.org/10.1002/joc.3370100103 2024-05-03T10:35:31Z Abstract Tropospheric temperatures for the Northern Hemisphere (NH) during the period 1977–1986 are analysed on the basis of 300/1000 mbar thickness data between latitudes 10 °N and 80 °N. The departures from the mean 1951–1960 are determined on a 10 ° by 10° grid. Averages and trends are calculated for latitude circles for the entire NH, separately for oceanic and continental areas, as well as for specific geographic regions. An attempt is made to find relationships between the anomaly patterns by means of teleconnections. It is found that in the 10–year period the tropical and subtropical troposphere was considerably warmer than during the reference period and that this positive anomaly was particularly prominent over the tropical and subtropical Pacific. The northern Pacific, the northern Atlantic, and the European‐Canadian sector of the Arctic showed coincident negative anomalies. The resulting increase in subtropical to mid‐latitude tropospheric temperature gradient over both oceans was calculated to be more than 1 K, indicating an intensified circulation during the period. Using teleconnections for various latitude and longitude sectors it can be shown that the NH anomaly pattern 1977–1986 is strongly influenced by variations in the thickness pattern over the subtropical Pacific along latitude circle 20°N. The strongest relations emerge between the subtropical Pacific and western North America, the East Atlantic, and central Asia, where over 60 per cent of the variances in thickness can be explained by thickness variations over the subtropical Pacific. Article in Journal/Newspaper Arctic Wiley Online Library Arctic Pacific International Journal of Climatology 10 1 3 19
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Tropospheric temperatures for the Northern Hemisphere (NH) during the period 1977–1986 are analysed on the basis of 300/1000 mbar thickness data between latitudes 10 °N and 80 °N. The departures from the mean 1951–1960 are determined on a 10 ° by 10° grid. Averages and trends are calculated for latitude circles for the entire NH, separately for oceanic and continental areas, as well as for specific geographic regions. An attempt is made to find relationships between the anomaly patterns by means of teleconnections. It is found that in the 10–year period the tropical and subtropical troposphere was considerably warmer than during the reference period and that this positive anomaly was particularly prominent over the tropical and subtropical Pacific. The northern Pacific, the northern Atlantic, and the European‐Canadian sector of the Arctic showed coincident negative anomalies. The resulting increase in subtropical to mid‐latitude tropospheric temperature gradient over both oceans was calculated to be more than 1 K, indicating an intensified circulation during the period. Using teleconnections for various latitude and longitude sectors it can be shown that the NH anomaly pattern 1977–1986 is strongly influenced by variations in the thickness pattern over the subtropical Pacific along latitude circle 20°N. The strongest relations emerge between the subtropical Pacific and western North America, the East Atlantic, and central Asia, where over 60 per cent of the variances in thickness can be explained by thickness variations over the subtropical Pacific.
format Article in Journal/Newspaper
author Weber, Gerd‐Rainer
spellingShingle Weber, Gerd‐Rainer
Tropospheric temperature anomalies in the Northern Hemisphere 1977–1986
author_facet Weber, Gerd‐Rainer
author_sort Weber, Gerd‐Rainer
title Tropospheric temperature anomalies in the Northern Hemisphere 1977–1986
title_short Tropospheric temperature anomalies in the Northern Hemisphere 1977–1986
title_full Tropospheric temperature anomalies in the Northern Hemisphere 1977–1986
title_fullStr Tropospheric temperature anomalies in the Northern Hemisphere 1977–1986
title_full_unstemmed Tropospheric temperature anomalies in the Northern Hemisphere 1977–1986
title_sort tropospheric temperature anomalies in the northern hemisphere 1977–1986
publisher Wiley
publishDate 1990
url http://dx.doi.org/10.1002/joc.3370100103
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.3370100103
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.3370100103
geographic Arctic
Pacific
geographic_facet Arctic
Pacific
genre Arctic
genre_facet Arctic
op_source International Journal of Climatology
volume 10, issue 1, page 3-19
ISSN 0899-8418 1097-0088
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/joc.3370100103
container_title International Journal of Climatology
container_volume 10
container_issue 1
container_start_page 3
op_container_end_page 19
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