Variability of teleconnections between the Atlantic subtropical high and the Indian monsoon low and related impacts on summer temperature over Egypt

Abstract A robust subtropical circulation index (SCI) is defined as the difference between the North Atlantic subtropical high and the Indian monsoon low. The SCI is negatively correlated to air temperatures over Egypt and is associated with large‐scale climate indices of the tropical and subtropica...

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Published in:Atmospheric Science Letters
Main Author: Hasanean, H. M.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2005
Subjects:
Online Access:http://dx.doi.org/10.1002/asl.113
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spelling crwiley:10.1002/asl.113 2024-06-02T08:11:11+00:00 Variability of teleconnections between the Atlantic subtropical high and the Indian monsoon low and related impacts on summer temperature over Egypt Hasanean, H. M. 2005 http://dx.doi.org/10.1002/asl.113 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl.113 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.113 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Atmospheric Science Letters volume 6, issue 3, page 176-182 ISSN 1530-261X 1530-261X journal-article 2005 crwiley https://doi.org/10.1002/asl.113 2024-05-03T11:05:22Z Abstract A robust subtropical circulation index (SCI) is defined as the difference between the North Atlantic subtropical high and the Indian monsoon low. The SCI is negatively correlated to air temperatures over Egypt and is associated with large‐scale climate indices of the tropical and subtropical Atlantic sector. Copyright © 2005 Royal Meteorological Society Article in Journal/Newspaper North Atlantic Wiley Online Library Indian Atmospheric Science Letters 6 3 176 182
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract A robust subtropical circulation index (SCI) is defined as the difference between the North Atlantic subtropical high and the Indian monsoon low. The SCI is negatively correlated to air temperatures over Egypt and is associated with large‐scale climate indices of the tropical and subtropical Atlantic sector. Copyright © 2005 Royal Meteorological Society
format Article in Journal/Newspaper
author Hasanean, H. M.
spellingShingle Hasanean, H. M.
Variability of teleconnections between the Atlantic subtropical high and the Indian monsoon low and related impacts on summer temperature over Egypt
author_facet Hasanean, H. M.
author_sort Hasanean, H. M.
title Variability of teleconnections between the Atlantic subtropical high and the Indian monsoon low and related impacts on summer temperature over Egypt
title_short Variability of teleconnections between the Atlantic subtropical high and the Indian monsoon low and related impacts on summer temperature over Egypt
title_full Variability of teleconnections between the Atlantic subtropical high and the Indian monsoon low and related impacts on summer temperature over Egypt
title_fullStr Variability of teleconnections between the Atlantic subtropical high and the Indian monsoon low and related impacts on summer temperature over Egypt
title_full_unstemmed Variability of teleconnections between the Atlantic subtropical high and the Indian monsoon low and related impacts on summer temperature over Egypt
title_sort variability of teleconnections between the atlantic subtropical high and the indian monsoon low and related impacts on summer temperature over egypt
publisher Wiley
publishDate 2005
url http://dx.doi.org/10.1002/asl.113
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl.113
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.113
geographic Indian
geographic_facet Indian
genre North Atlantic
genre_facet North Atlantic
op_source Atmospheric Science Letters
volume 6, issue 3, page 176-182
ISSN 1530-261X 1530-261X
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/asl.113
container_title Atmospheric Science Letters
container_volume 6
container_issue 3
container_start_page 176
op_container_end_page 182
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