The effect of the North Atlantic Oscillation on the Iraqi climate 1982-2000

In this study, we have analyzed the spatial and temporal correlation between the North Atlantic Oscillation (NAO) and the climate in Iraq, with a focus on precipitation, temperature, and number of Mediterranean cyclones. It was found that the influence of the NAO varies per climate indicator. For ex...

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Published in:Theoretical and Applied Climatology
Main Authors: Khidher, Salar Ali, Pilesjö, Petter
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2015
Subjects:
Online Access:https://lup.lub.lu.se/record/8195284
https://doi.org/10.1007/s00704-014-1327-4
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spelling ftulundlup:oai:lup.lub.lu.se:0407472e-40bb-45b5-b444-03795ee6718c 2023-05-15T17:31:39+02:00 The effect of the North Atlantic Oscillation on the Iraqi climate 1982-2000 Khidher, Salar Ali Pilesjö, Petter 2015 https://lup.lub.lu.se/record/8195284 https://doi.org/10.1007/s00704-014-1327-4 eng eng Springer https://lup.lub.lu.se/record/8195284 http://dx.doi.org/10.1007/s00704-014-1327-4 wos:000363061900027 scopus:84944276126 Theoretical and Applied Climatology; 122(3-4), pp 771-782 (2015) ISSN: 1434-4483 Meteorology and Atmospheric Sciences Climate Research contributiontojournal/article info:eu-repo/semantics/article text 2015 ftulundlup https://doi.org/10.1007/s00704-014-1327-4 2023-02-01T23:33:14Z In this study, we have analyzed the spatial and temporal correlation between the North Atlantic Oscillation (NAO) and the climate in Iraq, with a focus on precipitation, temperature, and number of Mediterranean cyclones. It was found that the influence of the NAO varies per climate indicator. For example, the influence is greater on precipitation than on temperature. One conclusion of the study is that the mean annual precipitation in Iraq increases during a negative phase of the NAO and decreases during a positive phase. In addition, the correlation between NAO and precipitation is more pronounced in the south of the country than in the middle and northern regions. Regarding the temporal correlation between NAO and precipitation, the influence of the NAO on Iraqi precipitation was found to be weak during the fall season, but to become more pronounced in the winter, culminating during the spring, and then vanishing in the summer. It was also concluded that when the NAO is in a positive phase, the area featuring a desert climate (Bwha) expands in Iraq, while the area featuring other climates decreases. During these years, both the Mediterranean climate (Csa) and the steppe climate (Bsha) cover a smaller part of the country due to the limited amount of precipitation. The opposite occurs during a negative phase of the NAO. Analysis of the number of Mediterranean cyclones that reach Iraq shows that there is no significant difference in the number of cyclones occurring during negative and positive phases of the NAO. However, there are differences in the strength of the cyclones. This study represents a first step in analyzing the relation between the NAO and the Iraqi climate and hopes to lead to further research. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Lund University Publications (LUP) Theoretical and Applied Climatology 122 3-4 771 782
institution Open Polar
collection Lund University Publications (LUP)
op_collection_id ftulundlup
language English
topic Meteorology and Atmospheric Sciences
Climate Research
spellingShingle Meteorology and Atmospheric Sciences
Climate Research
Khidher, Salar Ali
Pilesjö, Petter
The effect of the North Atlantic Oscillation on the Iraqi climate 1982-2000
topic_facet Meteorology and Atmospheric Sciences
Climate Research
description In this study, we have analyzed the spatial and temporal correlation between the North Atlantic Oscillation (NAO) and the climate in Iraq, with a focus on precipitation, temperature, and number of Mediterranean cyclones. It was found that the influence of the NAO varies per climate indicator. For example, the influence is greater on precipitation than on temperature. One conclusion of the study is that the mean annual precipitation in Iraq increases during a negative phase of the NAO and decreases during a positive phase. In addition, the correlation between NAO and precipitation is more pronounced in the south of the country than in the middle and northern regions. Regarding the temporal correlation between NAO and precipitation, the influence of the NAO on Iraqi precipitation was found to be weak during the fall season, but to become more pronounced in the winter, culminating during the spring, and then vanishing in the summer. It was also concluded that when the NAO is in a positive phase, the area featuring a desert climate (Bwha) expands in Iraq, while the area featuring other climates decreases. During these years, both the Mediterranean climate (Csa) and the steppe climate (Bsha) cover a smaller part of the country due to the limited amount of precipitation. The opposite occurs during a negative phase of the NAO. Analysis of the number of Mediterranean cyclones that reach Iraq shows that there is no significant difference in the number of cyclones occurring during negative and positive phases of the NAO. However, there are differences in the strength of the cyclones. This study represents a first step in analyzing the relation between the NAO and the Iraqi climate and hopes to lead to further research.
format Article in Journal/Newspaper
author Khidher, Salar Ali
Pilesjö, Petter
author_facet Khidher, Salar Ali
Pilesjö, Petter
author_sort Khidher, Salar Ali
title The effect of the North Atlantic Oscillation on the Iraqi climate 1982-2000
title_short The effect of the North Atlantic Oscillation on the Iraqi climate 1982-2000
title_full The effect of the North Atlantic Oscillation on the Iraqi climate 1982-2000
title_fullStr The effect of the North Atlantic Oscillation on the Iraqi climate 1982-2000
title_full_unstemmed The effect of the North Atlantic Oscillation on the Iraqi climate 1982-2000
title_sort effect of the north atlantic oscillation on the iraqi climate 1982-2000
publisher Springer
publishDate 2015
url https://lup.lub.lu.se/record/8195284
https://doi.org/10.1007/s00704-014-1327-4
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Theoretical and Applied Climatology; 122(3-4), pp 771-782 (2015)
ISSN: 1434-4483
op_relation https://lup.lub.lu.se/record/8195284
http://dx.doi.org/10.1007/s00704-014-1327-4
wos:000363061900027
scopus:84944276126
op_doi https://doi.org/10.1007/s00704-014-1327-4
container_title Theoretical and Applied Climatology
container_volume 122
container_issue 3-4
container_start_page 771
op_container_end_page 782
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