Climate impacts of the NAO are sensitive to how the NAO is defined
We analyze the sensitivity of the effects the North Atlantic Oscillation (NAO) exerts on surface temperature and precipitation in Europe to the definition of the NAO index. Seven different NAO indices are examined: two based on station sea level pressure (SLP) data, two based on action centers, and...
Published in: | Theoretical and Applied Climatology |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2015
|
Subjects: | |
Online Access: | https://doi.org/10.1007/s00704-014-1116-0 http://hdl.handle.net/11104/0236634 |
id |
ftczacademyscien:oai:asep.lib.cas.cz:CavUnEpca/0432100 |
---|---|
record_format |
openpolar |
spelling |
ftczacademyscien:oai:asep.lib.cas.cz:CavUnEpca/0432100 2024-02-04T10:02:26+01:00 Climate impacts of the NAO are sensitive to how the NAO is defined Pokorná, L. (Lucie) Huth, R. (Radan) 2015 https://doi.org/10.1007/s00704-014-1116-0 http://hdl.handle.net/11104/0236634 eng eng doi:10.1007/s00704-014-1116-0 urn:pissn: 0177-798x urn:eissn: 1434-4483 http://hdl.handle.net/11104/0236634 North-Atlantic-Oscillation atmospheric circulation winter temperature variability modes time variations Icelandic low precipitation surface frequency Europe info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftczacademyscien https://doi.org/10.1007/s00704-014-1116-0 2024-01-09T17:28:45Z We analyze the sensitivity of the effects the North Atlantic Oscillation (NAO) exerts on surface temperature and precipitation in Europe to the definition of the NAO index. Seven different NAO indices are examined: two based on station sea level pressure (SLP) data, two based on action centers, and three based on correlation/covariance structures described by principal component analysis (PCA). The analysis is based on monthly mean data; winter and summer seasons are analyzed separately. Temporal correlations between indices are weaker in summer than in winter for most pairs of indices. In particular, low correlations are found between station indices on the one hand and PCA-based indices on the other hand. The NAO effects are quantified by correlations between the indices and station data in Europe. Effects of the NAO on precipitation amount and wet day probability are very similar, while NAO effects on maximum temperature are stronger than those on minimum temperature. The sensitivity of the NAO effects on both surface temperature and precipitation to the choice of the NAO index is considerably higher in summer. Correlations differ among the NAO indices not only in their magnitude but in some regions in summer also in their sign. Article in Journal/Newspaper North Atlantic North Atlantic oscillation The Czech Academy of Sciences: Publication Activity (ASEP) Theoretical and Applied Climatology 119 3-4 639 652 |
institution |
Open Polar |
collection |
The Czech Academy of Sciences: Publication Activity (ASEP) |
op_collection_id |
ftczacademyscien |
language |
English |
topic |
North-Atlantic-Oscillation atmospheric circulation winter temperature variability modes time variations Icelandic low precipitation surface frequency Europe |
spellingShingle |
North-Atlantic-Oscillation atmospheric circulation winter temperature variability modes time variations Icelandic low precipitation surface frequency Europe Pokorná, L. (Lucie) Huth, R. (Radan) Climate impacts of the NAO are sensitive to how the NAO is defined |
topic_facet |
North-Atlantic-Oscillation atmospheric circulation winter temperature variability modes time variations Icelandic low precipitation surface frequency Europe |
description |
We analyze the sensitivity of the effects the North Atlantic Oscillation (NAO) exerts on surface temperature and precipitation in Europe to the definition of the NAO index. Seven different NAO indices are examined: two based on station sea level pressure (SLP) data, two based on action centers, and three based on correlation/covariance structures described by principal component analysis (PCA). The analysis is based on monthly mean data; winter and summer seasons are analyzed separately. Temporal correlations between indices are weaker in summer than in winter for most pairs of indices. In particular, low correlations are found between station indices on the one hand and PCA-based indices on the other hand. The NAO effects are quantified by correlations between the indices and station data in Europe. Effects of the NAO on precipitation amount and wet day probability are very similar, while NAO effects on maximum temperature are stronger than those on minimum temperature. The sensitivity of the NAO effects on both surface temperature and precipitation to the choice of the NAO index is considerably higher in summer. Correlations differ among the NAO indices not only in their magnitude but in some regions in summer also in their sign. |
format |
Article in Journal/Newspaper |
author |
Pokorná, L. (Lucie) Huth, R. (Radan) |
author_facet |
Pokorná, L. (Lucie) Huth, R. (Radan) |
author_sort |
Pokorná, L. (Lucie) |
title |
Climate impacts of the NAO are sensitive to how the NAO is defined |
title_short |
Climate impacts of the NAO are sensitive to how the NAO is defined |
title_full |
Climate impacts of the NAO are sensitive to how the NAO is defined |
title_fullStr |
Climate impacts of the NAO are sensitive to how the NAO is defined |
title_full_unstemmed |
Climate impacts of the NAO are sensitive to how the NAO is defined |
title_sort |
climate impacts of the nao are sensitive to how the nao is defined |
publishDate |
2015 |
url |
https://doi.org/10.1007/s00704-014-1116-0 http://hdl.handle.net/11104/0236634 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
doi:10.1007/s00704-014-1116-0 urn:pissn: 0177-798x urn:eissn: 1434-4483 http://hdl.handle.net/11104/0236634 |
op_doi |
https://doi.org/10.1007/s00704-014-1116-0 |
container_title |
Theoretical and Applied Climatology |
container_volume |
119 |
container_issue |
3-4 |
container_start_page |
639 |
op_container_end_page |
652 |
_version_ |
1789969112087134208 |