A likely outcome of the sunspot peaks’ influence on the North Atlantic Oscillation and Europe in winter
The effect on the North Atlantic Oscillation of 15 sunspot peaks depends on whether the Oscillation is in-phase or out-of-phase with the sunspot peaks. When it is in-phase the anomalies of sea-level pressure adds to the average pressure distribution, and when it is out-of-phase it subtracts from it....
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ftncar:oai:drupal-site.org:articles_14457 2023-07-30T04:05:07+02:00 A likely outcome of the sunspot peaks’ influence on the North Atlantic Oscillation and Europe in winter Van Loon, Harry (author) 2014-06-01 application/pdf http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-021-282 https://doi.org/10.1127/0941-2948/2014/0533 en eng Meteorlogische Zeitschrift http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-021-282 doi:10.1127/0941-2948/2014/0533 ark:/85065/d72r3snh Copyright Author(s) 2014. This work is distributed under the Creative Commons Attribution 3.0 License. Text article 2014 ftncar https://doi.org/10.1127/0941-2948/2014/0533 2023-07-17T18:16:58Z The effect on the North Atlantic Oscillation of 15 sunspot peaks depends on whether the Oscillation is in-phase or out-of-phase with the sunspot peaks. When it is in-phase the anomalies of sea-level pressure adds to the average pressure distribution, and when it is out-of-phase it subtracts from it. Consequently, the atmospheric conditions over Europe in a sunspot peak depends on whether the North Atlantic Oscillation is in- or out-of-phase with the sunspot peak. Article in Journal/Newspaper North Atlantic North Atlantic oscillation OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Meteorologische Zeitschrift 23 1 75 77 |
institution |
Open Polar |
collection |
OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) |
op_collection_id |
ftncar |
language |
English |
description |
The effect on the North Atlantic Oscillation of 15 sunspot peaks depends on whether the Oscillation is in-phase or out-of-phase with the sunspot peaks. When it is in-phase the anomalies of sea-level pressure adds to the average pressure distribution, and when it is out-of-phase it subtracts from it. Consequently, the atmospheric conditions over Europe in a sunspot peak depends on whether the North Atlantic Oscillation is in- or out-of-phase with the sunspot peak. |
author2 |
Van Loon, Harry (author) |
format |
Article in Journal/Newspaper |
title |
A likely outcome of the sunspot peaks’ influence on the North Atlantic Oscillation and Europe in winter |
spellingShingle |
A likely outcome of the sunspot peaks’ influence on the North Atlantic Oscillation and Europe in winter |
title_short |
A likely outcome of the sunspot peaks’ influence on the North Atlantic Oscillation and Europe in winter |
title_full |
A likely outcome of the sunspot peaks’ influence on the North Atlantic Oscillation and Europe in winter |
title_fullStr |
A likely outcome of the sunspot peaks’ influence on the North Atlantic Oscillation and Europe in winter |
title_full_unstemmed |
A likely outcome of the sunspot peaks’ influence on the North Atlantic Oscillation and Europe in winter |
title_sort |
likely outcome of the sunspot peaks’ influence on the north atlantic oscillation and europe in winter |
publishDate |
2014 |
url |
http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-021-282 https://doi.org/10.1127/0941-2948/2014/0533 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
Meteorlogische Zeitschrift http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-021-282 doi:10.1127/0941-2948/2014/0533 ark:/85065/d72r3snh |
op_rights |
Copyright Author(s) 2014. This work is distributed under the Creative Commons Attribution 3.0 License. |
op_doi |
https://doi.org/10.1127/0941-2948/2014/0533 |
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Meteorologische Zeitschrift |
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23 |
container_issue |
1 |
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75 |
op_container_end_page |
77 |
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1772816842457350144 |