Influences of different definitions of the winter NAO index on NAO action centers and its relationship with SST
Winter North Atlantic Oscillation (NAO) indexes from observations based on various winter durations are compared. Results show that there are significant differences in the interannual and decadal variations of these NAO indexes. For the same data source, a different definition of winter duration ca...
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2019-09-01
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Online Access: | http://dx.doi.org/10.1080/16742834.2019.1628607 |
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doaj-cb594808d1224ecaa1252356e14210382021-03-02T08:45:43ZengKeAi Communications Co., Ltd.Atmospheric and Oceanic Science Letters1674-28342376-61232019-09-0112532032810.1080/16742834.2019.16286071628607Influences of different definitions of the winter NAO index on NAO action centers and its relationship with SSTYujie JING0Yangchun LI1Yongfu XU2Guangzhou FAN3Chengdu University of Information TechnologyInstitute of Atmospheric Physics, Chinese Academy of SciencesInstitute of Atmospheric Physics, Chinese Academy of SciencesChengdu University of Information TechnologyWinter North Atlantic Oscillation (NAO) indexes from observations based on various winter durations are compared. Results show that there are significant differences in the interannual and decadal variations of these NAO indexes. For the same data source, a different definition of winter duration can lead to different signs of NAO index in some years, which mainly appear to be in the period of decadal phase transition. The different winter durations induce different cycles of the observation-based NAO. The longer the winter duration, the stronger the decadal variation. The NAO defined by different winter durations also can generate different descriptions of the NAO action centers, including the position and movement. The longer the winter duration, the more southerly action centers appear to be. The movement of the action centers affects not only site-based NAO indexes but also those defined by other methods, such as empirical orthogonal function (EOF) analysis. The length of time used in EOF analysis has a great influence on the spatial pattern of the NAO mode, which results in a considerable difference between the corresponding NAO indexes. Regardless of which NAO index is used, the NAO-related SST anomalies show the same tripole pattern. The longer the winter duration, the more significant the relationship between the NAO and SST affected by the timescale of sea–air interaction.http://dx.doi.org/10.1080/16742834.2019.1628607NAO indexwinter durationperiodaction centerssea surface temperature |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Yujie JING Yangchun LI Yongfu XU Guangzhou FAN |
spellingShingle |
Yujie JING Yangchun LI Yongfu XU Guangzhou FAN Influences of different definitions of the winter NAO index on NAO action centers and its relationship with SST Atmospheric and Oceanic Science Letters NAO index winter duration period action centers sea surface temperature |
author_facet |
Yujie JING Yangchun LI Yongfu XU Guangzhou FAN |
author_sort |
Yujie JING |
title |
Influences of different definitions of the winter NAO index on NAO action centers and its relationship with SST |
title_short |
Influences of different definitions of the winter NAO index on NAO action centers and its relationship with SST |
title_full |
Influences of different definitions of the winter NAO index on NAO action centers and its relationship with SST |
title_fullStr |
Influences of different definitions of the winter NAO index on NAO action centers and its relationship with SST |
title_full_unstemmed |
Influences of different definitions of the winter NAO index on NAO action centers and its relationship with SST |
title_sort |
influences of different definitions of the winter nao index on nao action centers and its relationship with sst |
publisher |
KeAi Communications Co., Ltd. |
series |
Atmospheric and Oceanic Science Letters |
issn |
1674-2834 2376-6123 |
publishDate |
2019-09-01 |
description |
Winter North Atlantic Oscillation (NAO) indexes from observations based on various winter durations are compared. Results show that there are significant differences in the interannual and decadal variations of these NAO indexes. For the same data source, a different definition of winter duration can lead to different signs of NAO index in some years, which mainly appear to be in the period of decadal phase transition. The different winter durations induce different cycles of the observation-based NAO. The longer the winter duration, the stronger the decadal variation. The NAO defined by different winter durations also can generate different descriptions of the NAO action centers, including the position and movement. The longer the winter duration, the more southerly action centers appear to be. The movement of the action centers affects not only site-based NAO indexes but also those defined by other methods, such as empirical orthogonal function (EOF) analysis. The length of time used in EOF analysis has a great influence on the spatial pattern of the NAO mode, which results in a considerable difference between the corresponding NAO indexes. Regardless of which NAO index is used, the NAO-related SST anomalies show the same tripole pattern. The longer the winter duration, the more significant the relationship between the NAO and SST affected by the timescale of sea–air interaction. |
topic |
NAO index winter duration period action centers sea surface temperature |
url |
http://dx.doi.org/10.1080/16742834.2019.1628607 |
work_keys_str_mv |
AT yujiejing influencesofdifferentdefinitionsofthewinternaoindexonnaoactioncentersanditsrelationshipwithsst AT yangchunli influencesofdifferentdefinitionsofthewinternaoindexonnaoactioncentersanditsrelationshipwithsst AT yongfuxu influencesofdifferentdefinitionsofthewinternaoindexonnaoactioncentersanditsrelationshipwithsst AT guangzhoufan influencesofdifferentdefinitionsofthewinternaoindexonnaoactioncentersanditsrelationshipwithsst |
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1724240442163200000 |