Northeast Atlantic Storm Activity and Its Uncertainty from the Late Nineteenth to the Twenty-First Century

Geostrophic wind speeds calculated from mean sea level pressure readings are used to derive time series of northeast Atlantic storminess. The technique of geostrophic wind speed triangles provides relatively homogeneous long-term storm activity data and is thus suited for statistical analyses. This...

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Published in:Journal of Climate
Main Authors: Krueger, O., Feser, F., Weisse, R
Format: Article in Journal/Newspaper
Language:English
Published: AMS 2019
Subjects:
Online Access:https://publications.hereon.de/id/36668
https://publications.hzg.de/id/36668
https://doi.org/10.1175/JCLI-D-18-0505.1
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spelling fthzgzmk:oai:publications.hereon.de:36668 2023-06-11T04:14:43+02:00 Northeast Atlantic Storm Activity and Its Uncertainty from the Late Nineteenth to the Twenty-First Century Krueger, O. Feser, F. Weisse, R 2019 https://publications.hereon.de/id/36668 https://publications.hzg.de/id/36668 https://doi.org/10.1175/JCLI-D-18-0505.1 en eng AMS https://dx.doi.org/10.1175/JCLI-D-18-0505.1 urn:issn:0894-8755 https://publications.hereon.de/id/36668 https://publications.hzg.de/id/36668 info:eu-repo/semantics/openAccess open_access oa_allgemein_hybrid issn:0894-8755 Krueger, O.; Feser, F.; Weisse, R: Northeast Atlantic Storm Activity and Its Uncertainty from the Late Nineteenth to the Twenty-First Century. In: Journal of Climate. Vol. 32 (2019) 6, 1919 - 1931. (DOI: /10.1175/JCLI-D-18-0505.1) info:eu-repo/semantics/article Zeitschrift Artikel 2019 fthzgzmk https://doi.org/10.1175/JCLI-D-18-0505.1 2023-05-28T23:24:46Z Geostrophic wind speeds calculated from mean sea level pressure readings are used to derive time series of northeast Atlantic storminess. The technique of geostrophic wind speed triangles provides relatively homogeneous long-term storm activity data and is thus suited for statistical analyses. This study makes use of historical air pressure data available from the International Surface Pressure Databank (ISPD) complemented with data from the Danish and Norwegian Meteorological Institutes. For the first time the time series of northeast Atlantic storminess is extended until the most recent year available, i. e. 2016. A multi-decadal increasing trend in storm activity starting in the mid-1960s until the 1990s, whose high storminess levels are comparable to those found in the late 19th century, initiated debate whether this would already be a sign of climate change. This study confirms that long-term storminess levels have returned to average values in recent years and that the multidecadal increase is part of an extended interdecadal oscillation. In addition, new storm activity uncertainty estimates were developed and novel insights into the connection with the North Atlantic Oscillation (NAO) are provided. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Northeast Atlantic Hereon Publications (Helmholtz-Zentrum) Journal of Climate 32 6 1919 1931
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collection Hereon Publications (Helmholtz-Zentrum)
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language English
description Geostrophic wind speeds calculated from mean sea level pressure readings are used to derive time series of northeast Atlantic storminess. The technique of geostrophic wind speed triangles provides relatively homogeneous long-term storm activity data and is thus suited for statistical analyses. This study makes use of historical air pressure data available from the International Surface Pressure Databank (ISPD) complemented with data from the Danish and Norwegian Meteorological Institutes. For the first time the time series of northeast Atlantic storminess is extended until the most recent year available, i. e. 2016. A multi-decadal increasing trend in storm activity starting in the mid-1960s until the 1990s, whose high storminess levels are comparable to those found in the late 19th century, initiated debate whether this would already be a sign of climate change. This study confirms that long-term storminess levels have returned to average values in recent years and that the multidecadal increase is part of an extended interdecadal oscillation. In addition, new storm activity uncertainty estimates were developed and novel insights into the connection with the North Atlantic Oscillation (NAO) are provided.
format Article in Journal/Newspaper
author Krueger, O.
Feser, F.
Weisse, R
spellingShingle Krueger, O.
Feser, F.
Weisse, R
Northeast Atlantic Storm Activity and Its Uncertainty from the Late Nineteenth to the Twenty-First Century
author_facet Krueger, O.
Feser, F.
Weisse, R
author_sort Krueger, O.
title Northeast Atlantic Storm Activity and Its Uncertainty from the Late Nineteenth to the Twenty-First Century
title_short Northeast Atlantic Storm Activity and Its Uncertainty from the Late Nineteenth to the Twenty-First Century
title_full Northeast Atlantic Storm Activity and Its Uncertainty from the Late Nineteenth to the Twenty-First Century
title_fullStr Northeast Atlantic Storm Activity and Its Uncertainty from the Late Nineteenth to the Twenty-First Century
title_full_unstemmed Northeast Atlantic Storm Activity and Its Uncertainty from the Late Nineteenth to the Twenty-First Century
title_sort northeast atlantic storm activity and its uncertainty from the late nineteenth to the twenty-first century
publisher AMS
publishDate 2019
url https://publications.hereon.de/id/36668
https://publications.hzg.de/id/36668
https://doi.org/10.1175/JCLI-D-18-0505.1
genre North Atlantic
North Atlantic oscillation
Northeast Atlantic
genre_facet North Atlantic
North Atlantic oscillation
Northeast Atlantic
op_source issn:0894-8755
Krueger, O.; Feser, F.; Weisse, R: Northeast Atlantic Storm Activity and Its Uncertainty from the Late Nineteenth to the Twenty-First Century. In: Journal of Climate. Vol. 32 (2019) 6, 1919 - 1931. (DOI: /10.1175/JCLI-D-18-0505.1)
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op_doi https://doi.org/10.1175/JCLI-D-18-0505.1
container_title Journal of Climate
container_volume 32
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container_start_page 1919
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