Variability of Winter Storminess in the Eastern United States during the Twentieth Century from Tide Gauges
Interannual to multidecadal variability of winter storminess in the eastern United States was studied using water level measurements from coastal tide gauges. The proximity to the coast of the primary winter storm track in the region allows the use of tide gauges to study temporal modulations in the...
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Digital Commons @ University of South Florida
2013
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Online Access: | https://digitalcommons.usf.edu/msc_facpub/2098 https://doi.org/10.1175/JCLI-D-12-00561.1 |
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ftusouthflorida:oai:digitalcommons.usf.edu:msc_facpub-3093 2023-07-30T04:01:50+02:00 Variability of Winter Storminess in the Eastern United States during the Twentieth Century from Tide Gauges Thompson, Philip R. Mitchum, Gary T. Vonesch, Cedric Li, Jianke 2013-01-01T08:00:00Z https://digitalcommons.usf.edu/msc_facpub/2098 https://doi.org/10.1175/JCLI-D-12-00561.1 unknown Digital Commons @ University of South Florida https://digitalcommons.usf.edu/msc_facpub/2098 doi:10.1175/JCLI-D-12-00561.1 https://doi.org/10.1175/JCLI-D-12-00561.1 Marine Science Faculty Publications Extratropical cyclones Sea level Storm surges Storm tracks Arctic Oscillation Multidecadal variability Life Sciences article 2013 ftusouthflorida https://doi.org/10.1175/JCLI-D-12-00561.1 2023-07-13T21:07:39Z Interannual to multidecadal variability of winter storminess in the eastern United States was studied using water level measurements from coastal tide gauges. The proximity to the coast of the primary winter storm track in the region allows the use of tide gauges to study temporal modulations in the frequency of these storms. Storms were identified in high-passed, detided sea level anomalies in 20 gauges from all coasts of North America to assess variability in winter storminess along particular storm tracks. The primary result is a significant multidecadal increase in the number of storms affecting the southeastern United States from the early to late twentieth century. The authors propose that this change is due to an increased tendency for the jet stream to meander south over the eastern United States since the 1950s. This mechanism is supported by long-term changes in the large-scale sea level pressure pattern over North America. The nature of the multidecadal change in storm frequency is unclear, because limited tide gauge record lengths prevent distinguishing between a trend and an oscillation. Article in Journal/Newspaper Arctic University of South Florida St. Petersburg: Digital USFSP Arctic Journal of Climate 26 23 9713 9726 |
institution |
Open Polar |
collection |
University of South Florida St. Petersburg: Digital USFSP |
op_collection_id |
ftusouthflorida |
language |
unknown |
topic |
Extratropical cyclones Sea level Storm surges Storm tracks Arctic Oscillation Multidecadal variability Life Sciences |
spellingShingle |
Extratropical cyclones Sea level Storm surges Storm tracks Arctic Oscillation Multidecadal variability Life Sciences Thompson, Philip R. Mitchum, Gary T. Vonesch, Cedric Li, Jianke Variability of Winter Storminess in the Eastern United States during the Twentieth Century from Tide Gauges |
topic_facet |
Extratropical cyclones Sea level Storm surges Storm tracks Arctic Oscillation Multidecadal variability Life Sciences |
description |
Interannual to multidecadal variability of winter storminess in the eastern United States was studied using water level measurements from coastal tide gauges. The proximity to the coast of the primary winter storm track in the region allows the use of tide gauges to study temporal modulations in the frequency of these storms. Storms were identified in high-passed, detided sea level anomalies in 20 gauges from all coasts of North America to assess variability in winter storminess along particular storm tracks. The primary result is a significant multidecadal increase in the number of storms affecting the southeastern United States from the early to late twentieth century. The authors propose that this change is due to an increased tendency for the jet stream to meander south over the eastern United States since the 1950s. This mechanism is supported by long-term changes in the large-scale sea level pressure pattern over North America. The nature of the multidecadal change in storm frequency is unclear, because limited tide gauge record lengths prevent distinguishing between a trend and an oscillation. |
format |
Article in Journal/Newspaper |
author |
Thompson, Philip R. Mitchum, Gary T. Vonesch, Cedric Li, Jianke |
author_facet |
Thompson, Philip R. Mitchum, Gary T. Vonesch, Cedric Li, Jianke |
author_sort |
Thompson, Philip R. |
title |
Variability of Winter Storminess in the Eastern United States during the Twentieth Century from Tide Gauges |
title_short |
Variability of Winter Storminess in the Eastern United States during the Twentieth Century from Tide Gauges |
title_full |
Variability of Winter Storminess in the Eastern United States during the Twentieth Century from Tide Gauges |
title_fullStr |
Variability of Winter Storminess in the Eastern United States during the Twentieth Century from Tide Gauges |
title_full_unstemmed |
Variability of Winter Storminess in the Eastern United States during the Twentieth Century from Tide Gauges |
title_sort |
variability of winter storminess in the eastern united states during the twentieth century from tide gauges |
publisher |
Digital Commons @ University of South Florida |
publishDate |
2013 |
url |
https://digitalcommons.usf.edu/msc_facpub/2098 https://doi.org/10.1175/JCLI-D-12-00561.1 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
Marine Science Faculty Publications |
op_relation |
https://digitalcommons.usf.edu/msc_facpub/2098 doi:10.1175/JCLI-D-12-00561.1 https://doi.org/10.1175/JCLI-D-12-00561.1 |
op_doi |
https://doi.org/10.1175/JCLI-D-12-00561.1 |
container_title |
Journal of Climate |
container_volume |
26 |
container_issue |
23 |
container_start_page |
9713 |
op_container_end_page |
9726 |
_version_ |
1772812577597816832 |