Subsynoptic‐scale features associated with extreme surface gusts in UK extratropical cyclone events
Numerous studies have addressed the mesoscale features within extratropical cyclones (ETCs) that are responsible for the most destructive winds, though few have utilized surface observation data, and most are based on case studies. By using a 39‐station UK surface observation network, coupled with i...
Ausführliche Beschreibung
Autor*in: |
Earl, N [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2017 |
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Rechteinformationen: |
Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Geophysical research letters - Washington, DC : Union, 1974, 44(2017), 8, Seite 3932-3940 |
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Übergeordnetes Werk: |
volume:44 ; year:2017 ; number:8 ; pages:3932-3940 |
Links: |
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DOI / URN: |
10.1002/2017GL073124 |
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520 | |a Numerous studies have addressed the mesoscale features within extratropical cyclones (ETCs) that are responsible for the most destructive winds, though few have utilized surface observation data, and most are based on case studies. By using a 39‐station UK surface observation network, coupled with in‐depth analysis of the causes of extreme gusts during the period 2008–2014, we show that larger‐scale features (warm and cold conveyer belts) are most commonly associated with the top 1% of UK gusts but smaller‐scale features generate the most extreme winds. The cold conveyor belt is far more destructive when joining the momentum of the ETC, rather than earlier in its trajectory, ahead of the approaching warm front. Sting jets and convective lines account for two thirds of severe surface gusts in the UK. A novel way to quantify the relative contributions of mesoscale extratropical cyclone features is introduced Larger‐scale features are most commonly associated with the top 1% of UK surface gusts but smaller‐scale features generate the most extreme 0.1% of winds Sting jets and convective lines account for two thirds of severe surface gusts in the UK | ||
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650 | 4 | |a extreme surface winds | |
650 | 4 | |a extratropical cyclones | |
650 | 4 | |a convective lines | |
650 | 4 | |a mesoscale features | |
650 | 4 | |a surface observations | |
650 | 4 | |a sting jets | |
650 | 4 | |a Gusts | |
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700 | 1 | |a Finch, R |4 oth | |
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10.1002/2017GL073124 doi PQ20170901 (DE-627)OLC1994201495 (DE-599)GBVOLC1994201495 (PRQ)p1367-5545437c210af69384ae37ce53dec383aeff962620cf5d5db758770ee148d0510 (KEY)0026932820170000044000803932subsynopticscalefeaturesassociatedwithextremesurfa DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Earl, N verfasserin aut Subsynoptic‐scale features associated with extreme surface gusts in UK extratropical cyclone events 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Numerous studies have addressed the mesoscale features within extratropical cyclones (ETCs) that are responsible for the most destructive winds, though few have utilized surface observation data, and most are based on case studies. By using a 39‐station UK surface observation network, coupled with in‐depth analysis of the causes of extreme gusts during the period 2008–2014, we show that larger‐scale features (warm and cold conveyer belts) are most commonly associated with the top 1% of UK gusts but smaller‐scale features generate the most extreme winds. The cold conveyor belt is far more destructive when joining the momentum of the ETC, rather than earlier in its trajectory, ahead of the approaching warm front. Sting jets and convective lines account for two thirds of severe surface gusts in the UK. A novel way to quantify the relative contributions of mesoscale extratropical cyclone features is introduced Larger‐scale features are most commonly associated with the top 1% of UK surface gusts but smaller‐scale features generate the most extreme 0.1% of winds Sting jets and convective lines account for two thirds of severe surface gusts in the UK Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. extreme surface winds extratropical cyclones convective lines mesoscale features surface observations sting jets Gusts Cyclones Tropical meteorology Meteorology Winds Surface temperature Dorling, S oth Starks, M oth Finch, R oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 44(2017), 8, Seite 3932-3940 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:44 year:2017 number:8 pages:3932-3940 http://dx.doi.org/10.1002/2017GL073124 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2017GL073124/abstract https://search.proquest.com/docview/1901450301 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 44 2017 8 3932-3940 |
spelling |
10.1002/2017GL073124 doi PQ20170901 (DE-627)OLC1994201495 (DE-599)GBVOLC1994201495 (PRQ)p1367-5545437c210af69384ae37ce53dec383aeff962620cf5d5db758770ee148d0510 (KEY)0026932820170000044000803932subsynopticscalefeaturesassociatedwithextremesurfa DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Earl, N verfasserin aut Subsynoptic‐scale features associated with extreme surface gusts in UK extratropical cyclone events 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Numerous studies have addressed the mesoscale features within extratropical cyclones (ETCs) that are responsible for the most destructive winds, though few have utilized surface observation data, and most are based on case studies. By using a 39‐station UK surface observation network, coupled with in‐depth analysis of the causes of extreme gusts during the period 2008–2014, we show that larger‐scale features (warm and cold conveyer belts) are most commonly associated with the top 1% of UK gusts but smaller‐scale features generate the most extreme winds. The cold conveyor belt is far more destructive when joining the momentum of the ETC, rather than earlier in its trajectory, ahead of the approaching warm front. Sting jets and convective lines account for two thirds of severe surface gusts in the UK. A novel way to quantify the relative contributions of mesoscale extratropical cyclone features is introduced Larger‐scale features are most commonly associated with the top 1% of UK surface gusts but smaller‐scale features generate the most extreme 0.1% of winds Sting jets and convective lines account for two thirds of severe surface gusts in the UK Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. extreme surface winds extratropical cyclones convective lines mesoscale features surface observations sting jets Gusts Cyclones Tropical meteorology Meteorology Winds Surface temperature Dorling, S oth Starks, M oth Finch, R oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 44(2017), 8, Seite 3932-3940 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:44 year:2017 number:8 pages:3932-3940 http://dx.doi.org/10.1002/2017GL073124 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2017GL073124/abstract https://search.proquest.com/docview/1901450301 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 44 2017 8 3932-3940 |
allfields_unstemmed |
10.1002/2017GL073124 doi PQ20170901 (DE-627)OLC1994201495 (DE-599)GBVOLC1994201495 (PRQ)p1367-5545437c210af69384ae37ce53dec383aeff962620cf5d5db758770ee148d0510 (KEY)0026932820170000044000803932subsynopticscalefeaturesassociatedwithextremesurfa DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Earl, N verfasserin aut Subsynoptic‐scale features associated with extreme surface gusts in UK extratropical cyclone events 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Numerous studies have addressed the mesoscale features within extratropical cyclones (ETCs) that are responsible for the most destructive winds, though few have utilized surface observation data, and most are based on case studies. By using a 39‐station UK surface observation network, coupled with in‐depth analysis of the causes of extreme gusts during the period 2008–2014, we show that larger‐scale features (warm and cold conveyer belts) are most commonly associated with the top 1% of UK gusts but smaller‐scale features generate the most extreme winds. The cold conveyor belt is far more destructive when joining the momentum of the ETC, rather than earlier in its trajectory, ahead of the approaching warm front. Sting jets and convective lines account for two thirds of severe surface gusts in the UK. A novel way to quantify the relative contributions of mesoscale extratropical cyclone features is introduced Larger‐scale features are most commonly associated with the top 1% of UK surface gusts but smaller‐scale features generate the most extreme 0.1% of winds Sting jets and convective lines account for two thirds of severe surface gusts in the UK Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. extreme surface winds extratropical cyclones convective lines mesoscale features surface observations sting jets Gusts Cyclones Tropical meteorology Meteorology Winds Surface temperature Dorling, S oth Starks, M oth Finch, R oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 44(2017), 8, Seite 3932-3940 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:44 year:2017 number:8 pages:3932-3940 http://dx.doi.org/10.1002/2017GL073124 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2017GL073124/abstract https://search.proquest.com/docview/1901450301 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 44 2017 8 3932-3940 |
allfieldsGer |
10.1002/2017GL073124 doi PQ20170901 (DE-627)OLC1994201495 (DE-599)GBVOLC1994201495 (PRQ)p1367-5545437c210af69384ae37ce53dec383aeff962620cf5d5db758770ee148d0510 (KEY)0026932820170000044000803932subsynopticscalefeaturesassociatedwithextremesurfa DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Earl, N verfasserin aut Subsynoptic‐scale features associated with extreme surface gusts in UK extratropical cyclone events 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Numerous studies have addressed the mesoscale features within extratropical cyclones (ETCs) that are responsible for the most destructive winds, though few have utilized surface observation data, and most are based on case studies. By using a 39‐station UK surface observation network, coupled with in‐depth analysis of the causes of extreme gusts during the period 2008–2014, we show that larger‐scale features (warm and cold conveyer belts) are most commonly associated with the top 1% of UK gusts but smaller‐scale features generate the most extreme winds. The cold conveyor belt is far more destructive when joining the momentum of the ETC, rather than earlier in its trajectory, ahead of the approaching warm front. Sting jets and convective lines account for two thirds of severe surface gusts in the UK. A novel way to quantify the relative contributions of mesoscale extratropical cyclone features is introduced Larger‐scale features are most commonly associated with the top 1% of UK surface gusts but smaller‐scale features generate the most extreme 0.1% of winds Sting jets and convective lines account for two thirds of severe surface gusts in the UK Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. extreme surface winds extratropical cyclones convective lines mesoscale features surface observations sting jets Gusts Cyclones Tropical meteorology Meteorology Winds Surface temperature Dorling, S oth Starks, M oth Finch, R oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 44(2017), 8, Seite 3932-3940 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:44 year:2017 number:8 pages:3932-3940 http://dx.doi.org/10.1002/2017GL073124 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2017GL073124/abstract https://search.proquest.com/docview/1901450301 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 44 2017 8 3932-3940 |
allfieldsSound |
10.1002/2017GL073124 doi PQ20170901 (DE-627)OLC1994201495 (DE-599)GBVOLC1994201495 (PRQ)p1367-5545437c210af69384ae37ce53dec383aeff962620cf5d5db758770ee148d0510 (KEY)0026932820170000044000803932subsynopticscalefeaturesassociatedwithextremesurfa DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Earl, N verfasserin aut Subsynoptic‐scale features associated with extreme surface gusts in UK extratropical cyclone events 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Numerous studies have addressed the mesoscale features within extratropical cyclones (ETCs) that are responsible for the most destructive winds, though few have utilized surface observation data, and most are based on case studies. By using a 39‐station UK surface observation network, coupled with in‐depth analysis of the causes of extreme gusts during the period 2008–2014, we show that larger‐scale features (warm and cold conveyer belts) are most commonly associated with the top 1% of UK gusts but smaller‐scale features generate the most extreme winds. The cold conveyor belt is far more destructive when joining the momentum of the ETC, rather than earlier in its trajectory, ahead of the approaching warm front. Sting jets and convective lines account for two thirds of severe surface gusts in the UK. A novel way to quantify the relative contributions of mesoscale extratropical cyclone features is introduced Larger‐scale features are most commonly associated with the top 1% of UK surface gusts but smaller‐scale features generate the most extreme 0.1% of winds Sting jets and convective lines account for two thirds of severe surface gusts in the UK Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. extreme surface winds extratropical cyclones convective lines mesoscale features surface observations sting jets Gusts Cyclones Tropical meteorology Meteorology Winds Surface temperature Dorling, S oth Starks, M oth Finch, R oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 44(2017), 8, Seite 3932-3940 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:44 year:2017 number:8 pages:3932-3940 http://dx.doi.org/10.1002/2017GL073124 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2017GL073124/abstract https://search.proquest.com/docview/1901450301 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 44 2017 8 3932-3940 |
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Earl, N ddc 550 bkl 38.70 misc extreme surface winds misc extratropical cyclones misc convective lines misc mesoscale features misc surface observations misc sting jets misc Gusts misc Cyclones misc Tropical meteorology misc Meteorology misc Winds misc Surface temperature Subsynoptic‐scale features associated with extreme surface gusts in UK extratropical cyclone events |
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550 DNB 38.70 bkl Subsynoptic‐scale features associated with extreme surface gusts in UK extratropical cyclone events extreme surface winds extratropical cyclones convective lines mesoscale features surface observations sting jets Gusts Cyclones Tropical meteorology Meteorology Winds Surface temperature |
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Subsynoptic‐scale features associated with extreme surface gusts in UK extratropical cyclone events |
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subsynoptic‐scale features associated with extreme surface gusts in uk extratropical cyclone events |
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Subsynoptic‐scale features associated with extreme surface gusts in UK extratropical cyclone events |
abstract |
Numerous studies have addressed the mesoscale features within extratropical cyclones (ETCs) that are responsible for the most destructive winds, though few have utilized surface observation data, and most are based on case studies. By using a 39‐station UK surface observation network, coupled with in‐depth analysis of the causes of extreme gusts during the period 2008–2014, we show that larger‐scale features (warm and cold conveyer belts) are most commonly associated with the top 1% of UK gusts but smaller‐scale features generate the most extreme winds. The cold conveyor belt is far more destructive when joining the momentum of the ETC, rather than earlier in its trajectory, ahead of the approaching warm front. Sting jets and convective lines account for two thirds of severe surface gusts in the UK. A novel way to quantify the relative contributions of mesoscale extratropical cyclone features is introduced Larger‐scale features are most commonly associated with the top 1% of UK surface gusts but smaller‐scale features generate the most extreme 0.1% of winds Sting jets and convective lines account for two thirds of severe surface gusts in the UK |
abstractGer |
Numerous studies have addressed the mesoscale features within extratropical cyclones (ETCs) that are responsible for the most destructive winds, though few have utilized surface observation data, and most are based on case studies. By using a 39‐station UK surface observation network, coupled with in‐depth analysis of the causes of extreme gusts during the period 2008–2014, we show that larger‐scale features (warm and cold conveyer belts) are most commonly associated with the top 1% of UK gusts but smaller‐scale features generate the most extreme winds. The cold conveyor belt is far more destructive when joining the momentum of the ETC, rather than earlier in its trajectory, ahead of the approaching warm front. Sting jets and convective lines account for two thirds of severe surface gusts in the UK. A novel way to quantify the relative contributions of mesoscale extratropical cyclone features is introduced Larger‐scale features are most commonly associated with the top 1% of UK surface gusts but smaller‐scale features generate the most extreme 0.1% of winds Sting jets and convective lines account for two thirds of severe surface gusts in the UK |
abstract_unstemmed |
Numerous studies have addressed the mesoscale features within extratropical cyclones (ETCs) that are responsible for the most destructive winds, though few have utilized surface observation data, and most are based on case studies. By using a 39‐station UK surface observation network, coupled with in‐depth analysis of the causes of extreme gusts during the period 2008–2014, we show that larger‐scale features (warm and cold conveyer belts) are most commonly associated with the top 1% of UK gusts but smaller‐scale features generate the most extreme winds. The cold conveyor belt is far more destructive when joining the momentum of the ETC, rather than earlier in its trajectory, ahead of the approaching warm front. Sting jets and convective lines account for two thirds of severe surface gusts in the UK. A novel way to quantify the relative contributions of mesoscale extratropical cyclone features is introduced Larger‐scale features are most commonly associated with the top 1% of UK surface gusts but smaller‐scale features generate the most extreme 0.1% of winds Sting jets and convective lines account for two thirds of severe surface gusts in the UK |
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container_issue |
8 |
title_short |
Subsynoptic‐scale features associated with extreme surface gusts in UK extratropical cyclone events |
url |
http://dx.doi.org/10.1002/2017GL073124 http://onlinelibrary.wiley.com/doi/10.1002/2017GL073124/abstract https://search.proquest.com/docview/1901450301 |
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