Case Studies of High Wind Events in Barrow, Alaska: Climatological Context and Development Processes
The Beaufort–Chukchi cyclones of October 1963 and August 2000 produced the highest winds ever recorded in Barrow, Alaska. In both cases, winds of 25 m s21 were observed with gusts unofficially reported at 33 m s21. The October 1963 storm caused significant flooding, contaminated drinking water, and...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.504.6889 2023-05-15T14:18:02+02:00 Case Studies of High Wind Events in Barrow, Alaska: Climatological Context and Development Processes Amanda H. Lynch Elizabeth N. Cassano John J. Cassano Leanne R. Lestak The Pennsylvania State University CiteSeerX Archives 2002 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.504.6889 http://nome.colorado.edu/HARC/Publications/Lynchetal2003.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.504.6889 http://nome.colorado.edu/HARC/Publications/Lynchetal2003.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://nome.colorado.edu/HARC/Publications/Lynchetal2003.pdf text 2002 ftciteseerx 2016-01-08T09:18:53Z The Beaufort–Chukchi cyclones of October 1963 and August 2000 produced the highest winds ever recorded in Barrow, Alaska. In both cases, winds of 25 m s21 were observed with gusts unofficially reported at 33 m s21. The October 1963 storm caused significant flooding, contaminated drinking water, and interrupted power supplies. The August 2000 storm caused the wreck of a $6 million dredge, and removed roofs from 40 buildings. Both storms were unusual in that they tracked eastward from the East Siberian Sea into the Chukchi and Beaufort Seas, rather than following a more typical northward track into the Arctic Ocean. This paper addresses, through modeling and analysis, the development processes of these two storms. The October 1963 system was a long-lived, warm core, zonally elongated cyclone that traversed around the Arctic basin through the Canadian Archipelago. The August 2000 system was an open-wave cyclone that dissipated rapidly into a weak, cold core eddy in the Alaskan sector of the Beaufort Sea. Approximating the contributions to development using terms in a quasigeostrophic omega equation, it was found that both storms were char-acterized by the increasing importance of the convergence of the Q vector (representing differential vorticity advection and thermal advection) in the midtroposphere, at the expense of forcing by the turbulent fluxes of heat, moisture, and momentum in the boundary layer. However, the influence of surface turbulent fluxes in the Text Archipelago Arctic Basin Arctic Arctic Ocean Barrow Beaufort Sea Canadian Archipelago Chukchi East Siberian Sea Alaska Unknown Arctic Arctic Ocean East Siberian Sea ENVELOPE(166.000,166.000,74.000,74.000) |
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English |
description |
The Beaufort–Chukchi cyclones of October 1963 and August 2000 produced the highest winds ever recorded in Barrow, Alaska. In both cases, winds of 25 m s21 were observed with gusts unofficially reported at 33 m s21. The October 1963 storm caused significant flooding, contaminated drinking water, and interrupted power supplies. The August 2000 storm caused the wreck of a $6 million dredge, and removed roofs from 40 buildings. Both storms were unusual in that they tracked eastward from the East Siberian Sea into the Chukchi and Beaufort Seas, rather than following a more typical northward track into the Arctic Ocean. This paper addresses, through modeling and analysis, the development processes of these two storms. The October 1963 system was a long-lived, warm core, zonally elongated cyclone that traversed around the Arctic basin through the Canadian Archipelago. The August 2000 system was an open-wave cyclone that dissipated rapidly into a weak, cold core eddy in the Alaskan sector of the Beaufort Sea. Approximating the contributions to development using terms in a quasigeostrophic omega equation, it was found that both storms were char-acterized by the increasing importance of the convergence of the Q vector (representing differential vorticity advection and thermal advection) in the midtroposphere, at the expense of forcing by the turbulent fluxes of heat, moisture, and momentum in the boundary layer. However, the influence of surface turbulent fluxes in the |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Amanda H. Lynch Elizabeth N. Cassano John J. Cassano Leanne R. Lestak |
spellingShingle |
Amanda H. Lynch Elizabeth N. Cassano John J. Cassano Leanne R. Lestak Case Studies of High Wind Events in Barrow, Alaska: Climatological Context and Development Processes |
author_facet |
Amanda H. Lynch Elizabeth N. Cassano John J. Cassano Leanne R. Lestak |
author_sort |
Amanda H. Lynch |
title |
Case Studies of High Wind Events in Barrow, Alaska: Climatological Context and Development Processes |
title_short |
Case Studies of High Wind Events in Barrow, Alaska: Climatological Context and Development Processes |
title_full |
Case Studies of High Wind Events in Barrow, Alaska: Climatological Context and Development Processes |
title_fullStr |
Case Studies of High Wind Events in Barrow, Alaska: Climatological Context and Development Processes |
title_full_unstemmed |
Case Studies of High Wind Events in Barrow, Alaska: Climatological Context and Development Processes |
title_sort |
case studies of high wind events in barrow, alaska: climatological context and development processes |
publishDate |
2002 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.504.6889 http://nome.colorado.edu/HARC/Publications/Lynchetal2003.pdf |
long_lat |
ENVELOPE(166.000,166.000,74.000,74.000) |
geographic |
Arctic Arctic Ocean East Siberian Sea |
geographic_facet |
Arctic Arctic Ocean East Siberian Sea |
genre |
Archipelago Arctic Basin Arctic Arctic Ocean Barrow Beaufort Sea Canadian Archipelago Chukchi East Siberian Sea Alaska |
genre_facet |
Archipelago Arctic Basin Arctic Arctic Ocean Barrow Beaufort Sea Canadian Archipelago Chukchi East Siberian Sea Alaska |
op_source |
http://nome.colorado.edu/HARC/Publications/Lynchetal2003.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.504.6889 http://nome.colorado.edu/HARC/Publications/Lynchetal2003.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766289795082878976 |