A Dynamic Analysis of a Record Breaking Winter Season Blocking Event

The objective of this work is to study in detail a strong North Pacific, large amplitude, and long-lived blocking event that occurred during January 23–February 16, 2014. Indeed, it was the 11th strongest Northern Hemisphere event lasting longer than 20 days since 1968. This event formed out of the...

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Main Author: Andrew D. Jensen
Format: Article
Language:English
Published: Wiley 2015-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2015/634896
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author Andrew D. Jensen
author_facet Andrew D. Jensen
author_sort Andrew D. Jensen
collection DOAJ
description The objective of this work is to study in detail a strong North Pacific, large amplitude, and long-lived blocking event that occurred during January 23–February 16, 2014. Indeed, it was the 11th strongest Northern Hemisphere event lasting longer than 20 days since 1968. This event formed out of the strong ridge that was associated with the devastating drought in the Western United States during the winter season of 2013-2014. This blocking event had many outstanding dynamical characteristics, the chief of which was that it survived an abrupt change in the planetary-scale flow when the Pacific North American pattern index changed from positive to negative in early February. The block then reintensified and persisted into mid-February. Several diagnostic techniques are employed to investigate the change in the planetary-scale flow during early February 2014 that have been applied to blocking before but aren’t as well known in the blocking literature.
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spelling doaj-art-461cc12caa2b4e9b9f3caa1c005e60bf2025-02-03T01:20:33ZengWileyAdvances in Meteorology1687-93091687-93172015-01-01201510.1155/2015/634896634896A Dynamic Analysis of a Record Breaking Winter Season Blocking EventAndrew D. Jensen0Department of Soil, Environmental, and Atmospheric Sciences, University of Missouri-Columbia, 302 Anheuser Busch Natural Resources Building, Columbia, MO 65211, USAThe objective of this work is to study in detail a strong North Pacific, large amplitude, and long-lived blocking event that occurred during January 23–February 16, 2014. Indeed, it was the 11th strongest Northern Hemisphere event lasting longer than 20 days since 1968. This event formed out of the strong ridge that was associated with the devastating drought in the Western United States during the winter season of 2013-2014. This blocking event had many outstanding dynamical characteristics, the chief of which was that it survived an abrupt change in the planetary-scale flow when the Pacific North American pattern index changed from positive to negative in early February. The block then reintensified and persisted into mid-February. Several diagnostic techniques are employed to investigate the change in the planetary-scale flow during early February 2014 that have been applied to blocking before but aren’t as well known in the blocking literature.http://dx.doi.org/10.1155/2015/634896
spellingShingle Andrew D. Jensen
A Dynamic Analysis of a Record Breaking Winter Season Blocking Event
Advances in Meteorology
title A Dynamic Analysis of a Record Breaking Winter Season Blocking Event
title_full A Dynamic Analysis of a Record Breaking Winter Season Blocking Event
title_fullStr A Dynamic Analysis of a Record Breaking Winter Season Blocking Event
title_full_unstemmed A Dynamic Analysis of a Record Breaking Winter Season Blocking Event
title_short A Dynamic Analysis of a Record Breaking Winter Season Blocking Event
title_sort dynamic analysis of a record breaking winter season blocking event
url http://dx.doi.org/10.1155/2015/634896
work_keys_str_mv AT andrewdjensen adynamicanalysisofarecordbreakingwinterseasonblockingevent
AT andrewdjensen dynamicanalysisofarecordbreakingwinterseasonblockingevent