THE SEVERE WINTER OF 1976-77: PRECURSORS AND PRECEDENTS

The severe winter of 1976-77 over the eastern United States was related to an exceptionally strong and unusual pattern of tropospheric winds and pressure anomalies that persisted from the previous October. The record bitter cold that occurred during January was additionally due to the southward disp...

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Main Authors: A. James Wagner, Long Range, Prediction Group
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.662.6209
http://nwas.org/digest/papers/1977/Vol02No4/1977v002no04-Wagner.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.662.6209 2023-05-15T15:00:22+02:00 THE SEVERE WINTER OF 1976-77: PRECURSORS AND PRECEDENTS A. James Wagner Long Range Prediction Group The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.662.6209 http://nwas.org/digest/papers/1977/Vol02No4/1977v002no04-Wagner.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.662.6209 http://nwas.org/digest/papers/1977/Vol02No4/1977v002no04-Wagner.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://nwas.org/digest/papers/1977/Vol02No4/1977v002no04-Wagner.pdf text ftciteseerx 2016-01-08T16:56:50Z The severe winter of 1976-77 over the eastern United States was related to an exceptionally strong and unusual pattern of tropospheric winds and pressure anomalies that persisted from the previous October. The record bitter cold that occurred during January was additionally due to the southward displacement of the cold polar Low, normally found over Northern Canada, by what appears to have been the strongest blo~king High ever observed over the Arctic region. A search of the records turned up. seve~al seve~ely co.ld w.ID:crs during the 20th Century. with that of 1917-18 being clo~est to the recent Winter 1D seventy, wlth slmllar antecedent and concurrent phenomena. 1. Text Arctic Unknown Arctic Canada
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description The severe winter of 1976-77 over the eastern United States was related to an exceptionally strong and unusual pattern of tropospheric winds and pressure anomalies that persisted from the previous October. The record bitter cold that occurred during January was additionally due to the southward displacement of the cold polar Low, normally found over Northern Canada, by what appears to have been the strongest blo~king High ever observed over the Arctic region. A search of the records turned up. seve~al seve~ely co.ld w.ID:crs during the 20th Century. with that of 1917-18 being clo~est to the recent Winter 1D seventy, wlth slmllar antecedent and concurrent phenomena. 1.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author A. James Wagner
Long Range
Prediction Group
spellingShingle A. James Wagner
Long Range
Prediction Group
THE SEVERE WINTER OF 1976-77: PRECURSORS AND PRECEDENTS
author_facet A. James Wagner
Long Range
Prediction Group
author_sort A. James Wagner
title THE SEVERE WINTER OF 1976-77: PRECURSORS AND PRECEDENTS
title_short THE SEVERE WINTER OF 1976-77: PRECURSORS AND PRECEDENTS
title_full THE SEVERE WINTER OF 1976-77: PRECURSORS AND PRECEDENTS
title_fullStr THE SEVERE WINTER OF 1976-77: PRECURSORS AND PRECEDENTS
title_full_unstemmed THE SEVERE WINTER OF 1976-77: PRECURSORS AND PRECEDENTS
title_sort severe winter of 1976-77: precursors and precedents
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.662.6209
http://nwas.org/digest/papers/1977/Vol02No4/1977v002no04-Wagner.pdf
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
genre_facet Arctic
op_source http://nwas.org/digest/papers/1977/Vol02No4/1977v002no04-Wagner.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.662.6209
http://nwas.org/digest/papers/1977/Vol02No4/1977v002no04-Wagner.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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