The answer is blowing in the wind

The North Atlantic Oscillation (NAO) is a natural climate variability and can be attributed to the UK warming in average winter temperature. Being responsible for both the strength and orientation of the Atlantic jetstream, the NAO is associated with the storm track beneath the jetstream. Changes in...

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Main Author: Woollings, T
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://ora.ox.ac.uk/objects/uuid:316dec10-06cf-4c52-8d75-85296ba3f0fc
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spelling ftuloxford:oai:ora.ox.ac.uk:uuid:316dec10-06cf-4c52-8d75-85296ba3f0fc 2024-10-06T13:51:02+00:00 The answer is blowing in the wind Woollings, T 2016-07-28 https://ora.ox.ac.uk/objects/uuid:316dec10-06cf-4c52-8d75-85296ba3f0fc eng eng https://ora.ox.ac.uk/objects/uuid:316dec10-06cf-4c52-8d75-85296ba3f0fc info:eu-repo/semantics/embargoedAccess Journal article 2016 ftuloxford 2024-09-06T07:47:30Z The North Atlantic Oscillation (NAO) is a natural climate variability and can be attributed to the UK warming in average winter temperature. Being responsible for both the strength and orientation of the Atlantic jetstream, the NAO is associated with the storm track beneath the jetstream. Changes in NAO is associated with large-scale waves that break in the upper atmosphere. The air waves which stretch for a few thousand kilometers, have some peaks and troughs and when distorted, becomes distorted and collapses into a very turbulent flow. Article in Journal/Newspaper North Atlantic North Atlantic oscillation ORA - Oxford University Research Archive
institution Open Polar
collection ORA - Oxford University Research Archive
op_collection_id ftuloxford
language English
description The North Atlantic Oscillation (NAO) is a natural climate variability and can be attributed to the UK warming in average winter temperature. Being responsible for both the strength and orientation of the Atlantic jetstream, the NAO is associated with the storm track beneath the jetstream. Changes in NAO is associated with large-scale waves that break in the upper atmosphere. The air waves which stretch for a few thousand kilometers, have some peaks and troughs and when distorted, becomes distorted and collapses into a very turbulent flow.
format Article in Journal/Newspaper
author Woollings, T
spellingShingle Woollings, T
The answer is blowing in the wind
author_facet Woollings, T
author_sort Woollings, T
title The answer is blowing in the wind
title_short The answer is blowing in the wind
title_full The answer is blowing in the wind
title_fullStr The answer is blowing in the wind
title_full_unstemmed The answer is blowing in the wind
title_sort answer is blowing in the wind
publishDate 2016
url https://ora.ox.ac.uk/objects/uuid:316dec10-06cf-4c52-8d75-85296ba3f0fc
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://ora.ox.ac.uk/objects/uuid:316dec10-06cf-4c52-8d75-85296ba3f0fc
op_rights info:eu-repo/semantics/embargoedAccess
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