The variability of the onset of spring in Britain

Abstract The first day of spring is defined in terms of daily maximum temperatures. Spring at Oxford as defined begins some time between the third week of February and the last week of April. The average date shows a secular change over the last hundred years. The date of the first day of spring is...

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Published in:Quarterly Journal of the Royal Meteorological Society
Main Author: Davis, N. E.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1972
Subjects:
Online Access:http://dx.doi.org/10.1002/qj.49709841805
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spelling crwiley:10.1002/qj.49709841805 2024-06-02T08:09:11+00:00 The variability of the onset of spring in Britain Davis, N. E. 1972 http://dx.doi.org/10.1002/qj.49709841805 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49709841805 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49709841805 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Quarterly Journal of the Royal Meteorological Society volume 98, issue 418, page 763-777 ISSN 0035-9009 1477-870X journal-article 1972 crwiley https://doi.org/10.1002/qj.49709841805 2024-05-03T11:07:31Z Abstract The first day of spring is defined in terms of daily maximum temperatures. Spring at Oxford as defined begins some time between the third week of February and the last week of April. The average date shows a secular change over the last hundred years. The date of the first day of spring is shown to be related to ice conditions in the Baltic and in the Iceland area, to the sea temperature pattern in the North Atlantic, the circulation patterns at 500 mb and to various atmospheric indices. Rules developed from these relationships enable ‘statistical’ forecasts for the first day of spring to be made. Article in Journal/Newspaper Iceland North Atlantic Wiley Online Library Quarterly Journal of the Royal Meteorological Society 98 418 763 777
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language English
description Abstract The first day of spring is defined in terms of daily maximum temperatures. Spring at Oxford as defined begins some time between the third week of February and the last week of April. The average date shows a secular change over the last hundred years. The date of the first day of spring is shown to be related to ice conditions in the Baltic and in the Iceland area, to the sea temperature pattern in the North Atlantic, the circulation patterns at 500 mb and to various atmospheric indices. Rules developed from these relationships enable ‘statistical’ forecasts for the first day of spring to be made.
format Article in Journal/Newspaper
author Davis, N. E.
spellingShingle Davis, N. E.
The variability of the onset of spring in Britain
author_facet Davis, N. E.
author_sort Davis, N. E.
title The variability of the onset of spring in Britain
title_short The variability of the onset of spring in Britain
title_full The variability of the onset of spring in Britain
title_fullStr The variability of the onset of spring in Britain
title_full_unstemmed The variability of the onset of spring in Britain
title_sort variability of the onset of spring in britain
publisher Wiley
publishDate 1972
url http://dx.doi.org/10.1002/qj.49709841805
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49709841805
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49709841805
genre Iceland
North Atlantic
genre_facet Iceland
North Atlantic
op_source Quarterly Journal of the Royal Meteorological Society
volume 98, issue 418, page 763-777
ISSN 0035-9009 1477-870X
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/qj.49709841805
container_title Quarterly Journal of the Royal Meteorological Society
container_volume 98
container_issue 418
container_start_page 763
op_container_end_page 777
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