The nile foold and world weather
Abstract Correlation coefficients are given with pressure, temperature, rain, ice and wind, and it is shown (a) that the Nile flood takes part in the southern oscillation as a member of the first group, (b) that equatorial temperatures are in inverse relation to the Nile flood, and (c) that the wint...
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crwiley:10.1002/qj.49705322106 2024-06-02T08:11:13+00:00 The nile foold and world weather Bliss, E. W. 1927 http://dx.doi.org/10.1002/qj.49705322106 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49705322106 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49705322106 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Quarterly Journal of the Royal Meteorological Society volume 53, issue 221, page 41-44 ISSN 0035-9009 1477-870X journal-article 1927 crwiley https://doi.org/10.1002/qj.49705322106 2024-05-03T10:39:30Z Abstract Correlation coefficients are given with pressure, temperature, rain, ice and wind, and it is shown (a) that the Nile flood takes part in the southern oscillation as a member of the first group, (b) that equatorial temperatures are in inverse relation to the Nile flood, and (c) that the winter North Atlantic circulation varies inversely with the preceding Nile flood. St. Helena pressure has no contemporary relationship with the Nile flood. A formula is derived for prediction on June 1 with a joint coefficient of 0.72. Article in Journal/Newspaper North Atlantic Wiley Online Library St. Helena ENVELOPE(8.575,8.575,63.621,63.621) Quarterly Journal of the Royal Meteorological Society 53 221 41 44 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Correlation coefficients are given with pressure, temperature, rain, ice and wind, and it is shown (a) that the Nile flood takes part in the southern oscillation as a member of the first group, (b) that equatorial temperatures are in inverse relation to the Nile flood, and (c) that the winter North Atlantic circulation varies inversely with the preceding Nile flood. St. Helena pressure has no contemporary relationship with the Nile flood. A formula is derived for prediction on June 1 with a joint coefficient of 0.72. |
format |
Article in Journal/Newspaper |
author |
Bliss, E. W. |
spellingShingle |
Bliss, E. W. The nile foold and world weather |
author_facet |
Bliss, E. W. |
author_sort |
Bliss, E. W. |
title |
The nile foold and world weather |
title_short |
The nile foold and world weather |
title_full |
The nile foold and world weather |
title_fullStr |
The nile foold and world weather |
title_full_unstemmed |
The nile foold and world weather |
title_sort |
nile foold and world weather |
publisher |
Wiley |
publishDate |
1927 |
url |
http://dx.doi.org/10.1002/qj.49705322106 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49705322106 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49705322106 |
long_lat |
ENVELOPE(8.575,8.575,63.621,63.621) |
geographic |
St. Helena |
geographic_facet |
St. Helena |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Quarterly Journal of the Royal Meteorological Society volume 53, issue 221, page 41-44 ISSN 0035-9009 1477-870X |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/qj.49705322106 |
container_title |
Quarterly Journal of the Royal Meteorological Society |
container_volume |
53 |
container_issue |
221 |
container_start_page |
41 |
op_container_end_page |
44 |
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1800757283956719616 |