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...

Full description

Bibliographic Details
Published in:Quarterly Journal of the Royal Meteorological Society
Main Author: Bliss, E. W.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1927
Subjects:
Online Access: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
id crwiley:10.1002/qj.49705322106
record_format openpolar
spelling 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
institution Open Polar
collection Wiley Online Library
op_collection_id 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
_version_ 1800757283956719616