Solar cycle signals in sea level pressure and sea surface temperature

We identify solar cycle signals in 155 years of global sea level pressure (SLP) and sea surface temperature (SST) data using a multiple linear regression approach. In SLP we find in the North Pacific a statistically significant weakening of the Aleutian Low and a northward shift of the Hawaiian High...

Full description

Bibliographic Details
Main Authors: I. Roy, J. D. Haigh
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2010
Subjects:
Online Access:https://doaj.org/article/a86e9afa8a3f4cc3898ba5e7b79676c0
id ftdoajarticles:oai:doaj.org/article:a86e9afa8a3f4cc3898ba5e7b79676c0
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:a86e9afa8a3f4cc3898ba5e7b79676c0 2023-05-15T13:15:00+02:00 Solar cycle signals in sea level pressure and sea surface temperature I. Roy J. D. Haigh 2010-03-01T00:00:00Z https://doaj.org/article/a86e9afa8a3f4cc3898ba5e7b79676c0 EN eng Copernicus Publications http://www.atmos-chem-phys.net/10/3147/2010/acp-10-3147-2010.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 1680-7316 1680-7324 https://doaj.org/article/a86e9afa8a3f4cc3898ba5e7b79676c0 Atmospheric Chemistry and Physics, Vol 10, Iss 6, Pp 3147-3153 (2010) Physics QC1-999 Chemistry QD1-999 article 2010 ftdoajarticles 2022-12-31T13:12:19Z We identify solar cycle signals in 155 years of global sea level pressure (SLP) and sea surface temperature (SST) data using a multiple linear regression approach. In SLP we find in the North Pacific a statistically significant weakening of the Aleutian Low and a northward shift of the Hawaiian High in response to higher solar activity, confirming the results of previous authors using different techniques. We also find a weak but broad reduction in pressure across the equatorial Pacific. In SST we identify a weak El Niño-like pattern in the tropics for the 155 year period, unlike the strong La Niña-like signal found recently by some other authors. We show that the latter have been influenced by the technique of compositing data from peak years of the sunspot cycle because these years have often coincided with the negative phase of the ENSO cycle. Furthermore, the date of peak annual sunspot number (SSN) generally falls a year or more in advance of the broader maximum of the 11-year solar cycle so that analyses which incorporate data from all years represent more coherently the difference between periods of high and low solar activity on these timescales. We also find that studies of the solar signal in SST over the second half of the 20th century may alias as ENSO signal if this is not properly taken into account. Article in Journal/Newspaper aleutian low Directory of Open Access Journals: DOAJ Articles Pacific
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Physics
QC1-999
Chemistry
QD1-999
spellingShingle Physics
QC1-999
Chemistry
QD1-999
I. Roy
J. D. Haigh
Solar cycle signals in sea level pressure and sea surface temperature
topic_facet Physics
QC1-999
Chemistry
QD1-999
description We identify solar cycle signals in 155 years of global sea level pressure (SLP) and sea surface temperature (SST) data using a multiple linear regression approach. In SLP we find in the North Pacific a statistically significant weakening of the Aleutian Low and a northward shift of the Hawaiian High in response to higher solar activity, confirming the results of previous authors using different techniques. We also find a weak but broad reduction in pressure across the equatorial Pacific. In SST we identify a weak El Niño-like pattern in the tropics for the 155 year period, unlike the strong La Niña-like signal found recently by some other authors. We show that the latter have been influenced by the technique of compositing data from peak years of the sunspot cycle because these years have often coincided with the negative phase of the ENSO cycle. Furthermore, the date of peak annual sunspot number (SSN) generally falls a year or more in advance of the broader maximum of the 11-year solar cycle so that analyses which incorporate data from all years represent more coherently the difference between periods of high and low solar activity on these timescales. We also find that studies of the solar signal in SST over the second half of the 20th century may alias as ENSO signal if this is not properly taken into account.
format Article in Journal/Newspaper
author I. Roy
J. D. Haigh
author_facet I. Roy
J. D. Haigh
author_sort I. Roy
title Solar cycle signals in sea level pressure and sea surface temperature
title_short Solar cycle signals in sea level pressure and sea surface temperature
title_full Solar cycle signals in sea level pressure and sea surface temperature
title_fullStr Solar cycle signals in sea level pressure and sea surface temperature
title_full_unstemmed Solar cycle signals in sea level pressure and sea surface temperature
title_sort solar cycle signals in sea level pressure and sea surface temperature
publisher Copernicus Publications
publishDate 2010
url https://doaj.org/article/a86e9afa8a3f4cc3898ba5e7b79676c0
geographic Pacific
geographic_facet Pacific
genre aleutian low
genre_facet aleutian low
op_source Atmospheric Chemistry and Physics, Vol 10, Iss 6, Pp 3147-3153 (2010)
op_relation http://www.atmos-chem-phys.net/10/3147/2010/acp-10-3147-2010.pdf
https://doaj.org/toc/1680-7316
https://doaj.org/toc/1680-7324
1680-7316
1680-7324
https://doaj.org/article/a86e9afa8a3f4cc3898ba5e7b79676c0
_version_ 1766266467889709056