Solar Activity and Svalbard Temperatures

The long temperature series at Svalbard (Longyearbyen) show large variations and a positive trend since its start in 1912. During this period solar activity has increased, as indicated by shorter solar cycles. The temperature at Svalbard is negatively correlated with the length of the solar cycle. T...

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Published in:Advances in Meteorology
Main Authors: Jan-Erik Solheim, Kjell Stordahl, Ole Humlum
Format: Article in Journal/Newspaper
Language:English
Published: Hindawi Limited 2011
Subjects:
Online Access:https://doi.org/10.1155/2011/543146
https://doaj.org/article/bc4a517369a14a2d81b3d564e467bba9
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spelling ftdoajarticles:oai:doaj.org/article:bc4a517369a14a2d81b3d564e467bba9 2023-05-15T17:08:30+02:00 Solar Activity and Svalbard Temperatures Jan-Erik Solheim Kjell Stordahl Ole Humlum 2011-01-01T00:00:00Z https://doi.org/10.1155/2011/543146 https://doaj.org/article/bc4a517369a14a2d81b3d564e467bba9 EN eng Hindawi Limited http://dx.doi.org/10.1155/2011/543146 https://doaj.org/toc/1687-9309 https://doaj.org/toc/1687-9317 1687-9309 1687-9317 doi:10.1155/2011/543146 https://doaj.org/article/bc4a517369a14a2d81b3d564e467bba9 Advances in Meteorology, Vol 2011 (2011) Meteorology. Climatology QC851-999 article 2011 ftdoajarticles https://doi.org/10.1155/2011/543146 2022-12-31T15:22:20Z The long temperature series at Svalbard (Longyearbyen) show large variations and a positive trend since its start in 1912. During this period solar activity has increased, as indicated by shorter solar cycles. The temperature at Svalbard is negatively correlated with the length of the solar cycle. The strongest negative correlation is found with lags 10–12 years. The relations between the length of a solar cycle and the mean temperature in the following cycle are used to model Svalbard annual mean temperature and seasonal temperature variations. Residuals from the annual and winter models show no autocorrelations on the 5 per cent level, which indicates that no additional parameters are needed to explain the temperature variations with 95 per cent significance. These models show that 60 per cent of the annual and winter temperature variations are explained by solar activity. For the spring, summer, and fall temperatures autocorrelations in the residuals exist, and additional variables may contribute to the variations. These models can be applied as forecasting models. We predict an annual mean temperature decrease for Svalbard of 3.5±2°C from solar cycle 23 to solar cycle 24 (2009–20) and a decrease in the winter temperature of ≈6°C. Article in Journal/Newspaper Longyearbyen Svalbard Directory of Open Access Journals: DOAJ Articles Svalbard Longyearbyen Advances in Meteorology 2011 1 8
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Meteorology. Climatology
QC851-999
spellingShingle Meteorology. Climatology
QC851-999
Jan-Erik Solheim
Kjell Stordahl
Ole Humlum
Solar Activity and Svalbard Temperatures
topic_facet Meteorology. Climatology
QC851-999
description The long temperature series at Svalbard (Longyearbyen) show large variations and a positive trend since its start in 1912. During this period solar activity has increased, as indicated by shorter solar cycles. The temperature at Svalbard is negatively correlated with the length of the solar cycle. The strongest negative correlation is found with lags 10–12 years. The relations between the length of a solar cycle and the mean temperature in the following cycle are used to model Svalbard annual mean temperature and seasonal temperature variations. Residuals from the annual and winter models show no autocorrelations on the 5 per cent level, which indicates that no additional parameters are needed to explain the temperature variations with 95 per cent significance. These models show that 60 per cent of the annual and winter temperature variations are explained by solar activity. For the spring, summer, and fall temperatures autocorrelations in the residuals exist, and additional variables may contribute to the variations. These models can be applied as forecasting models. We predict an annual mean temperature decrease for Svalbard of 3.5±2°C from solar cycle 23 to solar cycle 24 (2009–20) and a decrease in the winter temperature of ≈6°C.
format Article in Journal/Newspaper
author Jan-Erik Solheim
Kjell Stordahl
Ole Humlum
author_facet Jan-Erik Solheim
Kjell Stordahl
Ole Humlum
author_sort Jan-Erik Solheim
title Solar Activity and Svalbard Temperatures
title_short Solar Activity and Svalbard Temperatures
title_full Solar Activity and Svalbard Temperatures
title_fullStr Solar Activity and Svalbard Temperatures
title_full_unstemmed Solar Activity and Svalbard Temperatures
title_sort solar activity and svalbard temperatures
publisher Hindawi Limited
publishDate 2011
url https://doi.org/10.1155/2011/543146
https://doaj.org/article/bc4a517369a14a2d81b3d564e467bba9
geographic Svalbard
Longyearbyen
geographic_facet Svalbard
Longyearbyen
genre Longyearbyen
Svalbard
genre_facet Longyearbyen
Svalbard
op_source Advances in Meteorology, Vol 2011 (2011)
op_relation http://dx.doi.org/10.1155/2011/543146
https://doaj.org/toc/1687-9309
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doi:10.1155/2011/543146
https://doaj.org/article/bc4a517369a14a2d81b3d564e467bba9
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container_title Advances in Meteorology
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