Solar Forcing of Regional Climate Change During the Maunder Minimum
We examine the climate response to solar irradiance changes between the late 17th-century Maunder Minimum and the late 18th century. Global average temperature changes are small (about 0.3° to 0.4°C) in both a climate model and empirical reconstructions. However, regional temperature changes are qui...
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American Association for the Advancement of Science (AAAS)
2001
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Online Access: | http://dx.doi.org/10.1126/science.1064363 https://www.science.org/doi/pdf/10.1126/science.1064363 |
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craaas:10.1126/science.1064363 2024-09-09T19:23:38+00:00 Solar Forcing of Regional Climate Change During the Maunder Minimum Shindell, Drew T. Schmidt, Gavin A. Mann, Michael E. Rind, David Waple, Anne 2001 http://dx.doi.org/10.1126/science.1064363 https://www.science.org/doi/pdf/10.1126/science.1064363 en eng American Association for the Advancement of Science (AAAS) Science volume 294, issue 5549, page 2149-2152 ISSN 0036-8075 1095-9203 journal-article 2001 craaas https://doi.org/10.1126/science.1064363 2024-08-29T04:00:54Z We examine the climate response to solar irradiance changes between the late 17th-century Maunder Minimum and the late 18th century. Global average temperature changes are small (about 0.3° to 0.4°C) in both a climate model and empirical reconstructions. However, regional temperature changes are quite large. In the model, these occur primarily through a forced shift toward the low index state of the Arctic Oscillation/North Atlantic Oscillation as solar irradiance decreases. This leads to colder temperatures over the Northern Hemisphere continents, especially in winter (1° to 2°C), in agreement with historical records and proxy data for surface temperatures. Article in Journal/Newspaper Arctic Climate change North Atlantic North Atlantic oscillation AAAS Resource Center (American Association for the Advancement of Science) Arctic Science 294 5549 2149 2152 |
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Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
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craaas |
language |
English |
description |
We examine the climate response to solar irradiance changes between the late 17th-century Maunder Minimum and the late 18th century. Global average temperature changes are small (about 0.3° to 0.4°C) in both a climate model and empirical reconstructions. However, regional temperature changes are quite large. In the model, these occur primarily through a forced shift toward the low index state of the Arctic Oscillation/North Atlantic Oscillation as solar irradiance decreases. This leads to colder temperatures over the Northern Hemisphere continents, especially in winter (1° to 2°C), in agreement with historical records and proxy data for surface temperatures. |
format |
Article in Journal/Newspaper |
author |
Shindell, Drew T. Schmidt, Gavin A. Mann, Michael E. Rind, David Waple, Anne |
spellingShingle |
Shindell, Drew T. Schmidt, Gavin A. Mann, Michael E. Rind, David Waple, Anne Solar Forcing of Regional Climate Change During the Maunder Minimum |
author_facet |
Shindell, Drew T. Schmidt, Gavin A. Mann, Michael E. Rind, David Waple, Anne |
author_sort |
Shindell, Drew T. |
title |
Solar Forcing of Regional Climate Change During the Maunder Minimum |
title_short |
Solar Forcing of Regional Climate Change During the Maunder Minimum |
title_full |
Solar Forcing of Regional Climate Change During the Maunder Minimum |
title_fullStr |
Solar Forcing of Regional Climate Change During the Maunder Minimum |
title_full_unstemmed |
Solar Forcing of Regional Climate Change During the Maunder Minimum |
title_sort |
solar forcing of regional climate change during the maunder minimum |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
2001 |
url |
http://dx.doi.org/10.1126/science.1064363 https://www.science.org/doi/pdf/10.1126/science.1064363 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change North Atlantic North Atlantic oscillation |
genre_facet |
Arctic Climate change North Atlantic North Atlantic oscillation |
op_source |
Science volume 294, issue 5549, page 2149-2152 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.1064363 |
container_title |
Science |
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294 |
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5549 |
container_start_page |
2149 |
op_container_end_page |
2152 |
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1809893633182138368 |