The Maunder minimum and the Little Ice Age: an update from recent reconstructions and climate simulations
The Maunder minimum (MM) was a period of extremely low solar activity from approximately AD 1650 to 1715. In the solar physics literature, the MM is sometimes associated with a period of cooler global temperatures, referred to as the Little Ice Age (LIA), and thus taken as compelling evidence of a l...
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doaj-da80d6713ff1401b8d838aa71bad50722021-02-02T00:24:43ZengEDP SciencesJournal of Space Weather and Space Climate2115-72512017-01-017A3310.1051/swsc/2017034swsc170014The Maunder minimum and the Little Ice Age: an update from recent reconstructions and climate simulationsOwens Mathew J.Lockwood MikeHawkins EdUsoskin IlyaJones Gareth S.Barnard LukeSchurer AndrewFasullo JohnThe Maunder minimum (MM) was a period of extremely low solar activity from approximately AD 1650 to 1715. In the solar physics literature, the MM is sometimes associated with a period of cooler global temperatures, referred to as the Little Ice Age (LIA), and thus taken as compelling evidence of a large, direct solar influence on climate. In this study, we bring together existing simulation and observational studies, particularly the most recent solar activity and paleoclimate reconstructions, to examine this relation. Using northern hemisphere surface air temperature reconstructions, the LIA can be most readily defined as an approximately 480 year period spanning AD 1440–1920, although not all of this period was notably cold. While the MM occurred within the much longer LIA period, the timing of the features are not suggestive of causation and should not, in isolation, be used as evidence of significant solar forcing of climate. Climate model simulations suggest multiple factors, particularly volcanic activity, were crucial for causing the cooler temperatures in the northern hemisphere during the LIA. A reduction in total solar irradiance likely contributed to the LIA at a level comparable to changing land use.https://doi.org/10.1051/swsc/2017034Space climatetotal irradianceclimatesunspotclimate change |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Owens Mathew J. Lockwood Mike Hawkins Ed Usoskin Ilya Jones Gareth S. Barnard Luke Schurer Andrew Fasullo John |
spellingShingle |
Owens Mathew J. Lockwood Mike Hawkins Ed Usoskin Ilya Jones Gareth S. Barnard Luke Schurer Andrew Fasullo John The Maunder minimum and the Little Ice Age: an update from recent reconstructions and climate simulations Journal of Space Weather and Space Climate Space climate total irradiance climate sunspot climate change |
author_facet |
Owens Mathew J. Lockwood Mike Hawkins Ed Usoskin Ilya Jones Gareth S. Barnard Luke Schurer Andrew Fasullo John |
author_sort |
Owens Mathew J. |
title |
The Maunder minimum and the Little Ice Age: an update from recent reconstructions and climate simulations |
title_short |
The Maunder minimum and the Little Ice Age: an update from recent reconstructions and climate simulations |
title_full |
The Maunder minimum and the Little Ice Age: an update from recent reconstructions and climate simulations |
title_fullStr |
The Maunder minimum and the Little Ice Age: an update from recent reconstructions and climate simulations |
title_full_unstemmed |
The Maunder minimum and the Little Ice Age: an update from recent reconstructions and climate simulations |
title_sort |
maunder minimum and the little ice age: an update from recent reconstructions and climate simulations |
publisher |
EDP Sciences |
series |
Journal of Space Weather and Space Climate |
issn |
2115-7251 |
publishDate |
2017-01-01 |
description |
The Maunder minimum (MM) was a period of extremely low solar activity from approximately AD 1650 to 1715. In the solar physics literature, the MM is sometimes associated with a period of cooler global temperatures, referred to as the Little Ice Age (LIA), and thus taken as compelling evidence of a large, direct solar influence on climate. In this study, we bring together existing simulation and observational studies, particularly the most recent solar activity and paleoclimate reconstructions, to examine this relation. Using northern hemisphere surface air temperature reconstructions, the LIA can be most readily defined as an approximately 480 year period spanning AD 1440–1920, although not all of this period was notably cold. While the MM occurred within the much longer LIA period, the timing of the features are not suggestive of causation and should not, in isolation, be used as evidence of significant solar forcing of climate. Climate model simulations suggest multiple factors, particularly volcanic activity, were crucial for causing the cooler temperatures in the northern hemisphere during the LIA. A reduction in total solar irradiance likely contributed to the LIA at a level comparable to changing land use. |
topic |
Space climate total irradiance climate sunspot climate change |
url |
https://doi.org/10.1051/swsc/2017034 |
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