Ensemble meteorological reconstruction using circulation analogues of 1781–1785
This paper uses a method of atmospheric flow analogues to reconstruct an ensemble of atmospheric variables (namely sea-level pressure, surface temperature and wind speed) between 1781 and 1785. The properties of this ensemble are investigated and tested against observations of temperature. The goal...
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Series: | Climate of the Past |
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doaj-d6ea76054d504fe18506c2af057e3af22020-11-24T21:26:02ZengCopernicus PublicationsClimate of the Past1814-93241814-93322014-04-0110279780910.5194/cp-10-797-2014Ensemble meteorological reconstruction using circulation analogues of 1781–1785P. Yiou0M. Boichu1R. Vautard2M. Vrac3S. Jourdain4E. Garnier5F. Fluteau6L. Menut7Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ & IPSL – UMR8212, CE Saclay l'Orme des Merisiers, 91191 Gif-sur-Yvette, FranceLaboratoire de Météorologie Dynamique, UMR8539 X-ENS-UPMC & IPSL, Ecole Polytechnique, 91128 Palaiseau, FranceLaboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ & IPSL – UMR8212, CE Saclay l'Orme des Merisiers, 91191 Gif-sur-Yvette, FranceLaboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ & IPSL – UMR8212, CE Saclay l'Orme des Merisiers, 91191 Gif-sur-Yvette, FranceDClim, Météo France, 42 Avenue G. Coriolis, 31057 Toulouse, FranceInstitut Universitaire de France and Centre de Recherche d'Histoire Quantitative, CNRS – UMR6583 Université de Caen, 14032 Caen, FranceInstitut de Physique du Globe, UMR7154, Sorbonne Paris Cité, 1 rue Jussieu, 75238 Paris, FranceLaboratoire de Météorologie Dynamique, UMR8539 X-ENS-UPMC & IPSL, Ecole Polytechnique, 91128 Palaiseau, FranceThis paper uses a method of atmospheric flow analogues to reconstruct an ensemble of atmospheric variables (namely sea-level pressure, surface temperature and wind speed) between 1781 and 1785. The properties of this ensemble are investigated and tested against observations of temperature. The goal of the paper is to assess whether the atmospheric circulation during the Laki volcanic eruption (in 1783) and the subsequent winter were similar to the conditions that prevailed in the winter 2009/2010 and during spring 2010. We find that the 3 months following the Laki eruption in June 1783 barely had analogues in 2010. The cold winter of 1783/1784 yielded circulation analogues in 2009/2010. The reconstructed surface temperature over land bears significant correlations with local observations, although the amplitude of the reconstruction is weaker.http://www.clim-past.net/10/797/2014/cp-10-797-2014.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
P. Yiou M. Boichu R. Vautard M. Vrac S. Jourdain E. Garnier F. Fluteau L. Menut |
spellingShingle |
P. Yiou M. Boichu R. Vautard M. Vrac S. Jourdain E. Garnier F. Fluteau L. Menut Ensemble meteorological reconstruction using circulation analogues of 1781–1785 Climate of the Past |
author_facet |
P. Yiou M. Boichu R. Vautard M. Vrac S. Jourdain E. Garnier F. Fluteau L. Menut |
author_sort |
P. Yiou |
title |
Ensemble meteorological reconstruction using circulation analogues of 1781–1785 |
title_short |
Ensemble meteorological reconstruction using circulation analogues of 1781–1785 |
title_full |
Ensemble meteorological reconstruction using circulation analogues of 1781–1785 |
title_fullStr |
Ensemble meteorological reconstruction using circulation analogues of 1781–1785 |
title_full_unstemmed |
Ensemble meteorological reconstruction using circulation analogues of 1781–1785 |
title_sort |
ensemble meteorological reconstruction using circulation analogues of 1781–1785 |
publisher |
Copernicus Publications |
series |
Climate of the Past |
issn |
1814-9324 1814-9332 |
publishDate |
2014-04-01 |
description |
This paper uses a method of atmospheric flow analogues to reconstruct an
ensemble of atmospheric variables (namely sea-level pressure, surface
temperature and wind speed) between 1781 and 1785. The properties of this
ensemble are investigated and tested against observations of temperature. The
goal of the paper is to assess whether the atmospheric circulation during the
Laki volcanic eruption (in 1783) and the subsequent winter were similar to
the conditions that prevailed in the winter 2009/2010 and during spring 2010.
We find that the 3 months following the Laki eruption in June 1783 barely
had analogues in 2010. The cold winter of 1783/1784 yielded circulation
analogues in 2009/2010. The reconstructed surface temperature over land bears
significant correlations with local observations, although the amplitude of
the reconstruction is weaker. |
url |
http://www.clim-past.net/10/797/2014/cp-10-797-2014.pdf |
work_keys_str_mv |
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