Explaining extreme events of 2012 from a climate perspective

© 2013 American Meteorological Society. Artículo firmado por 78 autores. Attribution of extreme events is a challenging science and one that is currently undergoing considerable evolution. In this paper are 19 analyses by 18 different research groups, often using quite different methodologies, of 12...

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Published in:Bulletin of the American Meteorological Society
Main Authors: Barriopedro Cepero, David, García Herrera, Ricardo Francisco
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2013
Subjects:
52
Online Access:https://hdl.handle.net/20.500.14352/34231
https://doi.org/10.1175/BAMS-D-13-00085.1
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spelling ftunivcmadrid:oai:docta.ucm.es:20.500.14352/34231 2024-09-09T19:26:28+00:00 Explaining extreme events of 2012 from a climate perspective Barriopedro Cepero, David García Herrera, Ricardo Francisco 2013-09 application/pdf https://hdl.handle.net/20.500.14352/34231 https://doi.org/10.1175/BAMS-D-13-00085.1 eng eng American Meteorological Society https://hdl.handle.net/20.500.14352/34231 0003-0007 doi:10.1175/BAMS-D-13-00085.1 open access 52 Meteorology Atmospheric sciences Física atmosférica 2501 Ciencias de la Atmósfera journal article 2013 ftunivcmadrid https://doi.org/20.500.14352/3423110.1175/BAMS-D-13-00085.1 2024-08-29T23:43:41Z © 2013 American Meteorological Society. Artículo firmado por 78 autores. Attribution of extreme events is a challenging science and one that is currently undergoing considerable evolution. In this paper are 19 analyses by 18 different research groups, often using quite different methodologies, of 12 extreme events that occurred in 2012. In addition to investigating the causes of these extreme events, the multiple analyses of four of the events, the high temperatures in the United States, the record low levels of Arctic sea ice, and the heavy rain in northern Europe and eastern Australia, provide an opportunity to compare and contrast the strengths and weaknesses of the various methodologies. The differences also provide insights into the structural uncertainty of event attribution, that is, the uncertainty that arises directly from the differences in analysis methodology. In these cases, there was considerable agreement between the different assessments of the same event. However, different events had very different causes. Approximately half the analyses found some evidence that anthropogenically caused climate change was a contributing factor to the extreme event examined, though the effects of natural fluctuations of weather and climate on the evolution of many of the extreme events played key roles as well. Depto. de Física de la Tierra y Astrofísica Fac. de Ciencias Físicas TRUE pub Article in Journal/Newspaper Arctic Climate change Sea ice Docta Complutense (Universidad Complutense de Madrid - UCM) Arctic Bulletin of the American Meteorological Society 94 9 S1 S74
institution Open Polar
collection Docta Complutense (Universidad Complutense de Madrid - UCM)
op_collection_id ftunivcmadrid
language English
topic 52
Meteorology
Atmospheric sciences
Física atmosférica
2501 Ciencias de la Atmósfera
spellingShingle 52
Meteorology
Atmospheric sciences
Física atmosférica
2501 Ciencias de la Atmósfera
Barriopedro Cepero, David
García Herrera, Ricardo Francisco
Explaining extreme events of 2012 from a climate perspective
topic_facet 52
Meteorology
Atmospheric sciences
Física atmosférica
2501 Ciencias de la Atmósfera
description © 2013 American Meteorological Society. Artículo firmado por 78 autores. Attribution of extreme events is a challenging science and one that is currently undergoing considerable evolution. In this paper are 19 analyses by 18 different research groups, often using quite different methodologies, of 12 extreme events that occurred in 2012. In addition to investigating the causes of these extreme events, the multiple analyses of four of the events, the high temperatures in the United States, the record low levels of Arctic sea ice, and the heavy rain in northern Europe and eastern Australia, provide an opportunity to compare and contrast the strengths and weaknesses of the various methodologies. The differences also provide insights into the structural uncertainty of event attribution, that is, the uncertainty that arises directly from the differences in analysis methodology. In these cases, there was considerable agreement between the different assessments of the same event. However, different events had very different causes. Approximately half the analyses found some evidence that anthropogenically caused climate change was a contributing factor to the extreme event examined, though the effects of natural fluctuations of weather and climate on the evolution of many of the extreme events played key roles as well. Depto. de Física de la Tierra y Astrofísica Fac. de Ciencias Físicas TRUE pub
format Article in Journal/Newspaper
author Barriopedro Cepero, David
García Herrera, Ricardo Francisco
author_facet Barriopedro Cepero, David
García Herrera, Ricardo Francisco
author_sort Barriopedro Cepero, David
title Explaining extreme events of 2012 from a climate perspective
title_short Explaining extreme events of 2012 from a climate perspective
title_full Explaining extreme events of 2012 from a climate perspective
title_fullStr Explaining extreme events of 2012 from a climate perspective
title_full_unstemmed Explaining extreme events of 2012 from a climate perspective
title_sort explaining extreme events of 2012 from a climate perspective
publisher American Meteorological Society
publishDate 2013
url https://hdl.handle.net/20.500.14352/34231
https://doi.org/10.1175/BAMS-D-13-00085.1
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Sea ice
genre_facet Arctic
Climate change
Sea ice
op_relation https://hdl.handle.net/20.500.14352/34231
0003-0007
doi:10.1175/BAMS-D-13-00085.1
op_rights open access
op_doi https://doi.org/20.500.14352/3423110.1175/BAMS-D-13-00085.1
container_title Bulletin of the American Meteorological Society
container_volume 94
container_issue 9
container_start_page S1
op_container_end_page S74
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