Atmospheric circulation influence on the interannual variability of snow pack in the Spanish Pyrenees during the second half of the 20th century

12 páginas, 5 figuras, 6 tablas. Large areas in the Spanish Pyrenees are covered by snow between December and April, especially above 1650 m a.s.l., the location of the cold season 0°C isotherm. However, a significant negative trend in Pyrenean snow pack was detected during the second half of the 20...

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Published in:Hydrology Research
Main Authors: López-Moreno, Juan I., Vicente Serrano, Sergio M.
Format: Article in Journal/Newspaper
Language:English
Published: IWA Publishing 2007
Subjects:
ren
Online Access:http://hdl.handle.net/10261/35379
https://doi.org/10.2166/nh.2007.030
id ftcsic:oai:digital.csic.es:10261/35379
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spelling ftcsic:oai:digital.csic.es:10261/35379 2024-02-11T10:06:16+01:00 Atmospheric circulation influence on the interannual variability of snow pack in the Spanish Pyrenees during the second half of the 20th century López-Moreno, Juan I. Vicente Serrano, Sergio M. 2007 http://hdl.handle.net/10261/35379 https://doi.org/10.2166/nh.2007.030 en eng IWA Publishing http://dx.doi.org/10.2166/nh.2007.030 Nordic Hydrology 38(1): 33-44 (2007) 0029-1277 http://hdl.handle.net/10261/35379 doi:10.2166/nh.2007.030 open Iberian Peninsula North Atlantic Oscillation Snow accumulation Spanish Pyrenees Weather types artículo http://purl.org/coar/resource_type/c_6501 2007 ftcsic https://doi.org/10.2166/nh.2007.030 2024-01-16T09:31:35Z 12 páginas, 5 figuras, 6 tablas. Large areas in the Spanish Pyrenees are covered by snow between December and April, especially above 1650 m a.s.l., the location of the cold season 0°C isotherm. However, a significant negative trend in Pyrenean snow pack was detected during the second half of the 20th century. This paper analyses the interannual evolution of snow accumulation in these mountains in relation to the variability of atmospheric circulation. The study considers two spatial scales, from weather types over the Iberian Peninsula to hemispheric atmospheric patterns. The results show strong relationships between the annual occurrence of several weather types and spring snow accumulation. Changes in the frequency of several weather types are explained by the evolution of large scale hemispheric circulation patterns, especially the North Atlantic Oscillation (NAO). Thus, the positive trend observed in the NAO index leads to a decrease in the occurrence of types that favour snow accumulation and an increase in unfavourable conditions for snow pack during the second half of the 20th century. This study was supported by the following research projects: PIRIHEROS, REN 2003- 08678/HID, CGL2005-04508/BOS and CANOA, CGL 2004-04919-c02-01, all funded by the CICYT, Spanish Ministry of Science and Technology. The research of the authors was supported by postdoctoral fellowships from the Spanish Ministry of Education, Culture and Sports, Spain. Peer reviewed Article in Journal/Newspaper North Atlantic North Atlantic oscillation ren Digital.CSIC (Spanish National Research Council) Hydrology Research 38 1 33 44
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
topic Iberian Peninsula
North Atlantic Oscillation
Snow accumulation
Spanish Pyrenees
Weather types
spellingShingle Iberian Peninsula
North Atlantic Oscillation
Snow accumulation
Spanish Pyrenees
Weather types
López-Moreno, Juan I.
Vicente Serrano, Sergio M.
Atmospheric circulation influence on the interannual variability of snow pack in the Spanish Pyrenees during the second half of the 20th century
topic_facet Iberian Peninsula
North Atlantic Oscillation
Snow accumulation
Spanish Pyrenees
Weather types
description 12 páginas, 5 figuras, 6 tablas. Large areas in the Spanish Pyrenees are covered by snow between December and April, especially above 1650 m a.s.l., the location of the cold season 0°C isotherm. However, a significant negative trend in Pyrenean snow pack was detected during the second half of the 20th century. This paper analyses the interannual evolution of snow accumulation in these mountains in relation to the variability of atmospheric circulation. The study considers two spatial scales, from weather types over the Iberian Peninsula to hemispheric atmospheric patterns. The results show strong relationships between the annual occurrence of several weather types and spring snow accumulation. Changes in the frequency of several weather types are explained by the evolution of large scale hemispheric circulation patterns, especially the North Atlantic Oscillation (NAO). Thus, the positive trend observed in the NAO index leads to a decrease in the occurrence of types that favour snow accumulation and an increase in unfavourable conditions for snow pack during the second half of the 20th century. This study was supported by the following research projects: PIRIHEROS, REN 2003- 08678/HID, CGL2005-04508/BOS and CANOA, CGL 2004-04919-c02-01, all funded by the CICYT, Spanish Ministry of Science and Technology. The research of the authors was supported by postdoctoral fellowships from the Spanish Ministry of Education, Culture and Sports, Spain. Peer reviewed
format Article in Journal/Newspaper
author López-Moreno, Juan I.
Vicente Serrano, Sergio M.
author_facet López-Moreno, Juan I.
Vicente Serrano, Sergio M.
author_sort López-Moreno, Juan I.
title Atmospheric circulation influence on the interannual variability of snow pack in the Spanish Pyrenees during the second half of the 20th century
title_short Atmospheric circulation influence on the interannual variability of snow pack in the Spanish Pyrenees during the second half of the 20th century
title_full Atmospheric circulation influence on the interannual variability of snow pack in the Spanish Pyrenees during the second half of the 20th century
title_fullStr Atmospheric circulation influence on the interannual variability of snow pack in the Spanish Pyrenees during the second half of the 20th century
title_full_unstemmed Atmospheric circulation influence on the interannual variability of snow pack in the Spanish Pyrenees during the second half of the 20th century
title_sort atmospheric circulation influence on the interannual variability of snow pack in the spanish pyrenees during the second half of the 20th century
publisher IWA Publishing
publishDate 2007
url http://hdl.handle.net/10261/35379
https://doi.org/10.2166/nh.2007.030
genre North Atlantic
North Atlantic oscillation
ren
genre_facet North Atlantic
North Atlantic oscillation
ren
op_relation http://dx.doi.org/10.2166/nh.2007.030
Nordic Hydrology 38(1): 33-44 (2007)
0029-1277
http://hdl.handle.net/10261/35379
doi:10.2166/nh.2007.030
op_rights open
op_doi https://doi.org/10.2166/nh.2007.030
container_title Hydrology Research
container_volume 38
container_issue 1
container_start_page 33
op_container_end_page 44
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