The response of Iberian rivers to the North Atlantic Oscillation
In this study we analyzed the influence of the North Atlantic Oscillation (NAO) on the streamflow in 187 sub-basins of the Iberian Peninsula. Monthly and one-month lagged correlations were conducted to assess the spatio-temporal extent of the NAO influence on Iberian river discharges. Analysis of th...
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ftdoajarticles:oai:doaj.org/article:5490ab866ad1453fbf2c3db943593228 2023-05-15T17:29:57+02:00 The response of Iberian rivers to the North Atlantic Oscillation J. Lorenzo-Lacruz S. M. Vicente-Serrano J. I. López-Moreno J. C. González-Hidalgo E. Morán-Tejeda 2011-08-01T00:00:00Z https://doi.org/10.5194/hess-15-2581-2011 https://doaj.org/article/5490ab866ad1453fbf2c3db943593228 EN eng Copernicus Publications http://www.hydrol-earth-syst-sci.net/15/2581/2011/hess-15-2581-2011.pdf https://doaj.org/toc/1027-5606 https://doaj.org/toc/1607-7938 doi:10.5194/hess-15-2581-2011 1027-5606 1607-7938 https://doaj.org/article/5490ab866ad1453fbf2c3db943593228 Hydrology and Earth System Sciences, Vol 15, Iss 8, Pp 2581-2597 (2011) Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 article 2011 ftdoajarticles https://doi.org/10.5194/hess-15-2581-2011 2022-12-31T14:05:53Z In this study we analyzed the influence of the North Atlantic Oscillation (NAO) on the streamflow in 187 sub-basins of the Iberian Peninsula. Monthly and one-month lagged correlations were conducted to assess the spatio-temporal extent of the NAO influence on Iberian river discharges. Analysis of the persistence of the winter NAO throughout the year was also undertaken, together with analysis of streamflow anomalies during positive and negative NAO phases. Moving-window correlation analyses were conducted to assess potential changes in the temporal evolution of the NAO influence on Iberian streamflows. The results show that the NAO has a large impact on surface water resources throughout the Iberian Peninsula during winter, and in the Atlantic watershed during autumn. We showed that water resources management and snowmelt are causing the persistent dependence of streamflows on the previous winter NAO. We found that strongly positive streamflow anomalies occurred during winter, especially in the Atlantic watershed, and provide evidence of non-stationarity and spatial variability in the NAO influence on Iberian water resources. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles Hydrology and Earth System Sciences 15 8 2581 2597 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 |
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Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 J. Lorenzo-Lacruz S. M. Vicente-Serrano J. I. López-Moreno J. C. González-Hidalgo E. Morán-Tejeda The response of Iberian rivers to the North Atlantic Oscillation |
topic_facet |
Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 |
description |
In this study we analyzed the influence of the North Atlantic Oscillation (NAO) on the streamflow in 187 sub-basins of the Iberian Peninsula. Monthly and one-month lagged correlations were conducted to assess the spatio-temporal extent of the NAO influence on Iberian river discharges. Analysis of the persistence of the winter NAO throughout the year was also undertaken, together with analysis of streamflow anomalies during positive and negative NAO phases. Moving-window correlation analyses were conducted to assess potential changes in the temporal evolution of the NAO influence on Iberian streamflows. The results show that the NAO has a large impact on surface water resources throughout the Iberian Peninsula during winter, and in the Atlantic watershed during autumn. We showed that water resources management and snowmelt are causing the persistent dependence of streamflows on the previous winter NAO. We found that strongly positive streamflow anomalies occurred during winter, especially in the Atlantic watershed, and provide evidence of non-stationarity and spatial variability in the NAO influence on Iberian water resources. |
format |
Article in Journal/Newspaper |
author |
J. Lorenzo-Lacruz S. M. Vicente-Serrano J. I. López-Moreno J. C. González-Hidalgo E. Morán-Tejeda |
author_facet |
J. Lorenzo-Lacruz S. M. Vicente-Serrano J. I. López-Moreno J. C. González-Hidalgo E. Morán-Tejeda |
author_sort |
J. Lorenzo-Lacruz |
title |
The response of Iberian rivers to the North Atlantic Oscillation |
title_short |
The response of Iberian rivers to the North Atlantic Oscillation |
title_full |
The response of Iberian rivers to the North Atlantic Oscillation |
title_fullStr |
The response of Iberian rivers to the North Atlantic Oscillation |
title_full_unstemmed |
The response of Iberian rivers to the North Atlantic Oscillation |
title_sort |
response of iberian rivers to the north atlantic oscillation |
publisher |
Copernicus Publications |
publishDate |
2011 |
url |
https://doi.org/10.5194/hess-15-2581-2011 https://doaj.org/article/5490ab866ad1453fbf2c3db943593228 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_source |
Hydrology and Earth System Sciences, Vol 15, Iss 8, Pp 2581-2597 (2011) |
op_relation |
http://www.hydrol-earth-syst-sci.net/15/2581/2011/hess-15-2581-2011.pdf https://doaj.org/toc/1027-5606 https://doaj.org/toc/1607-7938 doi:10.5194/hess-15-2581-2011 1027-5606 1607-7938 https://doaj.org/article/5490ab866ad1453fbf2c3db943593228 |
op_doi |
https://doi.org/10.5194/hess-15-2581-2011 |
container_title |
Hydrology and Earth System Sciences |
container_volume |
15 |
container_issue |
8 |
container_start_page |
2581 |
op_container_end_page |
2597 |
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1766125205193752576 |