Trends in rainfall erosivity in NE Spain at annual, seasonal and daily scales, 1955-2006

9 Pags., 4 Tabls., 4 Figs. Rainfall erosivity refers to the ability of precipitation to erode soil, and depends on characteristics such as its total volume, duration, and intensity and amount of energy released by raindrops. Despite the relevance of rainfall erosivity for soil degradation prevention...

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Published in:Hydrology and Earth System Sciences
Main Authors: Angulo-Martínez, Marta, Beguería, Santiago
Format: Article in Journal/Newspaper
Language:English
Published: European Geosciences Union 2012
Subjects:
Online Access:http://hdl.handle.net/10261/58047
https://doi.org/10.5194/hess-16-3551-2012
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spelling ftcsic:oai:digital.csic.es:10261/58047 2024-02-11T10:06:32+01:00 Trends in rainfall erosivity in NE Spain at annual, seasonal and daily scales, 1955-2006 Angulo-Martínez, Marta Beguería, Santiago 2012-10 http://hdl.handle.net/10261/58047 https://doi.org/10.5194/hess-16-3551-2012 en eng European Geosciences Union http://dx.doi.org/10.5194/hess-16-3551-2012 Angulo-Martínez M, Beguería S. Trends in rainfall erosivity in NE Spain at annual, seasonal and daily scales, 1955-2006. Hydrological and Earth System Sciences 16 (10): 3551-3559 (2012) 1027-5606 http://hdl.handle.net/10261/58047 doi:10.5194/hess-16-3551-2012 1607-7938 open artículo http://purl.org/coar/resource_type/c_6501 2012 ftcsic https://doi.org/10.5194/hess-16-3551-2012 2024-01-16T09:41:32Z 9 Pags., 4 Tabls., 4 Figs. Rainfall erosivity refers to the ability of precipitation to erode soil, and depends on characteristics such as its total volume, duration, and intensity and amount of energy released by raindrops. Despite the relevance of rainfall erosivity for soil degradation prevention, very few studies have addressed its spatial and temporal variability. In this study the time variation of rainfall erosivity in the Ebro Valley (NE Spain) is assessed for the period 1955–2006. The results show a general decrease in annual and seasonal rainfall erosivity, which is explained by a decrease of very intense rainfall events whilst the frequency of moderate and low events increased. This trend is related to prevailing positive conditions of the main atmospheric teleconnection indices affecting the West Mediterranean, i.e. the North Atlantic Oscillation (NAO), the Mediterranean Oscillation (MO) and the Western Mediterranean Oscillation (WeMO). This work has been supported by research projects CGL2011- 24185 financed by the Spanish Ministry of Science and Innovation (CICYT) and the European Regional Development Fund (ERDFFEDER), 2010CZ0021 financed by the Spanish National Research Council (Consejo Superior de Investigaciones Científicas-CSIC) and the Czech Academy of Sciences, and “Grupo de Investigación E68: Geomorfología y Cambio Global” financed by the Aragón Government and the European Social Fund (ESF-FSE). Research of M. A.-M. was supported by a JAE-Predoc grant from the Spanish National Research Council (Consejo Superior de Investigaciones Científicas-CSIC). Peer reviewed Article in Journal/Newspaper North Atlantic North Atlantic oscillation Digital.CSIC (Spanish National Research Council) Hydrology and Earth System Sciences 16 10 3551 3559
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
description 9 Pags., 4 Tabls., 4 Figs. Rainfall erosivity refers to the ability of precipitation to erode soil, and depends on characteristics such as its total volume, duration, and intensity and amount of energy released by raindrops. Despite the relevance of rainfall erosivity for soil degradation prevention, very few studies have addressed its spatial and temporal variability. In this study the time variation of rainfall erosivity in the Ebro Valley (NE Spain) is assessed for the period 1955–2006. The results show a general decrease in annual and seasonal rainfall erosivity, which is explained by a decrease of very intense rainfall events whilst the frequency of moderate and low events increased. This trend is related to prevailing positive conditions of the main atmospheric teleconnection indices affecting the West Mediterranean, i.e. the North Atlantic Oscillation (NAO), the Mediterranean Oscillation (MO) and the Western Mediterranean Oscillation (WeMO). This work has been supported by research projects CGL2011- 24185 financed by the Spanish Ministry of Science and Innovation (CICYT) and the European Regional Development Fund (ERDFFEDER), 2010CZ0021 financed by the Spanish National Research Council (Consejo Superior de Investigaciones Científicas-CSIC) and the Czech Academy of Sciences, and “Grupo de Investigación E68: Geomorfología y Cambio Global” financed by the Aragón Government and the European Social Fund (ESF-FSE). Research of M. A.-M. was supported by a JAE-Predoc grant from the Spanish National Research Council (Consejo Superior de Investigaciones Científicas-CSIC). Peer reviewed
format Article in Journal/Newspaper
author Angulo-Martínez, Marta
Beguería, Santiago
spellingShingle Angulo-Martínez, Marta
Beguería, Santiago
Trends in rainfall erosivity in NE Spain at annual, seasonal and daily scales, 1955-2006
author_facet Angulo-Martínez, Marta
Beguería, Santiago
author_sort Angulo-Martínez, Marta
title Trends in rainfall erosivity in NE Spain at annual, seasonal and daily scales, 1955-2006
title_short Trends in rainfall erosivity in NE Spain at annual, seasonal and daily scales, 1955-2006
title_full Trends in rainfall erosivity in NE Spain at annual, seasonal and daily scales, 1955-2006
title_fullStr Trends in rainfall erosivity in NE Spain at annual, seasonal and daily scales, 1955-2006
title_full_unstemmed Trends in rainfall erosivity in NE Spain at annual, seasonal and daily scales, 1955-2006
title_sort trends in rainfall erosivity in ne spain at annual, seasonal and daily scales, 1955-2006
publisher European Geosciences Union
publishDate 2012
url http://hdl.handle.net/10261/58047
https://doi.org/10.5194/hess-16-3551-2012
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation http://dx.doi.org/10.5194/hess-16-3551-2012
Angulo-Martínez M, Beguería S. Trends in rainfall erosivity in NE Spain at annual, seasonal and daily scales, 1955-2006. Hydrological and Earth System Sciences 16 (10): 3551-3559 (2012)
1027-5606
http://hdl.handle.net/10261/58047
doi:10.5194/hess-16-3551-2012
1607-7938
op_rights open
op_doi https://doi.org/10.5194/hess-16-3551-2012
container_title Hydrology and Earth System Sciences
container_volume 16
container_issue 10
container_start_page 3551
op_container_end_page 3559
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