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Spatial variability of the relationships of runoff and sediment yield with weather types throughout the Mediterranean basin

  • Soil degradation by water is a serious environmental problem worldwide, with specific climatic factors being the major causes. We investigated the relationships between synoptic atmospheric patterns (i.e. weather types, WTs) and runoff, erosion and sediment yield throughout the Mediterranean basin by analyzing a large database of natural rainfall events at 68 research sites in 9 countries. Principal Component Analysis (PCA) was used to identify spatial relationships of the different WTs including three hydro-sedimentary variables: rainfall, runoff, and sediment yield (SY, used to refer to both soil erosion measured at plot scale and sediment yield registered at catchment scale). The results indicated 4 spatial classes of rainfall and runoff: (a) northern sites dependent on North (N) and North West (NW) flows; (b) eastern sites dependent on E and NE flows; (c) southern sites dependent on S and SE flows; and, finally, (d) western sites dependent on W and SW flows. Conversely, three spatial classes are identified for SY characterized by:Soil degradation by water is a serious environmental problem worldwide, with specific climatic factors being the major causes. We investigated the relationships between synoptic atmospheric patterns (i.e. weather types, WTs) and runoff, erosion and sediment yield throughout the Mediterranean basin by analyzing a large database of natural rainfall events at 68 research sites in 9 countries. Principal Component Analysis (PCA) was used to identify spatial relationships of the different WTs including three hydro-sedimentary variables: rainfall, runoff, and sediment yield (SY, used to refer to both soil erosion measured at plot scale and sediment yield registered at catchment scale). The results indicated 4 spatial classes of rainfall and runoff: (a) northern sites dependent on North (N) and North West (NW) flows; (b) eastern sites dependent on E and NE flows; (c) southern sites dependent on S and SE flows; and, finally, (d) western sites dependent on W and SW flows. Conversely, three spatial classes are identified for SY characterized by: (a) N and NE flows in northern sites (b) E flows in eastern sites, and (c) W and SW flows in western sites. Most of the rainfall, runoff and SY occurred during a small number of daily events, and just a few WTs accounted for large percentages of the total. Our results confirm that characterization by WT improves understanding of the general conditions under which runoff and SY occur, and provides useful information for understanding the spatial variability of runoff, and SY throughout the Mediterranean basin. The approach used here could be useful to aid of the design of regional water management and soil conservation measures.show moreshow less

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Author details:D. Pena-Angulo, E. Nadal-Romero, J. C. Gonzalez-Hidalgo, J. Albaladejo, V Andreu, V BagarelloORCiD, H. Barhi, R. J. Batalla, S. Bernal, R. Bienes, J. Campo, M. A. Campo-Bescos, A. Canatario-Duarte, Y. Canton, J. Casali, V CastilloORCiD, Artemi CerdaORCiD, A. Cheggour, Patricio CidORCiD, N. Cortesi, G. Desir, E. Diaz-Pereira, T. Espigares, Joan EstranyORCiD, M. Fernandez-Raga, Carla S. S. FerreiraORCiD, Vito FerroORCiD, Francesc GallartORCiD, R. Gimenez, E. Gimeno, J. A. Gomez, A. Gomez-Gutierrez, H. Gomez-Macpherson, O. Gonzalez-Pelayo, P. Hueso-Gonzalez, O. Kairis, G. P. Karatzas, S. Klotz, C. Kosmas, Noemi Lana-RenaultORCiD, T. Lasanta, J. Latron, R. Lazaro, Y. Le Bissonnais, C. Le Bouteiller, F. Licciardello, José Andrés Lopez-TarazonORCiDGND, A. Lucia, C. Marin, M. J. Marques, J. Martinez-Fernandez, M. Martinez-Mena, J. F. Martinez-Murillo, L. Mateos, N. Mathys, L. Merino-Martin, M. Moreno-de las Heras, N. Moustakas, J. M. Nicolau, A. Novara, V PampaloneORCiD, D. Raclot, M. L. Rodriguez-Blanco, Jesús Rodrigo-CominoORCiD, A. Romero-Diaz, E. Roose, J. L. Rubio, J. D. Ruiz-Sinoga, S. Schnabel, J. M. Senciales-Gonzalez, V SimonneauxORCiD, A. Sole-Benet, E. Taguas, M. M. Taboada-Castro, M. T. Taboada-Castro, Francesca TodiscoORCiD, X. Ubeda, E. A. Varouchakis, Damia VericatORCiD, L. Wittenberg, A. Zabaleta, M. Zorn
DOI:https://doi.org/10.1016/j.jhydrol.2019.01.059
ISSN:0022-1694
ISSN:1879-2707
Title of parent work (English):Journal of hydrology
Publisher:Elsevier
Place of publishing:Amsterdam
Publication type:Article
Language:English
Date of first publication:2019/02/07
Publication year:2019
Release date:2021/03/10
Tag:Erosion; Mediterranean basin; Runoff; Sediment yield; Synoptic weather types
Volume:571
Number of pages:16
First page:390
Last Page:405
Funding institution:MINECO-FEDER [CGL2014-52135-C3-3-R, CGL2014-59946-R, CGL2015-65569-R, CGL2015-64284-C2-2-R, PCIN-2017-061/AEI]; Spanish Ministry of Economy and Competitiveness, MEC [RYC-2013-14371, RYC-2010-06264]; Spanish Ministry of Education, Culture and Sports; Portuguese Science and Technology FoundationPortuguese Foundation for Science and Technology [SFRH/BPD/120093/2016]; Juan de la Cierva postdoctoral contract from the MEC [IJCI-2015-26463]; Vicenc Mut postdoctoral fellowship from the Autonomous Balearic Government [CAIB PD/038/2016]; Secretariat for Universities and Research of the Department of the Economy and Knowledge of the Autonomous Government of Catalonia [2014 SGR 645]; CERCA Programme; COST action CONNECTEUREuropean Cooperation in Science and Technology (COST) [ES1306]
Organizational units:Mathematisch-Naturwissenschaftliche Fakultät / Institut für Umweltwissenschaften und Geographie
DDC classification:5 Naturwissenschaften und Mathematik / 55 Geowissenschaften, Geologie / 550 Geowissenschaften
Peer review:Referiert
Publishing method:Open Access / Green Open-Access
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