TY - JOUR A1 - Pena-Angulo, D. A1 - Nadal-Romero, E. A1 - Gonzalez-Hidalgo, J. C. A1 - Albaladejo, J. A1 - Andreu, V A1 - Bagarello, V A1 - Barhi, H. A1 - Batalla, R. J. A1 - Bernal, S. A1 - Bienes, R. A1 - Campo, J. A1 - Campo-Bescos, M. A. A1 - Canatario-Duarte, A. A1 - Canton, Y. A1 - Casali, J. A1 - Castillo, V A1 - Cerda, Artemi A1 - Cheggour, A. A1 - Cid, Patricio A1 - Cortesi, N. A1 - Desir, G. A1 - Diaz-Pereira, E. A1 - Espigares, T. A1 - Estrany, Joan A1 - Fernandez-Raga, M. A1 - Ferreira, Carla S. S. A1 - Ferro, Vito A1 - Gallart, Francesc A1 - Gimenez, R. A1 - Gimeno, E. A1 - Gomez, J. A. A1 - Gomez-Gutierrez, A. A1 - Gomez-Macpherson, H. A1 - Gonzalez-Pelayo, O. A1 - Hueso-Gonzalez, P. A1 - Kairis, O. A1 - Karatzas, G. P. A1 - Klotz, S. A1 - Kosmas, C. A1 - Lana-Renault, Noemi A1 - Lasanta, T. A1 - Latron, J. A1 - Lazaro, R. A1 - Le Bissonnais, Y. A1 - Le Bouteiller, C. A1 - Licciardello, F. A1 - Lopez-Tarazon, José Andrés A1 - Lucia, A. A1 - Marin, C. A1 - Marques, M. J. A1 - Martinez-Fernandez, J. A1 - Martinez-Mena, M. A1 - Martinez-Murillo, J. F. A1 - Mateos, L. A1 - Mathys, N. A1 - Merino-Martin, L. A1 - Moreno-de las Heras, M. A1 - Moustakas, N. A1 - Nicolau, J. M. A1 - Novara, A. A1 - Pampalone, V A1 - Raclot, D. A1 - Rodriguez-Blanco, M. L. A1 - Rodrigo-Comino, Jesús A1 - Romero-Diaz, A. A1 - Roose, E. A1 - Rubio, J. L. A1 - Ruiz-Sinoga, J. D. A1 - Schnabel, S. A1 - Senciales-Gonzalez, J. M. A1 - Simonneaux, V A1 - Sole-Benet, A. A1 - Taguas, E. A1 - Taboada-Castro, M. M. A1 - Taboada-Castro, M. T. A1 - Todisco, Francesca A1 - Ubeda, X. A1 - Varouchakis, E. A. A1 - Vericat, Damia A1 - Wittenberg, L. A1 - Zabaleta, A. A1 - Zorn, M. T1 - Spatial variability of the relationships of runoff and sediment yield with weather types throughout the Mediterranean basin JF - Journal of hydrology N2 - 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. KW - Synoptic weather types KW - Erosion KW - Sediment yield KW - Runoff KW - Mediterranean basin Y1 - 2019 U6 - https://doi.org/10.1016/j.jhydrol.2019.01.059 SN - 0022-1694 SN - 1879-2707 VL - 571 SP - 390 EP - 405 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Park, Jungsu A1 - Batalla, Ramon J. A1 - Birgand, Francois A1 - Esteves, Michel A1 - Gentile, Francesco A1 - Harrington, Joseph R. A1 - Navratil, Oldrich A1 - Lopez-Tarazon, José Andrés A1 - Vericat, Damia T1 - Influences of Catchment and River Channel Characteristics on the Magnitude and Dynamics of Storage and Re-Suspension of Fine Sediments in River Beds JF - Water N2 - Fine particles or sediments are one of the important variables that should be considered for the proper management of water quality and aquatic ecosystems. In the present study, the effect of catchment characteristics on the performance of an already developed model for the estimation of fine sediments dynamics between the water column and sediment bed was tested, using 13 catchments distributed worldwide. The model was calibrated to determine two optimal model parameters. The first is the filtration parameter, which represents the filtration of fine sediments through pores of the stream bed during the recession period of a flood event. The second parameter is the bed erosion parameter that represents the active layer, directly related to the re-suspension of fine sediments during a flood event. A dependency of the filtration parameter with the catchment area was observed in catchments smaller than 100 km(2), whereas no particular relationship was observed for larger catchments (>100 km(2)). In contrast, the bed erosion parameter does not show a noticeable dependency with the area or other environmental characteristics. The model estimated the mass of fine sediments released from the sediment bed to the water column during flood events in the 13 catchments within 23% bias. KW - bed erosion KW - catchment area KW - filtration KW - sediment accumulation KW - sediment bed fluidization KW - sediment re-suspension Y1 - 2019 U6 - https://doi.org/10.3390/w11050878 SN - 2073-4441 VL - 11 IS - 5 PB - MDPI CY - Basel ER -