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Assessing multidecadal runoff (1970–2010) using regional hydrological modelling under data and water scarcity conditions in Peruvian Pacific catchment
dc.contributor.author | Rau, P. | |
dc.contributor.author | Bourrel, L. | |
dc.contributor.author | Labat, D. | |
dc.contributor.author | Ruelland, D. | |
dc.contributor.author | Frappart, F. | |
dc.contributor.author | Lavado-Casimiro, W. | |
dc.contributor.author | Dewitte, v | |
dc.contributor.author | Felipe-Obando, Oscar | |
dc.date.accessioned | 2019-07-07T18:41:17Z | |
dc.date.available | 2019-07-07T18:41:17Z | |
dc.date.issued | 2019-01 | |
dc.identifier.citation | Rau, P., Bourrel, L., Labat, D., Ruelland, D., Frappart, F., Lavado, W., … Felipe, O. (2019). Assessing multidecadal runoff (1970–2010) using regional hydrological modelling under data and water scarcity conditions in Peruvian Pacific catchments. Hydrological Processes, 33(1), 20–35. https://doi.org/10.1002/hyp.13318 | es_PE |
dc.identifier.uri | http://repositorio.senamhi.gob.pe/handle/20.500.12542/41 | |
dc.description.abstract | In a context of water scarcity in Peruvian Pacific catchments as a crucial issue for Peru, added to the paucity of data availability, we propose a methodology that provides new perspectives for freshwater availability estimation as a base reference for unimpaired conditions. Under those considerations, a regional discharge of 709 m3/s to the Pacific Ocean is estimated with a significant increasing trend of about 43 m3/s per decade over the 1970–2010 period. To represent the multidecadal behaviour of freshwater runoff along the region, a regional runoff analysis is proposed based on hydrological modelling at annual and monthly time step for unimpaired conditions over the whole 1970–2010 period. Differential Split-Sample Tests are used to assess the hydrological modelling robustness of the GR1A and GR2M conceptual lumped models, showing a satisfactory transposability from dry to wet years inside the thresholds defined for Nash–Sutcliffe and bias criteria. This allowed relating physical catchment characteristics with calibrated and validated model parameters, thus offering a regional perspective for dryland conditions in the study area (e.g., the anticlockwise hysteresis relationship found for seasonal precipitation–runoff relationship) as well as the impacts of climate variability and catchment characteristics. | en_US |
dc.description.sponsorship | Fondo Nacional de Desarrollo Científico, Tecnológico y de Innovación Tecnológica | en_US |
dc.format | application/pdf | |
dc.language.iso | eng | en_US |
dc.publisher | John Wiley and Sons Ltd | en_US |
dc.relation.ispartof | urn:issn:0885-6087 | |
dc.rights | info:eu-repo/semantics/openAccess | es_PE |
dc.rights | Attribution-NonCommercial-ShareAlike 3.0 United States | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-sa/3.0/us/ | * |
dc.source | Servicio Nacional de Meteorología e Hidrología del Perú | es_PE |
dc.source | Repositorio Institucional - SENAMHI | es_PE |
dc.subject | Dta and water scarcity | en_US |
dc.subject | GR1A | en_US |
dc.subject | GR2M | en_US |
dc.subject | hydrological modelling | en_US |
dc.subject | Peru | en_US |
dc.subject | Regional runoff | en_US |
dc.subject | Catchment | en_US |
dc.subject | Climate models | en_US |
dc.subject | Water | en_US |
dc.title | Assessing multidecadal runoff (1970–2010) using regional hydrological modelling under data and water scarcity conditions in Peruvian Pacific catchment | en_US |
dc.type | info:eu-repo/semantics/article | en_US |
dc.identifier.isni | 0000 0001 0746 0446 | |
dc.description.peerreview | Por pares | |
dc.identifier.doi | https://doi.org/ 10.1002/hyp.13318 | |
dc.source.volume | 33 | es_PE |
dc.source.issue | 1 | es_PE |
dc.source.initialpage | 20 | es_PE |
dc.source.initialpage | ||
dc.source.endpage | 35 | es_PE |
dc.source.journal | Hydrological Processes | es_PE |
dc.subject.sinia | conservacion y recuperacion de cuencas hidrograficas - Agua | |
dc.type.sinia | text/publicacion cientifica | |
dc.identifier.url | https://hdl.handle.net/20.500.12542/41 |
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