Assessment of the Role of Snowmelt in a Flood Event in a Gauged Catchment
An actual event that happened in the Roncal valley (Spain) is investigated and the results are compared between models with and without snowmelt. A distributed rainfall model is generated with the specific data recorded by the rain gauges of the catchment during the episode. To describe the process...
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| Veröffentlicht in: | Water (Basel) 2019-03, Vol.11 (3), p.506 |
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| creator | Mateo-Lázaro, Jesús Castillo-Mateo, Jorge Sánchez-Navarro, José Fuertes-Rodríguez, Víctor García-Gil, Alejandro Edo-Romero, Vanesa |
| description | An actual event that happened in the Roncal valley (Spain) is investigated and the results are compared between models with and without snowmelt. A distributed rainfall model is generated with the specific data recorded by the rain gauges of the catchment during the episode. To describe the process of water routing in the hydrological cycle of the basin, a model is used based on combinations of parallel linear reservoirs (PLR model), distribution by the basin, and tip-out into its drainage network configured using a digital terrain model (DTM). This PLR model allows simulation of the different actual reservoirs of the basin, including the snow and the contribution due to its melting which, in the model, depends on the temperature. The PLR model also allows for a water budget of the episode where, in addition to the effective rainfall contribution, the water that comes from the thaw is taken into account. The PLR model also allows determination of the amount of water that exists in the basin before and after the episode, data of great interest. When comparing the simulations with and without taking into account the thawing process, it is evident that the intervention of the snow reservoir has been decisive in causing a flood to occur. |
| doi_str_mv | 10.3390/w11030506 |
| format | Article |
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A distributed rainfall model is generated with the specific data recorded by the rain gauges of the catchment during the episode. To describe the process of water routing in the hydrological cycle of the basin, a model is used based on combinations of parallel linear reservoirs (PLR model), distribution by the basin, and tip-out into its drainage network configured using a digital terrain model (DTM). This PLR model allows simulation of the different actual reservoirs of the basin, including the snow and the contribution due to its melting which, in the model, depends on the temperature. The PLR model also allows for a water budget of the episode where, in addition to the effective rainfall contribution, the water that comes from the thaw is taken into account. The PLR model also allows determination of the amount of water that exists in the basin before and after the episode, data of great interest. When comparing the simulations with and without taking into account the thawing process, it is evident that the intervention of the snow reservoir has been decisive in causing a flood to occur.</description><identifier>ISSN: 2073-4441</identifier><identifier>EISSN: 2073-4441</identifier><identifier>DOI: 10.3390/w11030506</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Causes of ; Drainage patterns ; Environmental aspects ; Floods ; Gauges ; Hydrologic cycle ; Hydrology ; Investigations ; Measurement ; Moisture content ; Rain and rainfall ; Rain gauges ; Rainfall ; Reservoirs ; Snow ; Snowmelt ; Soil erosion ; Spain ; Terrain models ; Thawing ; Valleys ; Water budget ; Water content ; Water resources</subject><ispartof>Water (Basel), 2019-03, Vol.11 (3), p.506</ispartof><rights>COPYRIGHT 2019 MDPI AG</rights><rights>2019 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/). 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A distributed rainfall model is generated with the specific data recorded by the rain gauges of the catchment during the episode. To describe the process of water routing in the hydrological cycle of the basin, a model is used based on combinations of parallel linear reservoirs (PLR model), distribution by the basin, and tip-out into its drainage network configured using a digital terrain model (DTM). This PLR model allows simulation of the different actual reservoirs of the basin, including the snow and the contribution due to its melting which, in the model, depends on the temperature. The PLR model also allows for a water budget of the episode where, in addition to the effective rainfall contribution, the water that comes from the thaw is taken into account. The PLR model also allows determination of the amount of water that exists in the basin before and after the episode, data of great interest. 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Castillo-Mateo, Jorge ; Sánchez-Navarro, José ; Fuertes-Rodríguez, Víctor ; García-Gil, Alejandro ; Edo-Romero, Vanesa</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c331t-cb90d456d4e8ce5e232bd4ae1fa024b095ae769412bca54add9b71aef1eb90b73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Causes of</topic><topic>Drainage patterns</topic><topic>Environmental aspects</topic><topic>Floods</topic><topic>Gauges</topic><topic>Hydrologic cycle</topic><topic>Hydrology</topic><topic>Investigations</topic><topic>Measurement</topic><topic>Moisture content</topic><topic>Rain and rainfall</topic><topic>Rain gauges</topic><topic>Rainfall</topic><topic>Reservoirs</topic><topic>Snow</topic><topic>Snowmelt</topic><topic>Soil erosion</topic><topic>Spain</topic><topic>Terrain models</topic><topic>Thawing</topic><topic>Valleys</topic><topic>Water budget</topic><topic>Water content</topic><topic>Water resources</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Mateo-Lázaro, Jesús</creatorcontrib><creatorcontrib>Castillo-Mateo, Jorge</creatorcontrib><creatorcontrib>Sánchez-Navarro, José</creatorcontrib><creatorcontrib>Fuertes-Rodríguez, Víctor</creatorcontrib><creatorcontrib>García-Gil, Alejandro</creatorcontrib><creatorcontrib>Edo-Romero, Vanesa</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><jtitle>Water (Basel)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Mateo-Lázaro, Jesús</au><au>Castillo-Mateo, Jorge</au><au>Sánchez-Navarro, José</au><au>Fuertes-Rodríguez, Víctor</au><au>García-Gil, Alejandro</au><au>Edo-Romero, Vanesa</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Assessment of the Role of Snowmelt in a Flood Event in a Gauged Catchment</atitle><jtitle>Water (Basel)</jtitle><date>2019-03-11</date><risdate>2019</risdate><volume>11</volume><issue>3</issue><spage>506</spage><pages>506-</pages><issn>2073-4441</issn><eissn>2073-4441</eissn><abstract>An actual event that happened in the Roncal valley (Spain) is investigated and the results are compared between models with and without snowmelt. A distributed rainfall model is generated with the specific data recorded by the rain gauges of the catchment during the episode. To describe the process of water routing in the hydrological cycle of the basin, a model is used based on combinations of parallel linear reservoirs (PLR model), distribution by the basin, and tip-out into its drainage network configured using a digital terrain model (DTM). This PLR model allows simulation of the different actual reservoirs of the basin, including the snow and the contribution due to its melting which, in the model, depends on the temperature. The PLR model also allows for a water budget of the episode where, in addition to the effective rainfall contribution, the water that comes from the thaw is taken into account. The PLR model also allows determination of the amount of water that exists in the basin before and after the episode, data of great interest. 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| subjects | Causes of Drainage patterns Environmental aspects Floods Gauges Hydrologic cycle Hydrology Investigations Measurement Moisture content Rain and rainfall Rain gauges Rainfall Reservoirs Snow Snowmelt Soil erosion Spain Terrain models Thawing Valleys Water budget Water content Water resources |
| title | Assessment of the Role of Snowmelt in a Flood Event in a Gauged Catchment |
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