Flood forecast and flood vulnerability modeling in case of Wadi Fez, Morocco
The Wadi Fez basin, part of the Great Sebou Basin in northern Morocco, is located in the North part of the Tabular Middle Atlas and the central part of the Saïs plain. Its physiographic and morphological study contributes to a better knowledge of its functioning. It allows proposing solutions to the...
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Veröffentlicht in: | Arabian journal of geosciences 2022-03, Vol.15 (6), Article 525 |
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description | The Wadi Fez basin, part of the Great Sebou Basin in northern Morocco, is located in the North part of the Tabular Middle Atlas and the central part of the Saïs plain. Its physiographic and morphological study contributes to a better knowledge of its functioning. It allows proposing solutions to the decision makers for better socio-economic management of the region. We conduct our research based on the hydrological regime, the analysis of extreme flows frequency, the volume of precipitation, the concentration time, and the return periods of floods. Our results have determined that the Wadi Fez basin is rainy and sometimes torrential in winter, often generating floods in Fez and its surroundings. Moreover, the parameters of the substrate induce a large volume of water resources from upstream. However, the weak structure of the Wadi Fez hydrographic network and the water balance has highlighted a considerable loss of water resources, which handicaps the irrigation system of the vegetables and plantations of the basin. Furthermore, the hydrological modeling of the Wadi Fez basin by the HEC-HMS platform and the use of the HEC-RAS software have allowed the definition of the flood vulnerable areas and thus a better understanding of the one and two-dimensional modeling peak flow. Finally, the annual modulus and the different coefficients show hydroclimatic fluctuations of semi-arid climatic conditions, with a temperate winter and a hot summer. Therefore, our results suggest that it is necessary to decrease the infiltration/flooding ratio. For this reason, we recommend monitoring water runoff, protecting surface soils from flooding and active erosion by planting trees, and installing dikes and small dams to recharge groundwater in this basin. |
doi_str_mv | 10.1007/s12517-022-09760-6 |
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Its physiographic and morphological study contributes to a better knowledge of its functioning. It allows proposing solutions to the decision makers for better socio-economic management of the region. We conduct our research based on the hydrological regime, the analysis of extreme flows frequency, the volume of precipitation, the concentration time, and the return periods of floods. Our results have determined that the Wadi Fez basin is rainy and sometimes torrential in winter, often generating floods in Fez and its surroundings. Moreover, the parameters of the substrate induce a large volume of water resources from upstream. However, the weak structure of the Wadi Fez hydrographic network and the water balance has highlighted a considerable loss of water resources, which handicaps the irrigation system of the vegetables and plantations of the basin. Furthermore, the hydrological modeling of the Wadi Fez basin by the HEC-HMS platform and the use of the HEC-RAS software have allowed the definition of the flood vulnerable areas and thus a better understanding of the one and two-dimensional modeling peak flow. Finally, the annual modulus and the different coefficients show hydroclimatic fluctuations of semi-arid climatic conditions, with a temperate winter and a hot summer. Therefore, our results suggest that it is necessary to decrease the infiltration/flooding ratio. For this reason, we recommend monitoring water runoff, protecting surface soils from flooding and active erosion by planting trees, and installing dikes and small dams to recharge groundwater in this basin.</description><identifier>ISSN: 1866-7511</identifier><identifier>EISSN: 1866-7538</identifier><identifier>DOI: 10.1007/s12517-022-09760-6</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Aridity ; Climatic conditions ; Coefficients ; Concentration time ; Dikes ; Earth and Environmental Science ; Earth science ; Earth Sciences ; Economics ; Embankments ; Flood forecasting ; Flooding ; Floods ; Groundwater ; Groundwater basins ; Groundwater recharge ; Hydrologic regime ; Hydrology ; Irrigation systems ; Modelling ; Original Paper ; Rainfall ; Recharge dams ; Runoff ; Socioeconomic aspects ; Soil ; Soil erosion ; Soil surfaces ; Soil water ; Substrates ; Surface runoff ; Two dimensional flow ; Two dimensional models ; Vulnerability ; Water balance ; Water resources ; Winter</subject><ispartof>Arabian journal of geosciences, 2022-03, Vol.15 (6), Article 525</ispartof><rights>Saudi Society for Geosciences 2022</rights><rights>Saudi Society for Geosciences 2022.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2004-1f30975c7c3a152ffe845d6583bcb351f28c9f19edec19afb7b4976062940b713</citedby><cites>FETCH-LOGICAL-c2004-1f30975c7c3a152ffe845d6583bcb351f28c9f19edec19afb7b4976062940b713</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12517-022-09760-6$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12517-022-09760-6$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,778,782,27907,27908,41471,42540,51302</link.rule.ids></links><search><creatorcontrib>El Fathi, Badr</creatorcontrib><creatorcontrib>El Hassani, Farah</creatorcontrib><creatorcontrib>Moukhliss, Mohammed</creatorcontrib><creatorcontrib>Mazigh, Nouhaila</creatorcontrib><creatorcontrib>Dra, Abdelaziz</creatorcontrib><creatorcontrib>Ouallali, Abdessalam</creatorcontrib><creatorcontrib>Kherbeche, Abdelhak</creatorcontrib><creatorcontrib>Taleb, Abdeslam</creatorcontrib><title>Flood forecast and flood vulnerability modeling in case of Wadi Fez, Morocco</title><title>Arabian journal of geosciences</title><addtitle>Arab J Geosci</addtitle><description>The Wadi Fez basin, part of the Great Sebou Basin in northern Morocco, is located in the North part of the Tabular Middle Atlas and the central part of the Saïs plain. Its physiographic and morphological study contributes to a better knowledge of its functioning. It allows proposing solutions to the decision makers for better socio-economic management of the region. We conduct our research based on the hydrological regime, the analysis of extreme flows frequency, the volume of precipitation, the concentration time, and the return periods of floods. Our results have determined that the Wadi Fez basin is rainy and sometimes torrential in winter, often generating floods in Fez and its surroundings. Moreover, the parameters of the substrate induce a large volume of water resources from upstream. However, the weak structure of the Wadi Fez hydrographic network and the water balance has highlighted a considerable loss of water resources, which handicaps the irrigation system of the vegetables and plantations of the basin. Furthermore, the hydrological modeling of the Wadi Fez basin by the HEC-HMS platform and the use of the HEC-RAS software have allowed the definition of the flood vulnerable areas and thus a better understanding of the one and two-dimensional modeling peak flow. Finally, the annual modulus and the different coefficients show hydroclimatic fluctuations of semi-arid climatic conditions, with a temperate winter and a hot summer. Therefore, our results suggest that it is necessary to decrease the infiltration/flooding ratio. For this reason, we recommend monitoring water runoff, protecting surface soils from flooding and active erosion by planting trees, and installing dikes and small dams to recharge groundwater in this basin.</description><subject>Aridity</subject><subject>Climatic conditions</subject><subject>Coefficients</subject><subject>Concentration time</subject><subject>Dikes</subject><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Economics</subject><subject>Embankments</subject><subject>Flood forecasting</subject><subject>Flooding</subject><subject>Floods</subject><subject>Groundwater</subject><subject>Groundwater basins</subject><subject>Groundwater recharge</subject><subject>Hydrologic regime</subject><subject>Hydrology</subject><subject>Irrigation systems</subject><subject>Modelling</subject><subject>Original Paper</subject><subject>Rainfall</subject><subject>Recharge dams</subject><subject>Runoff</subject><subject>Socioeconomic aspects</subject><subject>Soil</subject><subject>Soil erosion</subject><subject>Soil surfaces</subject><subject>Soil water</subject><subject>Substrates</subject><subject>Surface runoff</subject><subject>Two dimensional flow</subject><subject>Two dimensional models</subject><subject>Vulnerability</subject><subject>Water balance</subject><subject>Water resources</subject><subject>Winter</subject><issn>1866-7511</issn><issn>1866-7538</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp9UE1LAzEQDaJgrf4BTwGvRjPJbpI9SrEqVLwoHkM2m5Qt201NukL99aZd0ZuHYT54783MQ-gS6A1QKm8TsBIkoYwRWklBiThCE1BCEFlydfxbA5yis5RWlApFpZqgxbwLocE-RGdN2mLT5-Yw-hy63kVTt1273eF1aFzX9kvc9jgDHQ4ev5umxXP3dY2fQwzWhnN04k2X3MVPnqK3-f3r7JEsXh6eZncLYhmlBQHP85GllZYbKJn3ThVlI0rFa1vzEjxTtvJQucZZqIyvZV3snxKsKmgtgU_R1ai7ieFjcGmrV2GIfV6pmeCqqDjkmCI2omwMKUXn9Sa2axN3Gqjeu6ZH13R2TR9c0yKT-EhKGdwvXfyT_of1DQbGbmY</recordid><startdate>20220301</startdate><enddate>20220301</enddate><creator>El Fathi, Badr</creator><creator>El Hassani, Farah</creator><creator>Moukhliss, Mohammed</creator><creator>Mazigh, Nouhaila</creator><creator>Dra, Abdelaziz</creator><creator>Ouallali, Abdessalam</creator><creator>Kherbeche, Abdelhak</creator><creator>Taleb, Abdeslam</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20220301</creationdate><title>Flood forecast and flood vulnerability modeling in case of Wadi Fez, Morocco</title><author>El Fathi, Badr ; El Hassani, Farah ; Moukhliss, Mohammed ; Mazigh, Nouhaila ; Dra, Abdelaziz ; Ouallali, Abdessalam ; Kherbeche, Abdelhak ; Taleb, Abdeslam</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2004-1f30975c7c3a152ffe845d6583bcb351f28c9f19edec19afb7b4976062940b713</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Aridity</topic><topic>Climatic conditions</topic><topic>Coefficients</topic><topic>Concentration time</topic><topic>Dikes</topic><topic>Earth and Environmental Science</topic><topic>Earth science</topic><topic>Earth Sciences</topic><topic>Economics</topic><topic>Embankments</topic><topic>Flood forecasting</topic><topic>Flooding</topic><topic>Floods</topic><topic>Groundwater</topic><topic>Groundwater basins</topic><topic>Groundwater recharge</topic><topic>Hydrologic regime</topic><topic>Hydrology</topic><topic>Irrigation systems</topic><topic>Modelling</topic><topic>Original Paper</topic><topic>Rainfall</topic><topic>Recharge dams</topic><topic>Runoff</topic><topic>Socioeconomic aspects</topic><topic>Soil</topic><topic>Soil erosion</topic><topic>Soil surfaces</topic><topic>Soil water</topic><topic>Substrates</topic><topic>Surface runoff</topic><topic>Two dimensional flow</topic><topic>Two dimensional models</topic><topic>Vulnerability</topic><topic>Water balance</topic><topic>Water resources</topic><topic>Winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>El Fathi, Badr</creatorcontrib><creatorcontrib>El Hassani, Farah</creatorcontrib><creatorcontrib>Moukhliss, Mohammed</creatorcontrib><creatorcontrib>Mazigh, Nouhaila</creatorcontrib><creatorcontrib>Dra, Abdelaziz</creatorcontrib><creatorcontrib>Ouallali, Abdessalam</creatorcontrib><creatorcontrib>Kherbeche, Abdelhak</creatorcontrib><creatorcontrib>Taleb, Abdeslam</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Arabian journal of geosciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>El Fathi, Badr</au><au>El Hassani, Farah</au><au>Moukhliss, Mohammed</au><au>Mazigh, Nouhaila</au><au>Dra, Abdelaziz</au><au>Ouallali, Abdessalam</au><au>Kherbeche, Abdelhak</au><au>Taleb, Abdeslam</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Flood forecast and flood vulnerability modeling in case of Wadi Fez, Morocco</atitle><jtitle>Arabian journal of geosciences</jtitle><stitle>Arab J Geosci</stitle><date>2022-03-01</date><risdate>2022</risdate><volume>15</volume><issue>6</issue><artnum>525</artnum><issn>1866-7511</issn><eissn>1866-7538</eissn><abstract>The Wadi Fez basin, part of the Great Sebou Basin in northern Morocco, is located in the North part of the Tabular Middle Atlas and the central part of the Saïs plain. Its physiographic and morphological study contributes to a better knowledge of its functioning. It allows proposing solutions to the decision makers for better socio-economic management of the region. We conduct our research based on the hydrological regime, the analysis of extreme flows frequency, the volume of precipitation, the concentration time, and the return periods of floods. Our results have determined that the Wadi Fez basin is rainy and sometimes torrential in winter, often generating floods in Fez and its surroundings. Moreover, the parameters of the substrate induce a large volume of water resources from upstream. However, the weak structure of the Wadi Fez hydrographic network and the water balance has highlighted a considerable loss of water resources, which handicaps the irrigation system of the vegetables and plantations of the basin. Furthermore, the hydrological modeling of the Wadi Fez basin by the HEC-HMS platform and the use of the HEC-RAS software have allowed the definition of the flood vulnerable areas and thus a better understanding of the one and two-dimensional modeling peak flow. Finally, the annual modulus and the different coefficients show hydroclimatic fluctuations of semi-arid climatic conditions, with a temperate winter and a hot summer. Therefore, our results suggest that it is necessary to decrease the infiltration/flooding ratio. For this reason, we recommend monitoring water runoff, protecting surface soils from flooding and active erosion by planting trees, and installing dikes and small dams to recharge groundwater in this basin.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s12517-022-09760-6</doi></addata></record> |
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subjects | Aridity Climatic conditions Coefficients Concentration time Dikes Earth and Environmental Science Earth science Earth Sciences Economics Embankments Flood forecasting Flooding Floods Groundwater Groundwater basins Groundwater recharge Hydrologic regime Hydrology Irrigation systems Modelling Original Paper Rainfall Recharge dams Runoff Socioeconomic aspects Soil Soil erosion Soil surfaces Soil water Substrates Surface runoff Two dimensional flow Two dimensional models Vulnerability Water balance Water resources Winter |
title | Flood forecast and flood vulnerability modeling in case of Wadi Fez, Morocco |
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