Flood Frequency Estimation in Data-Sparse Wainganga Basin, India, Using Continuous Simulation
Monsoon-related extreme flood events are experienced regularly across India, bringing costly damage, disruption and death to local communities. This study provides a route towards estimating the likely magnitude of extreme floods (e.g., the 1-in-100-year flood) at locations without gauged data, help...
Gespeichert in:
Veröffentlicht in: | Water (Basel) 2022-09, Vol.14 (18), p.2887 |
---|---|
Hauptverfasser: | , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | |
---|---|
container_issue | 18 |
container_start_page | 2887 |
container_title | Water (Basel) |
container_volume | 14 |
creator | Vesuviano, Gianni Griffin, Adam Stewart, Elizabeth |
description | Monsoon-related extreme flood events are experienced regularly across India, bringing costly damage, disruption and death to local communities. This study provides a route towards estimating the likely magnitude of extreme floods (e.g., the 1-in-100-year flood) at locations without gauged data, helping engineers to design resilient structures. Gridded rainfall and evapotranspiration estimates were used with a continuous simulation hydrological model to estimate annual maximum flow rates at nine locations corresponding with river flow gauging stations in the Wainganga river basin, a data-sparse region of India. Hosking–Wallis distribution tests were performed to identify the most appropriate distribution to model the annual maxima series, selecting the Generalized Pareto and Pearson Type III distributions. The L-moments and flood frequency curves of the modeled annual maxima were compared to gauged values. The Probability Distributed Model (PDM), properly calibrated to capture the dynamics of peak flows, was shown to be effective in approximating the Generalized Pareto distribution for annual maxima, and may be useful in modeling peak flows in areas with sparse data. Confidence in the model structure, parameterization, input data and catchment representation build confidence in the modeled flood estimates; this is particularly relevant if the method is applied in a location where no gauged flows exist for verification. |
doi_str_mv | 10.3390/w14182887 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2716598787</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2716598787</sourcerecordid><originalsourceid>FETCH-LOGICAL-c222t-54483d02d6e0f8774d08838de7a20fb1cd7ce2052684d521b1bf76dbccb1c4493</originalsourceid><addsrcrecordid>eNpNUE1LAzEQDaJgqT34DwKehK7mazfZo9auFgoeavEkSzbJlpRtUpNdSv-90Yo4DMwM83iP9wC4xuiO0hLdHzDDggjBz8CIIE4zxhg-_7dfgkmMW5SKlULkaAQ-qs57DatgPgfj1BHOY293srfeQevgk-xlttrLEA18l9ZtZGr4KKN1U7hw2sopXKdjA2fe9dYNfohwZXdD90NxBS5a2UUz-Z1jsK7mb7OXbPn6vJg9LDNFCOmznDFBNSK6MKgVnDONhKBCGy4JahusNFeGoJwUgumc4AY3LS90o1T6MVbSMbg58e6DTz5iX2_9EFySrAnHRV4KLnhC3Z5QKvgYg2nrfUhew7HGqP4OsP4LkH4B7lVh0Q</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2716598787</pqid></control><display><type>article</type><title>Flood Frequency Estimation in Data-Sparse Wainganga Basin, India, Using Continuous Simulation</title><source>MDPI - Multidisciplinary Digital Publishing Institute</source><source>EZB-FREE-00999 freely available EZB journals</source><creator>Vesuviano, Gianni ; Griffin, Adam ; Stewart, Elizabeth</creator><creatorcontrib>Vesuviano, Gianni ; Griffin, Adam ; Stewart, Elizabeth</creatorcontrib><description>Monsoon-related extreme flood events are experienced regularly across India, bringing costly damage, disruption and death to local communities. This study provides a route towards estimating the likely magnitude of extreme floods (e.g., the 1-in-100-year flood) at locations without gauged data, helping engineers to design resilient structures. Gridded rainfall and evapotranspiration estimates were used with a continuous simulation hydrological model to estimate annual maximum flow rates at nine locations corresponding with river flow gauging stations in the Wainganga river basin, a data-sparse region of India. Hosking–Wallis distribution tests were performed to identify the most appropriate distribution to model the annual maxima series, selecting the Generalized Pareto and Pearson Type III distributions. The L-moments and flood frequency curves of the modeled annual maxima were compared to gauged values. The Probability Distributed Model (PDM), properly calibrated to capture the dynamics of peak flows, was shown to be effective in approximating the Generalized Pareto distribution for annual maxima, and may be useful in modeling peak flows in areas with sparse data. Confidence in the model structure, parameterization, input data and catchment representation build confidence in the modeled flood estimates; this is particularly relevant if the method is applied in a location where no gauged flows exist for verification.</description><identifier>ISSN: 2073-4441</identifier><identifier>EISSN: 2073-4441</identifier><identifier>DOI: 10.3390/w14182887</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Dams ; Datasets ; Discharge measurement ; Evapotranspiration ; Flood frequency ; Floods ; Flow rates ; Flow velocity ; Gaging stations ; Hydroelectric power ; Hydrologic models ; Hydrology ; Irrigation ; Local communities ; Maxima ; Maximum flow ; Parameterization ; Rainfall ; Regression analysis ; River basins ; River flow ; River networks ; Rivers ; Simulation ; Stream discharge ; Wind</subject><ispartof>Water (Basel), 2022-09, Vol.14 (18), p.2887</ispartof><rights>2022 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 (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c222t-54483d02d6e0f8774d08838de7a20fb1cd7ce2052684d521b1bf76dbccb1c4493</citedby><cites>FETCH-LOGICAL-c222t-54483d02d6e0f8774d08838de7a20fb1cd7ce2052684d521b1bf76dbccb1c4493</cites><orcidid>0000-0003-2157-8875</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27903,27904</link.rule.ids></links><search><creatorcontrib>Vesuviano, Gianni</creatorcontrib><creatorcontrib>Griffin, Adam</creatorcontrib><creatorcontrib>Stewart, Elizabeth</creatorcontrib><title>Flood Frequency Estimation in Data-Sparse Wainganga Basin, India, Using Continuous Simulation</title><title>Water (Basel)</title><description>Monsoon-related extreme flood events are experienced regularly across India, bringing costly damage, disruption and death to local communities. This study provides a route towards estimating the likely magnitude of extreme floods (e.g., the 1-in-100-year flood) at locations without gauged data, helping engineers to design resilient structures. Gridded rainfall and evapotranspiration estimates were used with a continuous simulation hydrological model to estimate annual maximum flow rates at nine locations corresponding with river flow gauging stations in the Wainganga river basin, a data-sparse region of India. Hosking–Wallis distribution tests were performed to identify the most appropriate distribution to model the annual maxima series, selecting the Generalized Pareto and Pearson Type III distributions. The L-moments and flood frequency curves of the modeled annual maxima were compared to gauged values. The Probability Distributed Model (PDM), properly calibrated to capture the dynamics of peak flows, was shown to be effective in approximating the Generalized Pareto distribution for annual maxima, and may be useful in modeling peak flows in areas with sparse data. Confidence in the model structure, parameterization, input data and catchment representation build confidence in the modeled flood estimates; this is particularly relevant if the method is applied in a location where no gauged flows exist for verification.</description><subject>Dams</subject><subject>Datasets</subject><subject>Discharge measurement</subject><subject>Evapotranspiration</subject><subject>Flood frequency</subject><subject>Floods</subject><subject>Flow rates</subject><subject>Flow velocity</subject><subject>Gaging stations</subject><subject>Hydroelectric power</subject><subject>Hydrologic models</subject><subject>Hydrology</subject><subject>Irrigation</subject><subject>Local communities</subject><subject>Maxima</subject><subject>Maximum flow</subject><subject>Parameterization</subject><subject>Rainfall</subject><subject>Regression analysis</subject><subject>River basins</subject><subject>River flow</subject><subject>River networks</subject><subject>Rivers</subject><subject>Simulation</subject><subject>Stream discharge</subject><subject>Wind</subject><issn>2073-4441</issn><issn>2073-4441</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNpNUE1LAzEQDaJgqT34DwKehK7mazfZo9auFgoeavEkSzbJlpRtUpNdSv-90Yo4DMwM83iP9wC4xuiO0hLdHzDDggjBz8CIIE4zxhg-_7dfgkmMW5SKlULkaAQ-qs57DatgPgfj1BHOY293srfeQevgk-xlttrLEA18l9ZtZGr4KKN1U7hw2sopXKdjA2fe9dYNfohwZXdD90NxBS5a2UUz-Z1jsK7mb7OXbPn6vJg9LDNFCOmznDFBNSK6MKgVnDONhKBCGy4JahusNFeGoJwUgumc4AY3LS90o1T6MVbSMbg58e6DTz5iX2_9EFySrAnHRV4KLnhC3Z5QKvgYg2nrfUhew7HGqP4OsP4LkH4B7lVh0Q</recordid><startdate>20220915</startdate><enddate>20220915</enddate><creator>Vesuviano, Gianni</creator><creator>Griffin, Adam</creator><creator>Stewart, Elizabeth</creator><general>MDPI AG</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><orcidid>https://orcid.org/0000-0003-2157-8875</orcidid></search><sort><creationdate>20220915</creationdate><title>Flood Frequency Estimation in Data-Sparse Wainganga Basin, India, Using Continuous Simulation</title><author>Vesuviano, Gianni ; Griffin, Adam ; Stewart, Elizabeth</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c222t-54483d02d6e0f8774d08838de7a20fb1cd7ce2052684d521b1bf76dbccb1c4493</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Dams</topic><topic>Datasets</topic><topic>Discharge measurement</topic><topic>Evapotranspiration</topic><topic>Flood frequency</topic><topic>Floods</topic><topic>Flow rates</topic><topic>Flow velocity</topic><topic>Gaging stations</topic><topic>Hydroelectric power</topic><topic>Hydrologic models</topic><topic>Hydrology</topic><topic>Irrigation</topic><topic>Local communities</topic><topic>Maxima</topic><topic>Maximum flow</topic><topic>Parameterization</topic><topic>Rainfall</topic><topic>Regression analysis</topic><topic>River basins</topic><topic>River flow</topic><topic>River networks</topic><topic>Rivers</topic><topic>Simulation</topic><topic>Stream discharge</topic><topic>Wind</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Vesuviano, Gianni</creatorcontrib><creatorcontrib>Griffin, Adam</creatorcontrib><creatorcontrib>Stewart, Elizabeth</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>Vesuviano, Gianni</au><au>Griffin, Adam</au><au>Stewart, Elizabeth</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Flood Frequency Estimation in Data-Sparse Wainganga Basin, India, Using Continuous Simulation</atitle><jtitle>Water (Basel)</jtitle><date>2022-09-15</date><risdate>2022</risdate><volume>14</volume><issue>18</issue><spage>2887</spage><pages>2887-</pages><issn>2073-4441</issn><eissn>2073-4441</eissn><abstract>Monsoon-related extreme flood events are experienced regularly across India, bringing costly damage, disruption and death to local communities. This study provides a route towards estimating the likely magnitude of extreme floods (e.g., the 1-in-100-year flood) at locations without gauged data, helping engineers to design resilient structures. Gridded rainfall and evapotranspiration estimates were used with a continuous simulation hydrological model to estimate annual maximum flow rates at nine locations corresponding with river flow gauging stations in the Wainganga river basin, a data-sparse region of India. Hosking–Wallis distribution tests were performed to identify the most appropriate distribution to model the annual maxima series, selecting the Generalized Pareto and Pearson Type III distributions. The L-moments and flood frequency curves of the modeled annual maxima were compared to gauged values. The Probability Distributed Model (PDM), properly calibrated to capture the dynamics of peak flows, was shown to be effective in approximating the Generalized Pareto distribution for annual maxima, and may be useful in modeling peak flows in areas with sparse data. Confidence in the model structure, parameterization, input data and catchment representation build confidence in the modeled flood estimates; this is particularly relevant if the method is applied in a location where no gauged flows exist for verification.</abstract><cop>Basel</cop><pub>MDPI AG</pub><doi>10.3390/w14182887</doi><orcidid>https://orcid.org/0000-0003-2157-8875</orcidid><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 2073-4441 |
ispartof | Water (Basel), 2022-09, Vol.14 (18), p.2887 |
issn | 2073-4441 2073-4441 |
language | eng |
recordid | cdi_proquest_journals_2716598787 |
source | MDPI - Multidisciplinary Digital Publishing Institute; EZB-FREE-00999 freely available EZB journals |
subjects | Dams Datasets Discharge measurement Evapotranspiration Flood frequency Floods Flow rates Flow velocity Gaging stations Hydroelectric power Hydrologic models Hydrology Irrigation Local communities Maxima Maximum flow Parameterization Rainfall Regression analysis River basins River flow River networks Rivers Simulation Stream discharge Wind |
title | Flood Frequency Estimation in Data-Sparse Wainganga Basin, India, Using Continuous Simulation |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-27T14%3A45%3A45IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Flood%20Frequency%20Estimation%20in%20Data-Sparse%20Wainganga%20Basin,%20India,%20Using%20Continuous%20Simulation&rft.jtitle=Water%20(Basel)&rft.au=Vesuviano,%20Gianni&rft.date=2022-09-15&rft.volume=14&rft.issue=18&rft.spage=2887&rft.pages=2887-&rft.issn=2073-4441&rft.eissn=2073-4441&rft_id=info:doi/10.3390/w14182887&rft_dat=%3Cproquest_cross%3E2716598787%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2716598787&rft_id=info:pmid/&rfr_iscdi=true |