Temporal continuity of extreme precipitation events using sub‐daily precipitation: application to floods in the Ebro basin, northeastern Spain
ABSTRACT Extreme precipitation events have been studied widely in various regions because of their implications for hazard assessment and risk management, particularly those of a hydrologic nature. Extreme precipitation events have been commonly defined using daily precipitation series owing to a la...
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Veröffentlicht in: | International journal of climatology 2018-03, Vol.38 (4), p.1877-1892 |
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creator | Merino, A. Fernández‐González, S. García‐Ortega, E. Sánchez, J. L. López, L. Gascón, E. |
description | ABSTRACT
Extreme precipitation events have been studied widely in various regions because of their implications for hazard assessment and risk management, particularly those of a hydrologic nature. Extreme precipitation events have been commonly defined using daily precipitation series owing to a lack of long‐term data at higher temporal resolution. However, because of their potentially dramatic consequences, intense sub‐daily precipitation is of great importance for risk assessment. Here, we define a new concept of extreme precipitation event based on temporal continuity of that event through run analysis using hourly precipitation. The aim of this definition is to record intense precipitation events over a very short period as well as very persistent rainfall events that produce heavy accumulated precipitation over several days. Both types of event can present considerable hydrologic hazards and are not considered in the definition of extreme precipitation event that is based on a daily time scale. We applied this method to the 29 greatest flood events in the Ebro River basin during 2000–2014 to determine whether our definition can be used to identify events producing hydrologic risks. In addition, we compared the synoptic patterns and trends of events defined using this method and those based on a daily time scale. The results show that the new definition allowed for identification of the 29 analysed flood events (as opposed to extreme events based on a daily time scale), among which eight events were not identified. Moreover, using the new definition facilitates establishment of synoptic patterns and more detailed study of trends by discriminating events according to their duration. The results reveal how the use of daily precipitation can hide trends of shorter events, because positive trends are more dominant in extreme precipitation events at sub‐daily scale.
The extreme precipitation events have been commonly defined using daily precipitation series owing to a lack of long‐term data at high temporal resolution. However, because of their potentially dramatic consequences, intense sub‐daily precipitation is of great importance for risk assessment. We define a new concept of extreme precipitation event based on temporal continuity of the event through run analysis by using hourly precipitation. The method was applied over the 29 greatest flood events in the Ebro River basin. |
doi_str_mv | 10.1002/joc.5302 |
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Extreme precipitation events have been studied widely in various regions because of their implications for hazard assessment and risk management, particularly those of a hydrologic nature. Extreme precipitation events have been commonly defined using daily precipitation series owing to a lack of long‐term data at higher temporal resolution. However, because of their potentially dramatic consequences, intense sub‐daily precipitation is of great importance for risk assessment. Here, we define a new concept of extreme precipitation event based on temporal continuity of that event through run analysis using hourly precipitation. The aim of this definition is to record intense precipitation events over a very short period as well as very persistent rainfall events that produce heavy accumulated precipitation over several days. Both types of event can present considerable hydrologic hazards and are not considered in the definition of extreme precipitation event that is based on a daily time scale. We applied this method to the 29 greatest flood events in the Ebro River basin during 2000–2014 to determine whether our definition can be used to identify events producing hydrologic risks. In addition, we compared the synoptic patterns and trends of events defined using this method and those based on a daily time scale. The results show that the new definition allowed for identification of the 29 analysed flood events (as opposed to extreme events based on a daily time scale), among which eight events were not identified. Moreover, using the new definition facilitates establishment of synoptic patterns and more detailed study of trends by discriminating events according to their duration. The results reveal how the use of daily precipitation can hide trends of shorter events, because positive trends are more dominant in extreme precipitation events at sub‐daily scale.
The extreme precipitation events have been commonly defined using daily precipitation series owing to a lack of long‐term data at high temporal resolution. However, because of their potentially dramatic consequences, intense sub‐daily precipitation is of great importance for risk assessment. We define a new concept of extreme precipitation event based on temporal continuity of the event through run analysis by using hourly precipitation. The method was applied over the 29 greatest flood events in the Ebro River basin.</description><identifier>ISSN: 0899-8418</identifier><identifier>EISSN: 1097-0088</identifier><identifier>DOI: 10.1002/joc.5302</identifier><language>eng</language><publisher>Chichester, UK: John Wiley & Sons, Ltd</publisher><subject>Atmospheric precipitations ; Continuity ; Daily ; Daily precipitation ; Data processing ; Duration ; Ebro basin ; extreme precipitation ; Extreme weather ; Floods ; Geographical variations ; Hazard assessment ; Hazards ; Hydrologic data ; Hydrology ; Methods ; Precipitation ; Rain ; Rainfall ; Risk assessment ; Risk management ; River basins ; Rivers ; Spain ; synoptic patterns ; Temporal resolution ; Time ; trend ; Trends</subject><ispartof>International journal of climatology, 2018-03, Vol.38 (4), p.1877-1892</ispartof><rights>2017 Royal Meteorological Society</rights><rights>2018 Royal Meteorological Society</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2932-e4e597801f8cd58f4c6b59e3f26e48973aab8458626983d2453086ac78b8736f3</citedby><cites>FETCH-LOGICAL-c2932-e4e597801f8cd58f4c6b59e3f26e48973aab8458626983d2453086ac78b8736f3</cites><orcidid>0000-0002-1025-4093 ; 0000-0001-8806-6263</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fjoc.5302$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fjoc.5302$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>315,781,785,1418,27929,27930,45579,45580</link.rule.ids></links><search><creatorcontrib>Merino, A.</creatorcontrib><creatorcontrib>Fernández‐González, S.</creatorcontrib><creatorcontrib>García‐Ortega, E.</creatorcontrib><creatorcontrib>Sánchez, J. L.</creatorcontrib><creatorcontrib>López, L.</creatorcontrib><creatorcontrib>Gascón, E.</creatorcontrib><title>Temporal continuity of extreme precipitation events using sub‐daily precipitation: application to floods in the Ebro basin, northeastern Spain</title><title>International journal of climatology</title><description>ABSTRACT
Extreme precipitation events have been studied widely in various regions because of their implications for hazard assessment and risk management, particularly those of a hydrologic nature. Extreme precipitation events have been commonly defined using daily precipitation series owing to a lack of long‐term data at higher temporal resolution. However, because of their potentially dramatic consequences, intense sub‐daily precipitation is of great importance for risk assessment. Here, we define a new concept of extreme precipitation event based on temporal continuity of that event through run analysis using hourly precipitation. The aim of this definition is to record intense precipitation events over a very short period as well as very persistent rainfall events that produce heavy accumulated precipitation over several days. Both types of event can present considerable hydrologic hazards and are not considered in the definition of extreme precipitation event that is based on a daily time scale. We applied this method to the 29 greatest flood events in the Ebro River basin during 2000–2014 to determine whether our definition can be used to identify events producing hydrologic risks. In addition, we compared the synoptic patterns and trends of events defined using this method and those based on a daily time scale. The results show that the new definition allowed for identification of the 29 analysed flood events (as opposed to extreme events based on a daily time scale), among which eight events were not identified. Moreover, using the new definition facilitates establishment of synoptic patterns and more detailed study of trends by discriminating events according to their duration. The results reveal how the use of daily precipitation can hide trends of shorter events, because positive trends are more dominant in extreme precipitation events at sub‐daily scale.
The extreme precipitation events have been commonly defined using daily precipitation series owing to a lack of long‐term data at high temporal resolution. However, because of their potentially dramatic consequences, intense sub‐daily precipitation is of great importance for risk assessment. We define a new concept of extreme precipitation event based on temporal continuity of the event through run analysis by using hourly precipitation. The method was applied over the 29 greatest flood events in the Ebro River basin.</description><subject>Atmospheric precipitations</subject><subject>Continuity</subject><subject>Daily</subject><subject>Daily precipitation</subject><subject>Data processing</subject><subject>Duration</subject><subject>Ebro basin</subject><subject>extreme precipitation</subject><subject>Extreme weather</subject><subject>Floods</subject><subject>Geographical variations</subject><subject>Hazard assessment</subject><subject>Hazards</subject><subject>Hydrologic data</subject><subject>Hydrology</subject><subject>Methods</subject><subject>Precipitation</subject><subject>Rain</subject><subject>Rainfall</subject><subject>Risk assessment</subject><subject>Risk management</subject><subject>River basins</subject><subject>Rivers</subject><subject>Spain</subject><subject>synoptic patterns</subject><subject>Temporal resolution</subject><subject>Time</subject><subject>trend</subject><subject>Trends</subject><issn>0899-8418</issn><issn>1097-0088</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><recordid>eNp1kMtOwzAQRS0EEqUg8QmW2LAgxY7zsNmhqrxUqQvKOnKcCbhK7WA7QHZ8Qr-RLyGlbFiwGs3o3DvSQeiUkgklJL5cWTVJGYn30IgSkUeEcL6PRoQLEfGE8kN05P2KECIEzUZos4R1a51ssLImaNPp0GNbY_gIDtaAWwdKtzrIoK3B8AYmeNx5bZ6x78qvz00lddP_xa6wbNtGq10mWFw31lYe62F5ATwrncWlHDousLFuOEkfwBn82EptjtFBLRsPJ79zjJ5uZsvpXTRf3N5Pr-eRigWLI0ggFTkntOaqSnmdqKxMBbA6ziDhImdSljxJeRZngrMqTgYnPJMq5yXPWVazMTrb9bbOvnbgQ7GynTPDyyImlAomGEsG6nxHKWe9d1AXrdNr6fqCkmLre0ipYut7QKMd-q4b6P_liofF9If_Bg96hKc</recordid><startdate>20180330</startdate><enddate>20180330</enddate><creator>Merino, A.</creator><creator>Fernández‐González, S.</creator><creator>García‐Ortega, E.</creator><creator>Sánchez, J. L.</creator><creator>López, L.</creator><creator>Gascón, E.</creator><general>John Wiley & Sons, Ltd</general><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0002-1025-4093</orcidid><orcidid>https://orcid.org/0000-0001-8806-6263</orcidid></search><sort><creationdate>20180330</creationdate><title>Temporal continuity of extreme precipitation events using sub‐daily precipitation: application to floods in the Ebro basin, northeastern Spain</title><author>Merino, A. ; Fernández‐González, S. ; García‐Ortega, E. ; Sánchez, J. L. ; López, L. ; Gascón, E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2932-e4e597801f8cd58f4c6b59e3f26e48973aab8458626983d2453086ac78b8736f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Atmospheric precipitations</topic><topic>Continuity</topic><topic>Daily</topic><topic>Daily precipitation</topic><topic>Data processing</topic><topic>Duration</topic><topic>Ebro basin</topic><topic>extreme precipitation</topic><topic>Extreme weather</topic><topic>Floods</topic><topic>Geographical variations</topic><topic>Hazard assessment</topic><topic>Hazards</topic><topic>Hydrologic data</topic><topic>Hydrology</topic><topic>Methods</topic><topic>Precipitation</topic><topic>Rain</topic><topic>Rainfall</topic><topic>Risk assessment</topic><topic>Risk management</topic><topic>River basins</topic><topic>Rivers</topic><topic>Spain</topic><topic>synoptic patterns</topic><topic>Temporal resolution</topic><topic>Time</topic><topic>trend</topic><topic>Trends</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Merino, A.</creatorcontrib><creatorcontrib>Fernández‐González, S.</creatorcontrib><creatorcontrib>García‐Ortega, E.</creatorcontrib><creatorcontrib>Sánchez, J. L.</creatorcontrib><creatorcontrib>López, L.</creatorcontrib><creatorcontrib>Gascón, E.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>International journal of climatology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Merino, A.</au><au>Fernández‐González, S.</au><au>García‐Ortega, E.</au><au>Sánchez, J. L.</au><au>López, L.</au><au>Gascón, E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Temporal continuity of extreme precipitation events using sub‐daily precipitation: application to floods in the Ebro basin, northeastern Spain</atitle><jtitle>International journal of climatology</jtitle><date>2018-03-30</date><risdate>2018</risdate><volume>38</volume><issue>4</issue><spage>1877</spage><epage>1892</epage><pages>1877-1892</pages><issn>0899-8418</issn><eissn>1097-0088</eissn><abstract>ABSTRACT
Extreme precipitation events have been studied widely in various regions because of their implications for hazard assessment and risk management, particularly those of a hydrologic nature. Extreme precipitation events have been commonly defined using daily precipitation series owing to a lack of long‐term data at higher temporal resolution. However, because of their potentially dramatic consequences, intense sub‐daily precipitation is of great importance for risk assessment. Here, we define a new concept of extreme precipitation event based on temporal continuity of that event through run analysis using hourly precipitation. The aim of this definition is to record intense precipitation events over a very short period as well as very persistent rainfall events that produce heavy accumulated precipitation over several days. Both types of event can present considerable hydrologic hazards and are not considered in the definition of extreme precipitation event that is based on a daily time scale. We applied this method to the 29 greatest flood events in the Ebro River basin during 2000–2014 to determine whether our definition can be used to identify events producing hydrologic risks. In addition, we compared the synoptic patterns and trends of events defined using this method and those based on a daily time scale. The results show that the new definition allowed for identification of the 29 analysed flood events (as opposed to extreme events based on a daily time scale), among which eight events were not identified. Moreover, using the new definition facilitates establishment of synoptic patterns and more detailed study of trends by discriminating events according to their duration. The results reveal how the use of daily precipitation can hide trends of shorter events, because positive trends are more dominant in extreme precipitation events at sub‐daily scale.
The extreme precipitation events have been commonly defined using daily precipitation series owing to a lack of long‐term data at high temporal resolution. However, because of their potentially dramatic consequences, intense sub‐daily precipitation is of great importance for risk assessment. We define a new concept of extreme precipitation event based on temporal continuity of the event through run analysis by using hourly precipitation. The method was applied over the 29 greatest flood events in the Ebro River basin.</abstract><cop>Chichester, UK</cop><pub>John Wiley & Sons, Ltd</pub><doi>10.1002/joc.5302</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0002-1025-4093</orcidid><orcidid>https://orcid.org/0000-0001-8806-6263</orcidid></addata></record> |
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subjects | Atmospheric precipitations Continuity Daily Daily precipitation Data processing Duration Ebro basin extreme precipitation Extreme weather Floods Geographical variations Hazard assessment Hazards Hydrologic data Hydrology Methods Precipitation Rain Rainfall Risk assessment Risk management River basins Rivers Spain synoptic patterns Temporal resolution Time trend Trends |
title | Temporal continuity of extreme precipitation events using sub‐daily precipitation: application to floods in the Ebro basin, northeastern Spain |
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