FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1996014677> ?p ?o ?g. }

• W1996014677 endingPage "246" @default.
• W1996014677 startingPage "233" @default.
• W1996014677 abstract "CR Climate Research Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsSpecials CR 23:233-246 (2003) - doi:10.3354/cr023233 Assessing future discharge of the river Rhine using regional climate model integrations and a hydrological model M. V. Shabalova1, W. P. A. van Deursen2, T. A. Buishand1,* 1Royal Netherlands Meteorological Institute (KNMI), PO Box 201, 3730 AE De Bilt, The Netherlands 2Carthago Consultancy, Oostzeedijk Beneden 23a, 3062 VK Rotterdam, The Netherlands *Corresponding author. Email: adri.buishand@knmi.nl ABSTRACT: Climate change scenarios based on integrations of the Hadley Centre regional climate model HadRM2 are used to determine the change in the flow regime of the river Rhine by the end of the 21st century. Two scenarios are formulated: Scenario 1 accounting for the temperature increase (4.8°C on average over the basin) and changes in the mean precipitation, and Scenario 2 accounting additionally for changes in the temperature variance and an increase in the relative variability of precipitation. These scenarios are used as input into the RhineFlow hydrological model, a distributed water balance model of the Rhine basin that simulates river flow, soil moisture, snow pack and groundwater storage with a 10 d time step. Both scenarios result in higher mean discharges of the Rhine in winter (approx. +30%), but lower mean discharges in summer (approx. -30%), particularly in August (approx. -50%). RhineFlow simulations also indicate that the variability of the 10 d discharges increases significantly, even if the variability of the climatic inputs remains unchanged. The annual maximum discharge increases in magnitude throughout the Rhine and tends to occur more frequently in winter, thus suggesting an increasing risk of winter floods. This is especially pronounced in Scenario 2. At the Netherlands-German border, the magnitude of the 20 yr maximum discharge event increases by 14% in Scenario 1 and by 29% in Scenario 2; the present-day 20 yr event tends to reappear every 5 yr in Scenario 1 and every 3 yr in Scenario 2. The frequency of occurrence of low and very low flows increases, in both scenarios alike. KEY WORDS: Climate change impact · Regional climate model · Climate change scenarios · Rhine discharge · Extreme river flows Full text in pdf format PreviousNextExport citation RSS - Facebook - Tweet - linkedIn Cited by Published in CR Vol. 23, No. 3. Online publication date: April 10, 2003 Print ISSN: 0936-577X; Online ISSN: 1616-1572 Copyright © 2003 Inter-Research." @default.
• W1996014677 created "2016-06-24" @default.
• W1996014677 creator A5012529906 @default.
• W1996014677 creator A5065164080 @default.
• W1996014677 creator A5080469345 @default.
• W1996014677 date "2003-01-01" @default.
• W1996014677 modified "2023-10-17" @default.
• W1996014677 title "Assessing future discharge of the river Rhine using regional climate model integrations and a hydrological model" @default.
• W1996014677 cites W1591303585 @default.
• W1996014677 cites W1673176785 @default.
• W1996014677 cites W1968892883 @default.
• W1996014677 cites W1970812648 @default.
• W1996014677 cites W2023356830 @default.
• W1996014677 cites W2025441790 @default.
• W1996014677 cites W2033193876 @default.
• W1996014677 cites W2033904036 @default.
• W1996014677 cites W2033929895 @default.
• W1996014677 cites W2042332886 @default.
• W1996014677 cites W2047015815 @default.
• W1996014677 cites W2060831095 @default.
• W1996014677 cites W2077623746 @default.
• W1996014677 cites W2093659305 @default.
• W1996014677 cites W2122513430 @default.
• W1996014677 cites W2172951971 @default.
• W1996014677 cites W566195703 @default.
• W1996014677 cites W85630790 @default.
• W1996014677 doi "https://doi.org/10.3354/cr023233" @default.
• W1996014677 hasPublicationYear "2003" @default.
• W1996014677 type Work @default.
• W1996014677 sameAs 1996014677 @default.
• W1996014677 citedByCount "152" @default.
• W1996014677 countsByYear W19960146772012 @default.
• W1996014677 countsByYear W19960146772013 @default.
• W1996014677 countsByYear W19960146772014 @default.
• W1996014677 countsByYear W19960146772015 @default.
• W1996014677 countsByYear W19960146772016 @default.
• W1996014677 countsByYear W19960146772017 @default.
• W1996014677 countsByYear W19960146772018 @default.
• W1996014677 countsByYear W19960146772019 @default.
• W1996014677 countsByYear W19960146772020 @default.
• W1996014677 countsByYear W19960146772021 @default.
• W1996014677 countsByYear W19960146772022 @default.
• W1996014677 countsByYear W19960146772023 @default.
• W1996014677 crossrefType "journal-article" @default.
• W1996014677 hasAuthorship W1996014677A5012529906 @default.
• W1996014677 hasAuthorship W1996014677A5065164080 @default.
• W1996014677 hasAuthorship W1996014677A5080469345 @default.
• W1996014677 hasBestOaLocation W19960146771 @default.
• W1996014677 hasConcept C107054158 @default.
• W1996014677 hasConcept C111368507 @default.
• W1996014677 hasConcept C126197015 @default.
• W1996014677 hasConcept C126645576 @default.
• W1996014677 hasConcept C127313418 @default.
• W1996014677 hasConcept C132651083 @default.
• W1996014677 hasConcept C153294291 @default.
• W1996014677 hasConcept C168754636 @default.
• W1996014677 hasConcept C187320778 @default.
• W1996014677 hasConcept C197046000 @default.
• W1996014677 hasConcept C205649164 @default.
• W1996014677 hasConcept C39432304 @default.
• W1996014677 hasConcept C49204034 @default.
• W1996014677 hasConcept C53739315 @default.
• W1996014677 hasConcept C58640448 @default.
• W1996014677 hasConcept C76886044 @default.
• W1996014677 hasConcept C81660378 @default.
• W1996014677 hasConcept C91586092 @default.
• W1996014677 hasConceptScore W1996014677C107054158 @default.
• W1996014677 hasConceptScore W1996014677C111368507 @default.
• W1996014677 hasConceptScore W1996014677C126197015 @default.
• W1996014677 hasConceptScore W1996014677C126645576 @default.
• W1996014677 hasConceptScore W1996014677C127313418 @default.
• W1996014677 hasConceptScore W1996014677C132651083 @default.
• W1996014677 hasConceptScore W1996014677C153294291 @default.
• W1996014677 hasConceptScore W1996014677C168754636 @default.
• W1996014677 hasConceptScore W1996014677C187320778 @default.
• W1996014677 hasConceptScore W1996014677C197046000 @default.
• W1996014677 hasConceptScore W1996014677C205649164 @default.
• W1996014677 hasConceptScore W1996014677C39432304 @default.
• W1996014677 hasConceptScore W1996014677C49204034 @default.
• W1996014677 hasConceptScore W1996014677C53739315 @default.
• W1996014677 hasConceptScore W1996014677C58640448 @default.
• W1996014677 hasConceptScore W1996014677C76886044 @default.
• W1996014677 hasConceptScore W1996014677C81660378 @default.
• W1996014677 hasConceptScore W1996014677C91586092 @default.
• W1996014677 hasLocation W19960146771 @default.
• W1996014677 hasOpenAccess W1996014677 @default.
• W1996014677 hasPrimaryLocation W19960146771 @default.
• W1996014677 hasRelatedWork W1511270684 @default.
• W1996014677 hasRelatedWork W167282916 @default.
• W1996014677 hasRelatedWork W2079155244 @default.
• W1996014677 hasRelatedWork W2116919207 @default.
• W1996014677 hasRelatedWork W2373852752 @default.
• W1996014677 hasRelatedWork W2615233627 @default.
• W1996014677 hasRelatedWork W2738071454 @default.
• W1996014677 hasRelatedWork W2981013795 @default.
• W1996014677 hasRelatedWork W3005557374 @default.
• W1996014677 hasRelatedWork W4310226094 @default.
• W1996014677 hasVolume "23" @default.

• next