Matches in SemOpenAlex for { <https://semopenalex.org/work/W2804906348> ?p ?o ?g. }
- W2804906348 abstract "This study aims to evaluate the effects of the Canadian Regional Climate Model’s (CRCM) spatial resolution on summer-fall floods simulation. Seven different climate simulations issued from the fourth and the fifth version of the CRCM are employed. Four different climate simulations issued from the fourth version of the CRCM (CRCM4) are compared. They are composed of two simulations driven by the Canadian General Circulation Model (CGCM) and two driven by the ERA-40c reanalysis using grid meshes of 15 km and 45 km resolutions for each driver. Three climate simulations issued from the fifth version of the CRCM (CRCM5) driven by the ERA-Interim at 0.44° (≈ 48 km), 0.22° (≈ 24 km) and 0.11° (≈ 12 km) spatial resolutions are used. All comparisons are evaluated on a daily time-step for the 1961-1990 period (for CRCM4) and for the 1981-2010 period (for CRCM5).These seven simulations (four from CRCM4 and three from CRCM5) are used as input for two hydrological models of varying complexity (HSAMI and MOHYSE). Each model is calibrated using three different objective functions based on the Kling-Gupta Efficiency criteria (KGE) to target the summer-fall floods. Three seasonal indices are used to evaluate the CRCM outputs: bias (temperature), relative bias (precipitation) and variances ratio (temperature and precipitation). In an attempt to evaluate the effects of the spatial resolution on the hydrological modelling of summer-fall floods, streamflow simulations are generated using the seven climate datasets. The generated climate-driven streamflow simulations are analysed by two performance statistics: the seasonal values of KGE and the seasonal relative biases. Summer-fall floods are evaluated through the use of four flood indicators, the 2-year, 5-year, 10-year and 20-year return periods.The results revealed an impact of spatial resolution on climate model outputs (temperature and precipitation) and on summer-fall floods simulation by the two hydrological models and the three different calibration approaches, although this can be due to other elements such as domain size and climate model driver. The flood indicators demonstrate an increase on the summer-fall floods return periods with increasing resolution from both hydrological models. On the other hand the hydrological models structure and the calibration approaches did not show significant impacts on the summer-fall floods. The results highlight the need for further research to assess the additional uncertainty due to the impacts of the climate simulations spatial resolution on hydrological studies." @default.
- W2804906348 created "2018-06-01" @default.
- W2804906348 creator A5049105337 @default.
- W2804906348 date "2018-01-24" @default.
- W2804906348 modified "2023-09-23" @default.
- W2804906348 title "Effects of regional climate model spatial resolution on hydrological modelling of summer-fall floods in southern Quebec" @default.
- W2804906348 cites W1414668584 @default.
- W2804906348 cites W1505551852 @default.
- W2804906348 cites W1548396839 @default.
- W2804906348 cites W158363710 @default.
- W2804906348 cites W1592729344 @default.
- W2804906348 cites W180764761 @default.
- W2804906348 cites W196294027 @default.
- W2804906348 cites W1968965993 @default.
- W2804906348 cites W1972074159 @default.
- W2804906348 cites W1972076434 @default.
- W2804906348 cites W1972183204 @default.
- W2804906348 cites W1974085096 @default.
- W2804906348 cites W1975381791 @default.
- W2804906348 cites W1979062058 @default.
- W2804906348 cites W1990471334 @default.
- W2804906348 cites W1996014222 @default.
- W2804906348 cites W1999500305 @default.
- W2804906348 cites W2000759171 @default.
- W2804906348 cites W2003432069 @default.
- W2804906348 cites W2003776028 @default.
- W2804906348 cites W2004829667 @default.
- W2804906348 cites W2008072410 @default.
- W2804906348 cites W2012408626 @default.
- W2804906348 cites W2024966118 @default.
- W2804906348 cites W2030504740 @default.
- W2804906348 cites W2033904036 @default.
- W2804906348 cites W2034174587 @default.
- W2804906348 cites W2036243883 @default.
- W2804906348 cites W2037877157 @default.
- W2804906348 cites W2038192745 @default.
- W2804906348 cites W2046759075 @default.
- W2804906348 cites W2050834561 @default.
- W2804906348 cites W2054653365 @default.
- W2804906348 cites W2058233582 @default.
- W2804906348 cites W2058427382 @default.
- W2804906348 cites W2058998445 @default.
- W2804906348 cites W2062217294 @default.
- W2804906348 cites W2068194125 @default.
- W2804906348 cites W2073296897 @default.
- W2804906348 cites W2079232752 @default.
- W2804906348 cites W2081676979 @default.
- W2804906348 cites W2090249381 @default.
- W2804906348 cites W2093756001 @default.
- W2804906348 cites W2094349676 @default.
- W2804906348 cites W2096128876 @default.
- W2804906348 cites W2098999708 @default.
- W2804906348 cites W2101211037 @default.
- W2804906348 cites W2104082993 @default.
- W2804906348 cites W2115542045 @default.
- W2804906348 cites W2116356373 @default.
- W2804906348 cites W2116397061 @default.
- W2804906348 cites W2120012334 @default.
- W2804906348 cites W2121745948 @default.
- W2804906348 cites W2121798740 @default.
- W2804906348 cites W2122315938 @default.
- W2804906348 cites W2138763184 @default.
- W2804906348 cites W2139433170 @default.
- W2804906348 cites W2146338288 @default.
- W2804906348 cites W2151244793 @default.
- W2804906348 cites W2163131363 @default.
- W2804906348 cites W2164894943 @default.
- W2804906348 cites W2165848506 @default.
- W2804906348 cites W2167821992 @default.
- W2804906348 cites W2170816806 @default.
- W2804906348 cites W2329995161 @default.
- W2804906348 cites W2338949170 @default.
- W2804906348 cites W2372583805 @default.
- W2804906348 cites W2422022521 @default.
- W2804906348 cites W2474205594 @default.
- W2804906348 cites W2514208833 @default.
- W2804906348 cites W2521223623 @default.
- W2804906348 cites W2542036298 @default.
- W2804906348 cites W2766170004 @default.
- W2804906348 cites W2792905772 @default.
- W2804906348 cites W50285032 @default.
- W2804906348 hasPublicationYear "2018" @default.
- W2804906348 type Work @default.
- W2804906348 sameAs 2804906348 @default.
- W2804906348 citedByCount "0" @default.
- W2804906348 crossrefType "journal-article" @default.
- W2804906348 hasAuthorship W2804906348A5049105337 @default.
- W2804906348 hasConcept C107054158 @default.
- W2804906348 hasConcept C111368507 @default.
- W2804906348 hasConcept C126645576 @default.
- W2804906348 hasConcept C127313418 @default.
- W2804906348 hasConcept C132651083 @default.
- W2804906348 hasConcept C141452985 @default.
- W2804906348 hasConcept C153294291 @default.
- W2804906348 hasConcept C168754636 @default.
- W2804906348 hasConcept C205649164 @default.
- W2804906348 hasConcept C39432304 @default.
- W2804906348 hasConcept C41156917 @default.
- W2804906348 hasConcept C49204034 @default.
- W2804906348 hasConcept C53739315 @default.