FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2793526001> ?p ?o ?g. }

• W2793526001 endingPage "1057" @default.
• W2793526001 startingPage "1031" @default.
• W2793526001 abstract "Abstract Bathymetric data are a critical input to hydraulic models. However, river depth and shape cannot be systematically observed remotely, and field data are both scarce and expensive to collect. In flood modeling, river roughness and geometry compensate for each other, with different parameter sets often being able to map model predictions equally well to the observed data, commonly known as equifinality. This study presents a numerical experiment to investigate an effective yet parsimonious representation of channel geometry that can be used for operational flood forecasting. The LISFLOOD‐FP hydraulic model was used to simulate a hypothetical flood event in the Clarence catchment (Australia). A high‐resolution model simulation based on accurate bathymetric field data was used to benchmark coarser model simulations based on simplified river geometries. These simplified river geometries were derived from a combination of globally available empirical formulations, remote sensing data, and a limited number of measurements. Model predictive discrepancy between simulations with field data and simplified geometries allowed an assessment of the geometry impact on inundation dynamics. In this study site, the channel geometrical representation for a reliable inundation forecast could be achieved using remote sensing‐derived river width values combined with a few measurements of river depth sampled at strategic locations. Furthermore, this study showed that spatially distributed remote sensing‐derived inundation levels at the very early stages of a flood event have the potential to support the effective diagnosis of errors in model implementations." @default.
• W2793526001 created "2018-03-29" @default.
• W2793526001 creator A5012590564 @default.
• W2793526001 creator A5020270621 @default.
• W2793526001 creator A5044251090 @default.
• W2793526001 creator A5046307178 @default.
• W2793526001 date "2018-02-01" @default.
• W2793526001 modified "2023-10-15" @default.
• W2793526001 title "Effective Representation of River Geometry in Hydraulic Flood Forecast Models" @default.
• W2793526001 cites W1500512887 @default.
• W2793526001 cites W1549277179 @default.
• W2793526001 cites W1587869157 @default.
• W2793526001 cites W1631778242 @default.
• W2793526001 cites W1694119402 @default.
• W2793526001 cites W1781062510 @default.
• W2793526001 cites W1826913668 @default.
• W2793526001 cites W1843782814 @default.
• W2793526001 cites W1846570231 @default.
• W2793526001 cites W1862386067 @default.
• W2793526001 cites W1873066041 @default.
• W2793526001 cites W1890688639 @default.
• W2793526001 cites W1925824783 @default.
• W2793526001 cites W1935964479 @default.
• W2793526001 cites W1945275476 @default.
• W2793526001 cites W1967166174 @default.
• W2793526001 cites W1972074586 @default.
• W2793526001 cites W1972580235 @default.
• W2793526001 cites W1978235888 @default.
• W2793526001 cites W1978537006 @default.
• W2793526001 cites W1981549240 @default.
• W2793526001 cites W1986837469 @default.
• W2793526001 cites W1991921673 @default.
• W2793526001 cites W1992023913 @default.
• W2793526001 cites W1993754709 @default.
• W2793526001 cites W1994424126 @default.
• W2793526001 cites W1994777546 @default.
• W2793526001 cites W2001430721 @default.
• W2793526001 cites W2002610571 @default.
• W2793526001 cites W2006461609 @default.
• W2793526001 cites W2008682495 @default.
• W2793526001 cites W2014826590 @default.
• W2793526001 cites W2016303979 @default.
• W2793526001 cites W2017977562 @default.
• W2793526001 cites W2020266513 @default.
• W2793526001 cites W2021324314 @default.
• W2793526001 cites W2023020665 @default.
• W2793526001 cites W2030130356 @default.
• W2793526001 cites W2031206018 @default.
• W2793526001 cites W2032226859 @default.
• W2793526001 cites W2033117719 @default.
• W2793526001 cites W2033602192 @default.
• W2793526001 cites W2045239238 @default.
• W2793526001 cites W2049106247 @default.
• W2793526001 cites W2054631580 @default.
• W2793526001 cites W2055668893 @default.
• W2793526001 cites W2057128986 @default.
• W2793526001 cites W2063204990 @default.
• W2793526001 cites W2068990297 @default.
• W2793526001 cites W2073060807 @default.
• W2793526001 cites W2089594470 @default.
• W2793526001 cites W2090576362 @default.
• W2793526001 cites W2091819605 @default.
• W2793526001 cites W2097208041 @default.
• W2793526001 cites W2098430501 @default.
• W2793526001 cites W2101044141 @default.
• W2793526001 cites W2101475156 @default.
• W2793526001 cites W2106129499 @default.
• W2793526001 cites W2106781552 @default.
• W2793526001 cites W2109727347 @default.
• W2793526001 cites W2111456289 @default.
• W2793526001 cites W2112152298 @default.
• W2793526001 cites W2116939143 @default.
• W2793526001 cites W2130703758 @default.
• W2793526001 cites W2137565396 @default.
• W2793526001 cites W2138236578 @default.
• W2793526001 cites W2142734708 @default.
• W2793526001 cites W2145635192 @default.
• W2793526001 cites W2147771508 @default.
• W2793526001 cites W2157954302 @default.
• W2793526001 cites W2166309152 @default.
• W2793526001 cites W2166790957 @default.
• W2793526001 cites W2167533190 @default.
• W2793526001 cites W2170772598 @default.
• W2793526001 cites W2171675471 @default.
• W2793526001 cites W2179843978 @default.
• W2793526001 cites W2180404242 @default.
• W2793526001 cites W2192883182 @default.
• W2793526001 cites W2208198711 @default.
• W2793526001 cites W2266574579 @default.
• W2793526001 cites W2276725184 @default.
• W2793526001 cites W2290410585 @default.
• W2793526001 cites W2309448491 @default.
• W2793526001 cites W2398837725 @default.
• W2793526001 cites W2462089918 @default.
• W2793526001 cites W2507017087 @default.
• W2793526001 cites W2507587848 @default.
• W2793526001 cites W2527248197 @default.
• W2793526001 cites W2550967757 @default.

• next