FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1942021036> ?p ?o ?g. }

• W1942021036 endingPage "1456" @default.
• W1942021036 startingPage "1444" @default.
• W1942021036 abstract "ABSTRACT The term connectivity has emerged as a powerful concept in hydrology and geomorphology and is emerging as an innovative component of catchment erosion modeling studies. However, considerable confusion remains regarding its definition and quantification, especially as it relates to fluvial systems. This confusion is exacerbated by a lack of detailed case studies and by the tendency to treat water and sediment separately. Extreme flood events provide a useful framework to assess variability in connectivity, particularly the connection between channels and floodplains. The catastrophic flood of January 2011 in the Lockyer valley, southeast Queensland, Australia provides an opportunity to examine this dimension in some detail and to determine how these dynamics operate under high flow regimes. High resolution aerial photographs and multi‐temporal LiDAR digital elevation models (DEMs), coupled with hydrological modeling, are used to assess both the nature of hydrologic and sedimentological connectivity and their dominant controls. Longitudinal variations in flood inundation extent led to the identification of nine reaches which displayed varying channel–floodplain connectivity. The major control on connectivity was significant non‐linear changes in channel capacity due to the presence of notable macrochannels which contained a > 3000 average recurrence interval (ARI) event at mid‐catchment locations. The spatial pattern of hydrological connectivity was not straight‐forward in spite of bankfull discharges for selected reaches exceeding 5600 m 3 s –1 . Data indicate that the main channel boundary was the dominant source of sediment while the floodplains, where inundated, were the dominant sinks. Spatial variability in channel–floodplain hydrological connectivity leads to dis‐connectivity in the downstream transfer of sediments between reaches and affected sediment storage on adjacent floodplains. Consideration of such variability for even the most extreme flood events, highlights the need to carefully consider non‐linear changes in key variables such as channel capacity and flood conveyance in the development of a quantitative ‘connectivity index’. Copyright © 2013 John Wiley & Sons, Ltd." @default.
• W1942021036 created "2016-06-24" @default.
• W1942021036 creator A5023533251 @default.
• W1942021036 creator A5034376889 @default.
• W1942021036 creator A5040423781 @default.
• W1942021036 date "2013-05-30" @default.
• W1942021036 modified "2023-10-11" @default.
• W1942021036 title "Channel-floodplain connectivity during an extreme flood event: implications for sediment erosion, deposition, and delivery" @default.
• W1942021036 cites W1498793884 @default.
• W1942021036 cites W1507449691 @default.
• W1942021036 cites W1526822975 @default.
• W1942021036 cites W1529261671 @default.
• W1942021036 cites W1585186382 @default.
• W1942021036 cites W1826291402 @default.
• W1942021036 cites W1931550268 @default.
• W1942021036 cites W1974173367 @default.
• W1942021036 cites W1979821905 @default.
• W1942021036 cites W1987552704 @default.
• W1942021036 cites W1990287524 @default.
• W1942021036 cites W1992000306 @default.
• W1942021036 cites W1996725283 @default.
• W1942021036 cites W1997061485 @default.
• W1942021036 cites W2007075065 @default.
• W1942021036 cites W2007255999 @default.
• W1942021036 cites W2023426064 @default.
• W1942021036 cites W2026086547 @default.
• W1942021036 cites W2029840025 @default.
• W1942021036 cites W2030312177 @default.
• W1942021036 cites W2033757943 @default.
• W1942021036 cites W2037179245 @default.
• W1942021036 cites W2038039104 @default.
• W1942021036 cites W2054732079 @default.
• W1942021036 cites W2064243108 @default.
• W1942021036 cites W2067215661 @default.
• W1942021036 cites W2071080899 @default.
• W1942021036 cites W2071684211 @default.
• W1942021036 cites W2073141769 @default.
• W1942021036 cites W2076573461 @default.
• W1942021036 cites W2077281443 @default.
• W1942021036 cites W2077959121 @default.
• W1942021036 cites W2083797361 @default.
• W1942021036 cites W2084062027 @default.
• W1942021036 cites W2087255756 @default.
• W1942021036 cites W2087930008 @default.
• W1942021036 cites W2088297506 @default.
• W1942021036 cites W2089000436 @default.
• W1942021036 cites W2120619026 @default.
• W1942021036 cites W2127441956 @default.
• W1942021036 cites W2136198117 @default.
• W1942021036 cites W2155951939 @default.
• W1942021036 cites W2796375484 @default.
• W1942021036 cites W4244441313 @default.
• W1942021036 doi "https://doi.org/10.1002/esp.3430" @default.
• W1942021036 hasPublicationYear "2013" @default.
• W1942021036 type Work @default.
• W1942021036 sameAs 1942021036 @default.
• W1942021036 citedByCount "30" @default.
• W1942021036 countsByYear W19420210362013 @default.
• W1942021036 countsByYear W19420210362016 @default.
• W1942021036 countsByYear W19420210362017 @default.
• W1942021036 countsByYear W19420210362018 @default.
• W1942021036 countsByYear W19420210362019 @default.
• W1942021036 countsByYear W19420210362020 @default.
• W1942021036 countsByYear W19420210362021 @default.
• W1942021036 countsByYear W19420210362022 @default.
• W1942021036 countsByYear W19420210362023 @default.
• W1942021036 crossrefType "journal-article" @default.
• W1942021036 hasAuthorship W1942021036A5023533251 @default.
• W1942021036 hasAuthorship W1942021036A5034376889 @default.
• W1942021036 hasAuthorship W1942021036A5040423781 @default.
• W1942021036 hasConcept C109007969 @default.
• W1942021036 hasConcept C112959462 @default.
• W1942021036 hasConcept C114793014 @default.
• W1942021036 hasConcept C119599485 @default.
• W1942021036 hasConcept C123157820 @default.
• W1942021036 hasConcept C127162648 @default.
• W1942021036 hasConcept C127313418 @default.
• W1942021036 hasConcept C127413603 @default.
• W1942021036 hasConcept C155681218 @default.
• W1942021036 hasConcept C166957645 @default.
• W1942021036 hasConcept C181843262 @default.
• W1942021036 hasConcept C187320778 @default.
• W1942021036 hasConcept C205649164 @default.
• W1942021036 hasConcept C2816523 @default.
• W1942021036 hasConcept C39432304 @default.
• W1942021036 hasConcept C58640448 @default.
• W1942021036 hasConcept C62649853 @default.
• W1942021036 hasConcept C64584415 @default.
• W1942021036 hasConcept C74256435 @default.
• W1942021036 hasConcept C76886044 @default.
• W1942021036 hasConceptScore W1942021036C109007969 @default.
• W1942021036 hasConceptScore W1942021036C112959462 @default.
• W1942021036 hasConceptScore W1942021036C114793014 @default.
• W1942021036 hasConceptScore W1942021036C119599485 @default.
• W1942021036 hasConceptScore W1942021036C123157820 @default.
• W1942021036 hasConceptScore W1942021036C127162648 @default.
• W1942021036 hasConceptScore W1942021036C127313418 @default.
• W1942021036 hasConceptScore W1942021036C127413603 @default.

• next