FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2340493211> ?p ?o ?g. }

• W2340493211 endingPage "101" @default.
• W2340493211 startingPage "90" @default.
• W2340493211 abstract "Abstract The Araguaia River in central Brazil is the largest river draining the Brazilian savanna. Located in a tropical wet-dry climate, the middle Araguaia River has an extensive and complex alluvial floodplain composed of a mosaic of geomorphologic units, dense alluvial forest, and many floodplain lakes. The Araguaia River is not currently dammed, and thus it provides an opportunity to analyze flooding hydrology in a relatively un-altered tropical system. Using average daily discharge measurements from 1975 to 2011, we analyze patterns of peak discharge attenuation (defined as the reduction in absolute peak discharge in m 3  s − 1 ). We link peak discharge attenuation to bankfull discharge, explore whether peak discharge attenuation results in increased base level flows in the dry season following peak discharge, and use a simplified short-term water budget to determine whether peak discharge attenuation results in the loss of discharge from the channel over the flooding season (November to May). In addition, we explore other potential factors causing peak discharge attenuation, including surface water connectivity between the channel and floodplain lakes and floodplain lake area change between the dry season and the wet season. Although fluvial connectivity between the main channel and the floodplains starts before bankfull stage, we find that large peak discharge attenuation (up to 30% reduction in peak discharge) in the middle Araguaia usually occurs when the river rises above bankfull discharge. The river flow that is lost to the floodplain and floodplain lakes when peak discharge attenuation occurs usually returns to the channel by the end of the flooding season. However, the odds of increased baseflows in the dry season after flooding seasons with peak discharge attenuation are higher compared to flooding seasons without peak discharge attenuation for one of the studied reaches. Some types of floodplain lakes greatly increase in area from the dry season to the wet season, and many floodplain lakes become connected via surface water in the wet season. We have not found similar examples of peak attenuation in this type of tropical wet-dry floodplain system, indicating that the middle Araguaia River may be a unique system or that further research is needed." @default.
• W2340493211 created "2016-06-24" @default.
• W2340493211 creator A5013153136 @default.
• W2340493211 creator A5056106966 @default.
• W2340493211 date "2016-08-01" @default.
• W2340493211 modified "2023-10-13" @default.
• W2340493211 title "Flooding hydrology and peak discharge attenuation along the middle Araguaia River in central Brazil" @default.
• W2340493211 cites W1576669151 @default.
• W2340493211 cites W1967485254 @default.
• W2340493211 cites W1970101073 @default.
• W2340493211 cites W1970962423 @default.
• W2340493211 cites W1971630418 @default.
• W2340493211 cites W1983484955 @default.
• W2340493211 cites W1984242994 @default.
• W2340493211 cites W1989293071 @default.
• W2340493211 cites W1989746171 @default.
• W2340493211 cites W1998573861 @default.
• W2340493211 cites W2006427720 @default.
• W2340493211 cites W2017489522 @default.
• W2340493211 cites W2022221953 @default.
• W2340493211 cites W2035956818 @default.
• W2340493211 cites W2043442250 @default.
• W2340493211 cites W2044285054 @default.
• W2340493211 cites W2045301461 @default.
• W2340493211 cites W2060849424 @default.
• W2340493211 cites W2068400486 @default.
• W2340493211 cites W2077765918 @default.
• W2340493211 cites W2082167141 @default.
• W2340493211 cites W2082237253 @default.
• W2340493211 cites W2090057113 @default.
• W2340493211 cites W2094651287 @default.
• W2340493211 cites W2095344712 @default.
• W2340493211 cites W2096113236 @default.
• W2340493211 cites W2101678239 @default.
• W2340493211 cites W2101753605 @default.
• W2340493211 cites W2116664747 @default.
• W2340493211 cites W2121465475 @default.
• W2340493211 cites W2125980029 @default.
• W2340493211 cites W2126473894 @default.
• W2340493211 cites W2133238415 @default.
• W2340493211 cites W2142743292 @default.
• W2340493211 cites W2145087958 @default.
• W2340493211 cites W2154330429 @default.
• W2340493211 cites W2156376546 @default.
• W2340493211 cites W2162348455 @default.
• W2340493211 cites W2346537738 @default.
• W2340493211 cites W4250391486 @default.
• W2340493211 cites W43752361 @default.
• W2340493211 doi "https://doi.org/10.1016/j.catena.2016.03.043" @default.
• W2340493211 hasPublicationYear "2016" @default.
• W2340493211 type Work @default.
• W2340493211 sameAs 2340493211 @default.
• W2340493211 citedByCount "39" @default.
• W2340493211 countsByYear W23404932112017 @default.
• W2340493211 countsByYear W23404932112018 @default.
• W2340493211 countsByYear W23404932112019 @default.
• W2340493211 countsByYear W23404932112020 @default.
• W2340493211 countsByYear W23404932112021 @default.
• W2340493211 countsByYear W23404932112022 @default.
• W2340493211 countsByYear W23404932112023 @default.
• W2340493211 crossrefType "journal-article" @default.
• W2340493211 hasAuthorship W2340493211A5013153136 @default.
• W2340493211 hasAuthorship W2340493211A5056106966 @default.
• W2340493211 hasBestOaLocation W23404932111 @default.
• W2340493211 hasConcept C114793014 @default.
• W2340493211 hasConcept C120665830 @default.
• W2340493211 hasConcept C121332964 @default.
• W2340493211 hasConcept C127313418 @default.
• W2340493211 hasConcept C15744967 @default.
• W2340493211 hasConcept C184652730 @default.
• W2340493211 hasConcept C186594467 @default.
• W2340493211 hasConcept C187320778 @default.
• W2340493211 hasConcept C39432304 @default.
• W2340493211 hasConcept C542102704 @default.
• W2340493211 hasConcept C76886044 @default.
• W2340493211 hasConceptScore W2340493211C114793014 @default.
• W2340493211 hasConceptScore W2340493211C120665830 @default.
• W2340493211 hasConceptScore W2340493211C121332964 @default.
• W2340493211 hasConceptScore W2340493211C127313418 @default.
• W2340493211 hasConceptScore W2340493211C15744967 @default.
• W2340493211 hasConceptScore W2340493211C184652730 @default.
• W2340493211 hasConceptScore W2340493211C186594467 @default.
• W2340493211 hasConceptScore W2340493211C187320778 @default.
• W2340493211 hasConceptScore W2340493211C39432304 @default.
• W2340493211 hasConceptScore W2340493211C542102704 @default.
• W2340493211 hasConceptScore W2340493211C76886044 @default.
• W2340493211 hasFunder F4320306076 @default.
• W2340493211 hasLocation W23404932111 @default.
• W2340493211 hasOpenAccess W2340493211 @default.
• W2340493211 hasPrimaryLocation W23404932111 @default.
• W2340493211 hasRelatedWork W1552602368 @default.
• W2340493211 hasRelatedWork W1652433593 @default.
• W2340493211 hasRelatedWork W2015964053 @default.
• W2340493211 hasRelatedWork W2020535921 @default.
• W2340493211 hasRelatedWork W2027431735 @default.
• W2340493211 hasRelatedWork W2030153807 @default.
• W2340493211 hasRelatedWork W2065309139 @default.
• W2340493211 hasRelatedWork W2151186631 @default.

• next