FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3093706134> ?p ?o ?g. }

• W3093706134 endingPage "5416" @default.
• W3093706134 startingPage "5402" @default.
• W3093706134 abstract "Abstract Climate‐driven alterations of hydro‐meteorological conditions can change river flow regimes and potentially affect the migration behaviour of fishes and the productivity of important fisheries in the Amazon basin, such as those for the continental‐scale migratory goliath catfishes ( Brachyplatystoma , Pimelodidae). In this study, we investigated hydrologic responses to climate change using a hydrologic model forced with climate inputs, which integrate historical (2001–2010) observations and general circulation model (GCM) projections under the emission scenario Representative Concentration Pathway 8.5. We developed an empirical model to characterize future (2090–2099) climate‐change impacts on goliath catfish spawning migrations as a function of river flow depth dynamics at the upstream elevational limit of spawning (250 m) in headwater basins of the Amazon. The model results revealed spatially variable impacts of climate change on the catfish spawning migrations. The Marañón, Ucayali, Juruá, Purus, and Madeira basins had a predicted increase in the annual mean (3–8%) and maximum (1.1–4.9%) spawning migration rate (i.e., the fraction of fish that migrate to the spawning grounds in a day), mainly due to the lengthened rising phase of flow‐driven migratory events during wet seasons. The Caquetá‐Japurá, Putumayo‐Içá, Napo, and Blanco rivers had predicted decreases (3–7%) in the mean migration rate because of decreases in the length of the rising season of flow depth and the frequency of migratory events. The predicted timing of fish spawning migrations (quantified by the temporal centroid of migration rates) was delayed by 7–10 days in the west‐central and southwest regions and was 8 days earlier in the northwest and northcentral areas, due to changes in the onset of the rising season. We established a river depth baseline that controls the onset of goliath catfish spawning migration. This depth varies between 0.9–5.6 m across study sites. We found that the estimated depth baseline was most sensitive to uncertainties in river width and cross‐sectional channel shape. These results may help inform sustainable adaptation strategies for ecosystem conservation and local fisheries management in the Amazon basin." @default.
• W3093706134 created "2020-10-29" @default.
• W3093706134 creator A5017343084 @default.
• W3093706134 creator A5041199920 @default.
• W3093706134 creator A5043707054 @default.
• W3093706134 creator A5044052813 @default.
• W3093706134 creator A5063214837 @default.
• W3093706134 creator A5063570054 @default.
• W3093706134 creator A5067115370 @default.
• W3093706134 creator A5069061182 @default.
• W3093706134 creator A5070171363 @default.
• W3093706134 creator A5088963922 @default.
• W3093706134 date "2020-11-05" @default.
• W3093706134 modified "2023-10-12" @default.
• W3093706134 title "Future climate impacts on the hydrology of headwater streams in the Amazon River Basin: Implications for migratory goliath catfishes" @default.
• W3093706134 cites W1500296370 @default.
• W3093706134 cites W1520348967 @default.
• W3093706134 cites W1530720880 @default.
• W3093706134 cites W1587869157 @default.
• W3093706134 cites W1838144200 @default.
• W3093706134 cites W1947824874 @default.
• W3093706134 cites W1950151724 @default.
• W3093706134 cites W1976984961 @default.
• W3093706134 cites W1983747486 @default.
• W3093706134 cites W1984083988 @default.
• W3093706134 cites W1989910206 @default.
• W3093706134 cites W1993929674 @default.
• W3093706134 cites W1995622703 @default.
• W3093706134 cites W2001788659 @default.
• W3093706134 cites W2011560911 @default.
• W3093706134 cites W2017559255 @default.
• W3093706134 cites W2024966118 @default.
• W3093706134 cites W2042692910 @default.
• W3093706134 cites W2046373044 @default.
• W3093706134 cites W2054653365 @default.
• W3093706134 cites W2056744606 @default.
• W3093706134 cites W2081469389 @default.
• W3093706134 cites W2088194513 @default.
• W3093706134 cites W2093667908 @default.
• W3093706134 cites W2102036164 @default.
• W3093706134 cites W2116145880 @default.
• W3093706134 cites W2121621290 @default.
• W3093706134 cites W2125394241 @default.
• W3093706134 cites W2138763184 @default.
• W3093706134 cites W2139051261 @default.
• W3093706134 cites W2157954302 @default.
• W3093706134 cites W2171034873 @default.
• W3093706134 cites W2265611037 @default.
• W3093706134 cites W2310867653 @default.
• W3093706134 cites W2317766022 @default.
• W3093706134 cites W2411745069 @default.
• W3093706134 cites W2481081268 @default.
• W3093706134 cites W2493090550 @default.
• W3093706134 cites W2503568925 @default.
• W3093706134 cites W2520452758 @default.
• W3093706134 cites W2554889480 @default.
• W3093706134 cites W2586486036 @default.
• W3093706134 cites W2620109964 @default.
• W3093706134 cites W2767319224 @default.
• W3093706134 cites W2800102383 @default.
• W3093706134 cites W2895126088 @default.
• W3093706134 cites W2913172698 @default.
• W3093706134 cites W2969878846 @default.
• W3093706134 cites W2993838707 @default.
• W3093706134 cites W3003393482 @default.
• W3093706134 cites W3022999716 @default.
• W3093706134 doi "https://doi.org/10.1002/hyp.13952" @default.
• W3093706134 hasPublicationYear "2020" @default.
• W3093706134 type Work @default.
• W3093706134 sameAs 3093706134 @default.
• W3093706134 citedByCount "7" @default.
• W3093706134 countsByYear W30937061342021 @default.
• W3093706134 countsByYear W30937061342022 @default.
• W3093706134 countsByYear W30937061342023 @default.
• W3093706134 crossrefType "journal-article" @default.
• W3093706134 hasAuthorship W3093706134A5017343084 @default.
• W3093706134 hasAuthorship W3093706134A5041199920 @default.
• W3093706134 hasAuthorship W3093706134A5043707054 @default.
• W3093706134 hasAuthorship W3093706134A5044052813 @default.
• W3093706134 hasAuthorship W3093706134A5063214837 @default.
• W3093706134 hasAuthorship W3093706134A5063570054 @default.
• W3093706134 hasAuthorship W3093706134A5067115370 @default.
• W3093706134 hasAuthorship W3093706134A5069061182 @default.
• W3093706134 hasAuthorship W3093706134A5070171363 @default.
• W3093706134 hasAuthorship W3093706134A5088963922 @default.
• W3093706134 hasConcept C109007969 @default.
• W3093706134 hasConcept C114793014 @default.
• W3093706134 hasConcept C117773394 @default.
• W3093706134 hasConcept C126645576 @default.
• W3093706134 hasConcept C127313418 @default.
• W3093706134 hasConcept C132651083 @default.
• W3093706134 hasConcept C139719470 @default.
• W3093706134 hasConcept C162324750 @default.
• W3093706134 hasConcept C187320778 @default.
• W3093706134 hasConcept C18903297 @default.
• W3093706134 hasConcept C204983608 @default.
• W3093706134 hasConcept C205649164 @default.
• W3093706134 hasConcept C2776654248 @default.

• next