Matches in SemOpenAlex for { <https://semopenalex.org/work/W1692246507> ?p ?o ?g. }
- W1692246507 endingPage "121" @default.
- W1692246507 startingPage "108" @default.
- W1692246507 abstract "River sensitivity describes the nature and rate of channel adjustments. An approach to analysis of geomorphic river sensitivity outlined in this paper relates potential sensitivity based on the expected capacity of adjustment for a river type to the recent history of channel adjustment. This approach was trialled to assess low, moderate and high geomorphic sensitivity for four different types of river (10 reaches in total) along the Lower Tongariro River, North Island, New Zealand. Building upon the River Styles framework, river types were differentiated based upon valley setting (width and confinement), channel planform, geomorphic unit assemblages and bed material size. From this, the behavioural regime and potential for adjustment (type and extent) were determined. Historical maps and aerial photographs were geo-rectified and the channel planform digitised to assess channel adjustments for each reach from 1928 to 2007. Floodplain width controlled by terraces, exerted a strong influence upon reach scale sensitivity for the partly-confined, wandering, cobble-bed river. Although forced boundaries occur infrequently, the width of the active channel zone is constrained. An unconfined braided river reach directly downstream of the terrace-confined section was the most geomorphically sensitive reach. The channel in this reach adjusted recurrently to sediment inputs that were flushed through more confined, better connected upstream reaches. A meandering, sand-bed river in downstream reaches has exhibited negligible rates of channel migration. However, channel narrowing in this reach and the associated delta indicate that the system is approaching a threshold condition, beyond which channel avulsion is likely to occur. As this would trigger more rapid migration, this reach is considered to be more geomorphically sensitive than analysis of its low migration rate alone would indicate. This demonstrates how sensitivity is fashioned both by the behavioural regime of a reach and flow/sediment input from upstream. The approach to assess geomorphic river sensitivity outlined here could support ‘room to move’ or ‘freedom space’ approaches to river management by relating likely channel adjustments for the type of river under consideration to the area of land that is required to contain ‘natural’ patterns and rates of geomorphic functionality." @default.
- W1692246507 created "2016-06-24" @default.
- W1692246507 creator A5087334667 @default.
- W1692246507 creator A5088814817 @default.
- W1692246507 date "2015-12-01" @default.
- W1692246507 modified "2023-09-25" @default.
- W1692246507 title "Assessing geomorphic sensitivity in relation to river capacity for adjustment" @default.
- W1692246507 cites W1572223630 @default.
- W1692246507 cites W1597339747 @default.
- W1692246507 cites W1981100159 @default.
- W1692246507 cites W1982544174 @default.
- W1692246507 cites W1983009123 @default.
- W1692246507 cites W1985093159 @default.
- W1692246507 cites W1993543335 @default.
- W1692246507 cites W2007511908 @default.
- W1692246507 cites W2011738126 @default.
- W1692246507 cites W2017754297 @default.
- W1692246507 cites W2019409002 @default.
- W1692246507 cites W2020489173 @default.
- W1692246507 cites W2037438634 @default.
- W1692246507 cites W2039374518 @default.
- W1692246507 cites W2039869390 @default.
- W1692246507 cites W2048164109 @default.
- W1692246507 cites W2055940891 @default.
- W1692246507 cites W2057839787 @default.
- W1692246507 cites W2063105305 @default.
- W1692246507 cites W2069834850 @default.
- W1692246507 cites W2075151628 @default.
- W1692246507 cites W2075975612 @default.
- W1692246507 cites W2077632965 @default.
- W1692246507 cites W2087469764 @default.
- W1692246507 cites W2101071735 @default.
- W1692246507 cites W2114666631 @default.
- W1692246507 cites W2125454074 @default.
- W1692246507 cites W2146981313 @default.
- W1692246507 cites W2147366826 @default.
- W1692246507 cites W2153361544 @default.
- W1692246507 cites W2153839336 @default.
- W1692246507 cites W2156847720 @default.
- W1692246507 cites W2319440775 @default.
- W1692246507 cites W2328303514 @default.
- W1692246507 doi "https://doi.org/10.1016/j.geomorph.2015.09.009" @default.
- W1692246507 hasPublicationYear "2015" @default.
- W1692246507 type Work @default.
- W1692246507 sameAs 1692246507 @default.
- W1692246507 citedByCount "42" @default.
- W1692246507 countsByYear W16922465072016 @default.
- W1692246507 countsByYear W16922465072017 @default.
- W1692246507 countsByYear W16922465072018 @default.
- W1692246507 countsByYear W16922465072019 @default.
- W1692246507 countsByYear W16922465072020 @default.
- W1692246507 countsByYear W16922465072021 @default.
- W1692246507 countsByYear W16922465072022 @default.
- W1692246507 countsByYear W16922465072023 @default.
- W1692246507 crossrefType "journal-article" @default.
- W1692246507 hasAuthorship W1692246507A5087334667 @default.
- W1692246507 hasAuthorship W1692246507A5088814817 @default.
- W1692246507 hasConcept C114793014 @default.
- W1692246507 hasConcept C115038398 @default.
- W1692246507 hasConcept C119599485 @default.
- W1692246507 hasConcept C127162648 @default.
- W1692246507 hasConcept C127313418 @default.
- W1692246507 hasConcept C127413603 @default.
- W1692246507 hasConcept C127491152 @default.
- W1692246507 hasConcept C135114317 @default.
- W1692246507 hasConcept C146978453 @default.
- W1692246507 hasConcept C155681218 @default.
- W1692246507 hasConcept C166957645 @default.
- W1692246507 hasConcept C185933670 @default.
- W1692246507 hasConcept C187320778 @default.
- W1692246507 hasConcept C18903297 @default.
- W1692246507 hasConcept C20470049 @default.
- W1692246507 hasConcept C205649164 @default.
- W1692246507 hasConcept C2776638177 @default.
- W1692246507 hasConcept C2816523 @default.
- W1692246507 hasConcept C5072461 @default.
- W1692246507 hasConcept C58640448 @default.
- W1692246507 hasConcept C65589250 @default.
- W1692246507 hasConcept C76886044 @default.
- W1692246507 hasConcept C86803240 @default.
- W1692246507 hasConceptScore W1692246507C114793014 @default.
- W1692246507 hasConceptScore W1692246507C115038398 @default.
- W1692246507 hasConceptScore W1692246507C119599485 @default.
- W1692246507 hasConceptScore W1692246507C127162648 @default.
- W1692246507 hasConceptScore W1692246507C127313418 @default.
- W1692246507 hasConceptScore W1692246507C127413603 @default.
- W1692246507 hasConceptScore W1692246507C127491152 @default.
- W1692246507 hasConceptScore W1692246507C135114317 @default.
- W1692246507 hasConceptScore W1692246507C146978453 @default.
- W1692246507 hasConceptScore W1692246507C155681218 @default.
- W1692246507 hasConceptScore W1692246507C166957645 @default.
- W1692246507 hasConceptScore W1692246507C185933670 @default.
- W1692246507 hasConceptScore W1692246507C187320778 @default.
- W1692246507 hasConceptScore W1692246507C18903297 @default.
- W1692246507 hasConceptScore W1692246507C20470049 @default.
- W1692246507 hasConceptScore W1692246507C205649164 @default.
- W1692246507 hasConceptScore W1692246507C2776638177 @default.
- W1692246507 hasConceptScore W1692246507C2816523 @default.