Deciphering historic change in tributary-junction fans in response to catchment-wide sedimentary disturbance

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dc.contributor.advisor Tunnicliffe, J en
dc.contributor.advisor Brierley, G en
dc.contributor.author Leenman, Anya en
dc.date.accessioned 2016-05-24T21:52:48Z en
dc.date.issued 2016 en
dc.identifier.citation 2016 en
dc.identifier.uri http://hdl.handle.net/2292/28901 en
dc.description Full text is available to authenticated members of The University of Auckland only. en
dc.description.abstract Alluvial fans at tributary junctions are important moderators of sediment flux through river networks, particularly where the main stem and tributary valleys are responding to disturbance at different rates. In this work, I examine the factors that govern the decadal-scale rate and morphologic expression of tributary-junction fan development, following major sedimentary disturbance. In New Zealand’s East Cape region, the combination of recent deforestation with sandstone and mudstone lithology, high rainfall, uplift, and steep topography produce a landscape where rates of hillslope erosion and sediment transfer through rivers are some of the highest measured on earth. This study investigates the response of tributary-junction alluvial fans to sediment generation following deforestation and during extreme storms, such as Cyclone Bola in 1988. The dynamics of five tributary-junction fans along the Tapuaeroa River are examined for the period 1939-2015, using historic aerial photography, channel cross-sectional surveys and structure-frommotion photogrammetry. In response to major sediment loading, fan morphologic change included areal increases of up to 130,000 m², aggradation of up to 12 m, and fan-front progradation of up to 170 m. The maximum volume of fan sediment storage ranged from 15,000 to 1,500,000 m³. Change in fan morphology, sediment storage and coupling was related to temporal and spatial variation in a range of influences, both in the tributary catchments and the main stem channel. The major influences were climate, change in land cover, tributary-catchment connectivity, and most importantly, the nature of fan interaction with the main stem channel, at both seasonal and decadal scales. The fans’ ability to buffer the Tapuaeroa River from change in the tributaries was strongly conditioned by their interaction with the main stem channel. Their buffering capacity decreased through the study period, when the main stem aggraded and widened. Although previous studies have examined relationships between fan morphometry and tributary catchment characteristics, this study has shown that fan morphometry can vary considerably at decadal, annual or even monthly timescales. Such studies could benefit by examining regional histories of sedimentary disturbance. en
dc.publisher ResearchSpace@Auckland en
dc.relation.ispartof Masters Thesis - University of Auckland en
dc.relation.isreferencedby UoA99264871905702091 en
dc.rights Items in ResearchSpace are protected by copyright, with all rights reserved, unless otherwise indicated. Previously published items are made available in accordance with the copyright policy of the publisher. en
dc.rights Restricted Item. Available to authenticated members of The University of Auckland. en
dc.rights.uri https://researchspace.auckland.ac.nz/docs/uoa-docs/rights.htm en
dc.rights.uri http://creativecommons.org/licenses/by-nc-sa/3.0/nz/ en
dc.title Deciphering historic change in tributary-junction fans in response to catchment-wide sedimentary disturbance en
dc.type Thesis en
thesis.degree.discipline Geography en
thesis.degree.grantor The University of Auckland en
thesis.degree.level Masters en
dc.rights.holder Copyright: The Author en
pubs.elements-id 528112 en
pubs.record-created-at-source-date 2016-05-25 en


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