Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul
Autor(a) principal: | |
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Data de Publicação: | 2023 |
Tipo de documento: | Tese |
Idioma: | eng |
Título da fonte: | Repositório Institucional da Universidade Federal Fluminense (RIUFF) |
Texto Completo: | http://app.uff.br/riuff/handle/1/28323 |
Resumo: | Coastal dune development and evolution has been one of the main research topics in coastal science (Martínez and Psuty, 2004). However, due to the complexity of the interactions between different driving factors that dictate coastal dune dynamics, the roles that each of the abiotic and biotic drivers play in formation and transformation of these deposits are still poorly understood (Provoost et al., 2011; Barchyn and Hugenholtz, 2012). In a historical time-scale (years to decades) dunefields can undergo significant morphological and ecological changes, shifting from an active/unvegetated state to a stabilized/vegetated state, and vice versa (Hesp, 2013). Studying how dunes evolve in a meso-scale analysis poses a significant challenge to researchers because of the difficulty in combining or obtaining spatial data with enough resolution over a significant period of time (Pickart and Hesp, 2019), and therefore studies that show medium to long-term dune changes are scarce (Hesp, 2013). In the Younghusband Peninsula dune system (South-east coast of South Australia), the availability of high-resolution historical spatial data, combined with climatic data, oceanographic data, and specific environmental conditions, constitutes a good opportunity to study different aspects of meso-scale morphological changes and their main driving factors. The objective of this body of work is to examine the different aspects of meso-scale driving factors of coastal dune dynamics, with the Younghusband Peninsula (YP) as a study case. This work investigates specifically: (1) What were the potential drivers of vegetation cover changes in the last ~70 years; (2) What were the geomorphological changes that occurred due to this vegetation cover vi changes and how did this morphological evolution take place; and (3) What are the main drivers that dictate the foredune morphological variability identified in the southern portion of the YP. The first part of this study (published in Earth Surface Processes and Landforms Journal – Moulton et al., 2019) uses historical aerial images and data from potential biotic and abiotic drivers to investigate why vegetation cover has changed in the last ~70 years in the northern YP. Results show that the decline in exotic rabbit abundance, especially in the 1950s after the introduction of the Myxomatosis virus, present significant correlation to periods of greater vegetation growth. Other factors, such as wind and precipitation variability, did not present any explanatory correlation, leading to the conclusion that rabbit grazing was the most important driving factor of vegetation growth in the YP during this period. The second part of this study investigates the geomorphological transformations induced by the vegetation changes and how the evolution of different dune types took place, with the use of historical aerial imagery and three-dimensional high-resolution topographic data. From 1949 to 2018, the dune system went through significant geomorphological changes due to vegetation stabilization, with relatively simple active transgressive dunefields changing into a complex landscape of active and vegetated blowout/parabolic dunes. Vegetation growth on the marginal interdune depressions and plains, forming narrow elongate vegetated ridges was the main process that lead to the development of a complex of blowouts and parabolic dunes, most of which are already stabilized by 2018. The third and final part of this study investigates the role of various factors controlling foredune evolution that accounts for the alongshore geomorphological vii and volumetric differences along the southeastern portion of the Younghusband Peninsula. For this study a 16 km stretch of beach on the barrier was selected, where minimal environmental changes in some factors such as wind energy and aeolian transport occur. Results show a south to north alongshore increase in foredune height and volume for the 3 years surveyed, together with an increase in wave energy, while other driving factors showed minimal to no changes. These findings indicate that wave energy has an indirect positive relationship with foredune accretion, with wave driven sediment supply to the beach increasing as wave energy rises from south to north. In this study area wave energy has more significant role than aeolian transport limitations on foredune (and relict foredune) development. |
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Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do SulCoastal dunesCoastal geomorphologyVegetal coverCoastal processesDunaZona costeiraGeomorfologiaVegetaçãoDunas costeirasGeomorfologia costeiraCobertura vegetalProcessos costeirosCoastal dune development and evolution has been one of the main research topics in coastal science (Martínez and Psuty, 2004). However, due to the complexity of the interactions between different driving factors that dictate coastal dune dynamics, the roles that each of the abiotic and biotic drivers play in formation and transformation of these deposits are still poorly understood (Provoost et al., 2011; Barchyn and Hugenholtz, 2012). In a historical time-scale (years to decades) dunefields can undergo significant morphological and ecological changes, shifting from an active/unvegetated state to a stabilized/vegetated state, and vice versa (Hesp, 2013). Studying how dunes evolve in a meso-scale analysis poses a significant challenge to researchers because of the difficulty in combining or obtaining spatial data with enough resolution over a significant period of time (Pickart and Hesp, 2019), and therefore studies that show medium to long-term dune changes are scarce (Hesp, 2013). In the Younghusband Peninsula dune system (South-east coast of South Australia), the availability of high-resolution historical spatial data, combined with climatic data, oceanographic data, and specific environmental conditions, constitutes a good opportunity to study different aspects of meso-scale morphological changes and their main driving factors. The objective of this body of work is to examine the different aspects of meso-scale driving factors of coastal dune dynamics, with the Younghusband Peninsula (YP) as a study case. This work investigates specifically: (1) What were the potential drivers of vegetation cover changes in the last ~70 years; (2) What were the geomorphological changes that occurred due to this vegetation cover vi changes and how did this morphological evolution take place; and (3) What are the main drivers that dictate the foredune morphological variability identified in the southern portion of the YP. The first part of this study (published in Earth Surface Processes and Landforms Journal – Moulton et al., 2019) uses historical aerial images and data from potential biotic and abiotic drivers to investigate why vegetation cover has changed in the last ~70 years in the northern YP. Results show that the decline in exotic rabbit abundance, especially in the 1950s after the introduction of the Myxomatosis virus, present significant correlation to periods of greater vegetation growth. Other factors, such as wind and precipitation variability, did not present any explanatory correlation, leading to the conclusion that rabbit grazing was the most important driving factor of vegetation growth in the YP during this period. The second part of this study investigates the geomorphological transformations induced by the vegetation changes and how the evolution of different dune types took place, with the use of historical aerial imagery and three-dimensional high-resolution topographic data. From 1949 to 2018, the dune system went through significant geomorphological changes due to vegetation stabilization, with relatively simple active transgressive dunefields changing into a complex landscape of active and vegetated blowout/parabolic dunes. Vegetation growth on the marginal interdune depressions and plains, forming narrow elongate vegetated ridges was the main process that lead to the development of a complex of blowouts and parabolic dunes, most of which are already stabilized by 2018. The third and final part of this study investigates the role of various factors controlling foredune evolution that accounts for the alongshore geomorphological vii and volumetric differences along the southeastern portion of the Younghusband Peninsula. For this study a 16 km stretch of beach on the barrier was selected, where minimal environmental changes in some factors such as wind energy and aeolian transport occur. Results show a south to north alongshore increase in foredune height and volume for the 3 years surveyed, together with an increase in wave energy, while other driving factors showed minimal to no changes. These findings indicate that wave energy has an indirect positive relationship with foredune accretion, with wave driven sediment supply to the beach increasing as wave energy rises from south to north. In this study area wave energy has more significant role than aeolian transport limitations on foredune (and relict foredune) development.O desenvolvimento e a evolução das dunas costeiras têm sido um dos principais tópicos de pesquisa em ciências costeiras (Martínez e Psuty, 2004). No entanto, devido à complexidade das interações entre os diferentes fatores controladores que determinam a dinâmica das dunas costeiras, os papéis que cada um dos fatores abióticos e bióticos desempenham na formação e transformação desses depósitos ainda são pouco compreendidos (Provoost et al., 2011; Barchyn e Hugenholtz, 2012). Em uma escala de tempo histórica (anos a décadas), campos de dunas podem sofrer mudanças morfológicas e ecológicas significativas, passando de um estado ativo/ não-vegetado para um estado estabilizado/vegetado e vice-versa (Hesp, 2013). Estudar como as dunas evoluem em uma análise em meso-escala representa um desafio significativo para os pesquisadores devido à viii dificuldade em combinar ou obter dados espaciais com resolução suficiente durante um período de tempo significativo (Pickart e Hesp, 2019) e, portanto, estudos que mostram mudanças de médio a longo prazo em dunas costeiras são escassos (Hesp, 2013). No campo de dunas da Península de Younghusband (costa sudeste da Austrália Meridional), a disponibilidade de dados espaciais históricos de alta resolução, combinados com dados climáticos, dados oceanográficos e condições ambientais específicas, constitui uma boa oportunidade para estudar diferentes aspectos das mudanças morfológicas em meso-escala e seus principais fatores determinantes. O objetivo deste trabalho é examinar os diferentes aspectos dos fatores controladores da dinâmica das dunas costeiras em meso-escala, tendo a Península de Younghusband (YP) como um caso de estudo. Este trabalho investiga especificamente: (1) Quais foram os possíveis fatores controladores que implicaram nas mudanças de cobertura vegetal nos últimos ~70 anos; (2) Quais foram as mudanças geomorfológicas que ocorreram devido a essa alteração da cobertura vegetal e como se sucedeu essa evolução morfológica; e (3) Quais são os principais fatores que determinam a variabilidade morfológica das dunas frontais identificadas na porção sul da península. A primeira parte deste estudo (publicada na revista Earth Surface Processes and Landforms - Moulton et al., 2019) usa imagens aéreas históricas e dados de possíveis fatores bióticos e abióticos para investigar por que a cobertura vegetal mudou nos últimos ~ 70 anos na porção norte da península de Younghusband. Os resultados mostram que o declínio da abundância de coelhos exóticos, principalmente no início da década de 1950 após a introdução do vírus ix da Mixomatose, apresenta correlação significativa com períodos de maior crescimento da vegetação. Outros fatores, como a variabilidade do vento e da precipitação, não apresentaram correlação explicativa, levando à conclusão de que a redução dos coelhos foi o fator determinante mais importante do crescimento da vegetação no YP nesse período. A segunda parte deste estudo investiga as transformações geomorfológicas induzidas pelas mudanças da vegetação e como ocorreu a evolução de diferentes tipos de dunas, com o uso de imagens aéreas históricas e dados topográficos tridimensionais de alta resolução. De 1949 a 2018, o sistema de dunas passou por mudanças geomorfológicas significativas devido à estabilização da vegetação, com campos de dunas transgressivos ativos relativamente simples mudando para uma paisagem complexa de dunas parabólicas e cortes eólicos. O crescimento da vegetação nas depressões interdunares e planícies de deflação, formando corredores alongados e estreitos de vegetação, foi o principal mecanismo que levou ao desenvolvimento de uma série de cortes eólicos e dunas parabólicas, a maioria dos quais já se encontravam estabilizados em 2018. A terceira e última parte deste estudo investiga o papel de vários fatores que controlam a evolução das dunas frontais, responsáveis pelas diferenças geomorfológicas e volumétricas encontradas ao longo da linha de costa da porção sudeste da Península de Younghusband. Para este estudo, foi selecionado um trecho de 16 km de praia, onde mudanças ambientais mínimas ocorrem em relação a certos fatores, como energia eólica e transporte eólico. Os resultados mostram um aumento de sul para norte na altura e no volume das dunas frontais nos três anos pesquisados, juntamente com um aumento na x energia das ondas, enquanto outros fatores determinantes mostraram mudanças mínimas ou inexistentes. Essas descobertas indicam que a energia das ondas tem uma relação indireta positiva com a acumulação eólica das dunas frontais, sugerindo que as ondas têm um papel importante no suprimento de sedimentos em direção à praia, aumentando à medida que a energia das ondas sobe de sul para o norte. Nesta área de estudo, a energia das ondas tem um papel mais significativo do que as limitações de transporte eólico no desenvolvimento de dunas frontais (e dunas frontais relíquias).164 p.Fernandez, Guilherme BorgesHesp, Patrick AllanSilva, Graziela Miot daSilva, Cleverson GuizanGuedes, Carlos Conforti FerreiraSherman, DouglasDillenburg, Sérgio RebelloMoulton, Martim Almeida Braga2023-03-24T14:19:46Z2023-03-24T14:19:46Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/doctoralThesisapplication/pdfMOULTON, Martim Almeida Braga. Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul. 2019. 164 f. Tese (Doutorado em Geografia) – Programa de Pós-Graduação em Geografia, Instituto de Geociências, Universidade Federal Fluminense, Niterói, 2019.http://app.uff.br/riuff/handle/1/28323CC-BY-SAinfo:eu-repo/semantics/openAccessengreponame:Repositório Institucional da Universidade Federal Fluminense (RIUFF)instname:Universidade Federal Fluminense (UFF)instacron:UFF2023-03-24T14:19:49Zoai:app.uff.br:1/28323Repositório InstitucionalPUBhttps://app.uff.br/oai/requestriuff@id.uff.bropendoar:21202024-08-19T10:51:29.777710Repositório Institucional da Universidade Federal Fluminense (RIUFF) - Universidade Federal Fluminense (UFF)false |
dc.title.none.fl_str_mv |
Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul |
title |
Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul |
spellingShingle |
Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul Moulton, Martim Almeida Braga Coastal dunes Coastal geomorphology Vegetal cover Coastal processes Duna Zona costeira Geomorfologia Vegetação Dunas costeiras Geomorfologia costeira Cobertura vegetal Processos costeiros |
title_short |
Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul |
title_full |
Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul |
title_fullStr |
Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul |
title_full_unstemmed |
Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul |
title_sort |
Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul |
author |
Moulton, Martim Almeida Braga |
author_facet |
Moulton, Martim Almeida Braga |
author_role |
author |
dc.contributor.none.fl_str_mv |
Fernandez, Guilherme Borges Hesp, Patrick Allan Silva, Graziela Miot da Silva, Cleverson Guizan Guedes, Carlos Conforti Ferreira Sherman, Douglas Dillenburg, Sérgio Rebello |
dc.contributor.author.fl_str_mv |
Moulton, Martim Almeida Braga |
dc.subject.por.fl_str_mv |
Coastal dunes Coastal geomorphology Vegetal cover Coastal processes Duna Zona costeira Geomorfologia Vegetação Dunas costeiras Geomorfologia costeira Cobertura vegetal Processos costeiros |
topic |
Coastal dunes Coastal geomorphology Vegetal cover Coastal processes Duna Zona costeira Geomorfologia Vegetação Dunas costeiras Geomorfologia costeira Cobertura vegetal Processos costeiros |
description |
Coastal dune development and evolution has been one of the main research topics in coastal science (Martínez and Psuty, 2004). However, due to the complexity of the interactions between different driving factors that dictate coastal dune dynamics, the roles that each of the abiotic and biotic drivers play in formation and transformation of these deposits are still poorly understood (Provoost et al., 2011; Barchyn and Hugenholtz, 2012). In a historical time-scale (years to decades) dunefields can undergo significant morphological and ecological changes, shifting from an active/unvegetated state to a stabilized/vegetated state, and vice versa (Hesp, 2013). Studying how dunes evolve in a meso-scale analysis poses a significant challenge to researchers because of the difficulty in combining or obtaining spatial data with enough resolution over a significant period of time (Pickart and Hesp, 2019), and therefore studies that show medium to long-term dune changes are scarce (Hesp, 2013). In the Younghusband Peninsula dune system (South-east coast of South Australia), the availability of high-resolution historical spatial data, combined with climatic data, oceanographic data, and specific environmental conditions, constitutes a good opportunity to study different aspects of meso-scale morphological changes and their main driving factors. The objective of this body of work is to examine the different aspects of meso-scale driving factors of coastal dune dynamics, with the Younghusband Peninsula (YP) as a study case. This work investigates specifically: (1) What were the potential drivers of vegetation cover changes in the last ~70 years; (2) What were the geomorphological changes that occurred due to this vegetation cover vi changes and how did this morphological evolution take place; and (3) What are the main drivers that dictate the foredune morphological variability identified in the southern portion of the YP. The first part of this study (published in Earth Surface Processes and Landforms Journal – Moulton et al., 2019) uses historical aerial images and data from potential biotic and abiotic drivers to investigate why vegetation cover has changed in the last ~70 years in the northern YP. Results show that the decline in exotic rabbit abundance, especially in the 1950s after the introduction of the Myxomatosis virus, present significant correlation to periods of greater vegetation growth. Other factors, such as wind and precipitation variability, did not present any explanatory correlation, leading to the conclusion that rabbit grazing was the most important driving factor of vegetation growth in the YP during this period. The second part of this study investigates the geomorphological transformations induced by the vegetation changes and how the evolution of different dune types took place, with the use of historical aerial imagery and three-dimensional high-resolution topographic data. From 1949 to 2018, the dune system went through significant geomorphological changes due to vegetation stabilization, with relatively simple active transgressive dunefields changing into a complex landscape of active and vegetated blowout/parabolic dunes. Vegetation growth on the marginal interdune depressions and plains, forming narrow elongate vegetated ridges was the main process that lead to the development of a complex of blowouts and parabolic dunes, most of which are already stabilized by 2018. The third and final part of this study investigates the role of various factors controlling foredune evolution that accounts for the alongshore geomorphological vii and volumetric differences along the southeastern portion of the Younghusband Peninsula. For this study a 16 km stretch of beach on the barrier was selected, where minimal environmental changes in some factors such as wind energy and aeolian transport occur. Results show a south to north alongshore increase in foredune height and volume for the 3 years surveyed, together with an increase in wave energy, while other driving factors showed minimal to no changes. These findings indicate that wave energy has an indirect positive relationship with foredune accretion, with wave driven sediment supply to the beach increasing as wave energy rises from south to north. In this study area wave energy has more significant role than aeolian transport limitations on foredune (and relict foredune) development. |
publishDate |
2023 |
dc.date.none.fl_str_mv |
2023-03-24T14:19:46Z 2023-03-24T14:19:46Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/doctoralThesis |
format |
doctoralThesis |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
MOULTON, Martim Almeida Braga. Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul. 2019. 164 f. Tese (Doutorado em Geografia) – Programa de Pós-Graduação em Geografia, Instituto de Geociências, Universidade Federal Fluminense, Niterói, 2019. http://app.uff.br/riuff/handle/1/28323 |
identifier_str_mv |
MOULTON, Martim Almeida Braga. Drivers of coastal dune dynamics on the Younghusband Peninsula, South Australia = Fatores controladores da dinâmica de dunas costeiras na Península de Younghusband, Austrália do Sul. 2019. 164 f. Tese (Doutorado em Geografia) – Programa de Pós-Graduação em Geografia, Instituto de Geociências, Universidade Federal Fluminense, Niterói, 2019. |
url |
http://app.uff.br/riuff/handle/1/28323 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
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CC-BY-SA info:eu-repo/semantics/openAccess |
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CC-BY-SA |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
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reponame:Repositório Institucional da Universidade Federal Fluminense (RIUFF) instname:Universidade Federal Fluminense (UFF) instacron:UFF |
instname_str |
Universidade Federal Fluminense (UFF) |
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UFF |
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UFF |
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Repositório Institucional da Universidade Federal Fluminense (RIUFF) |
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Repositório Institucional da Universidade Federal Fluminense (RIUFF) |
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Repositório Institucional da Universidade Federal Fluminense (RIUFF) - Universidade Federal Fluminense (UFF) |
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riuff@id.uff.br |
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1811823590077628416 |