28 results on '"Vieira da Silva, Guilherme"'
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2. Sediment pathways and morphodynamic response to a multi-purpose artificial reef – New insights
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Vieira da Silva, Guilherme, Hamilton, Daniel, Strauss, Darrell, Murray, Thomas, and Tomlinson, Rodger
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- 2022
- Full Text
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3. Building coastal resilience via sand backpassing - A framework for developing a decision support tool for sand management
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Vieira da Silva, Guilherme, Strauss, Darrell, Murray, Thomas, Tomlinson, Rodger, Taylor, Joshua, and Prenzler, Paul
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- 2021
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4. The role of cuspate spits on wave attenuation and energy redistribution in a coastal lagoon, Lagoa dos Patos, Brazil
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Malheiros Miranda, Inaiê, Toldo, Jr, Elírio Ernestino, da Fontoura Klein, Antonio Henrique, Strauss, Darrell, and Vieira da Silva, Guilherme
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- 2020
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5. Headland bypassing and overpassing: form, processes and applications
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Klein, Antonio H.F., primary, Vieira da Silva, Guilherme, additional, Taborda, Rui, additional, da Silva, Ana P., additional, and Short, Andrew D., additional
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- 2020
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6. Contributors
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Aarninkhof, Stefan, primary, Ashton, Andrew D., additional, Baldock, Tom E., additional, Beuzen, Tom, additional, Bosboom, Judith, additional, R. Bryan, Karin, additional, Burningham, Helene, additional, Castelle, Bruno, additional, Coco, Giovanni, additional, Vila-Concejo, Ana, additional, da Silva, Ana P., additional, de Vries, Sierd, additional, den Heijer, Kees, additional, Fernandez-Nunez, Miriam, additional, Ferreira, Óscar, additional, Flemming, Burghard, additional, Gallop, Shari L., additional, Gawehn, Matthijs, additional, Gómez-Pujol, Lluís, additional, D. Goodwin, Ian, additional, Guisado-Pintado, Emilia, additional, Harley, Mitchell, additional, Houser, Chris, additional, Hughes, Michael G., additional, J. Hein, Christopher, additional, Jackson, Derek W.T., additional, Klein, Antonio H.F., additional, López-Ruiz, Alejandro, additional, Largier, John L., additional, Lee, Mark, additional, Locknick, Summer, additional, Losada, Miguel Á., additional, Loureiro, Carlos, additional, Luijendijk, Arjen, additional, J. Méndez, Fernando, additional, Mortlock, Thomas, additional, Murray, Brad, additional, Orfila, Alejandro, additional, Ortega-Sánchez, Miguel, additional, Pereira, Luci, additional, Power, Hannah E., additional, Ribó, Marta, additional, Rueda, Ana, additional, Ruiz de Alegría-Arzaburu, Amaia, additional, Senechal, Nadia, additional, Short, Andrew D., additional, Splinter, Kristen, additional, Taborda, Rui, additional, Thom, Bruce, additional, Ton, Anne, additional, Trimble, Sarah, additional, Trindade, Wellington, additional, Vieira da Silva, Guilherme, additional, Vos, Sander, additional, Walker, Ian J., additional, Wengrove, Meagan, additional, Wernette, Phil, additional, and Winter, Gundula, additional
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- 2020
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7. The influence of wave-, wind- and tide-forced currents on headland sand bypassing – Study case: Santa Catarina Island north shore, Brazil
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Vieira da Silva, Guilherme, Toldo Jr., Elírio E., Klein, Antonio H. da F., and Short, Andrew D.
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- 2018
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8. Investigating Nearshore Morphodynamics Response to Extreme Storms and Storm Groups
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Zhang, Hong, Vieira da Silva, Guilherme, Oo, Ye Htet, Zhang, Hong, Vieira da Silva, Guilherme, and Oo, Ye Htet
- Abstract
Combating coastal erosion is becoming increasingly challenging due to population growth near beaches, and the dynamic nature of nearshore morphological processes. Along a zeta-shaped coastline, such as Gold Coast in Australia, the degree of exposure of the beaches to waves varies alongshore depending on the incident wave direction. Since waves are one of the main drivers of sediment transport along the coast, changing wave direction can disturb the modal sediment transport. This phenomenon can cause localised erosion, and it is therefore important to quantify the impact at different locations along the coast. By doing so, effective coastal protection strategies can be developed to ensure the resilience of coastal communities. Recent studies have reported changes in wave climate (e.g., frequency and intensity of storms, shifts in wave direction) in response to climate change, making coasts more vulnerable to unusual waves. In addition to the waves, water levels play an important role in beach erosion, and the non-astronomical component of water levels (i.e., surge) presents a correlation with wave height during extreme storm events. Moreover, storm groups, where beach recovery is near zero between successive storms, may further increase erosion along the coast. Therefore, an investigation of the impact of waves, surge, and storm groups is important for effective coastal management. In this context, this study aimed to understand the beach response to extreme storms and storm groups on a zeta-shaped open coastline. This was achieved through analysis of (i) storm wave fields using different boundary forcing to study the wave transformations from offshore to nearshore, (ii) extreme joint probability of significant wave height and water level, and (iii) the response of different antecedent beach profiles induced by a storm group and its order. A numerical modelling approach was used, incorporating a spectral wave model and a morphological model for wave and beach erosion, Thesis (PhD Doctorate), Doctor of Philosophy (PhD), School of Eng & Built Env, Science, Environment, Engineering and Technology, Full Text
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- 2023
9. Headland sand bypassing — Quantification of net sediment transport in embayed beaches, Santa Catarina Island North Shore, Southern Brazil
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Vieira da Silva, Guilherme, Toldo, Elírio E., Jr, Klein, Antonio H. da F., Short, Andrew D., and Woodroffe, Colin D.
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- 2016
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10. Longshore sediment transport variability changes by the end of the 21st century.
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Vieira da Silva, Guilherme, Strauss, Darrell, Murray, Thomas, Alvarez, Fernando, Hemer, Mark, and Meucci, Alberto
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SEDIMENT transport ,COASTAL engineering ,COASTAL ecology ,COASTS - Abstract
Projections of wave climate for the Gold Coast, Queensland suggest a reduction in wave height combined with an anticlockwise shift in wave direction which may lead to an overall local reduction in longshore sediment transport (LST). Understanding changes in LST variability into the future is crucial to better manage the coastline and prepare for future adaptation pathways. The aim of this paper is to analyse the variability of LST at the end of the 21st century and the implications it may have on coastal management. To do so, a benchmark model was established to assess the LST along the entire coast by using a Delft3D model, where boundary conditions are derived from a global wave hindcast forced with the Climate Forecast System Reanalysis (CFSR). The Delft3D model was calibrated using the pumping rates of an artificial sand bypassing system at the northern Gold Coast for three representative years encompassing: low (2004), average (2001) and high (2003) LST rates. Then a hybrid wave downscaling technique was applied to obtain the wave data at the breaking point at three locations along the coast where the Coastal Engineering Research Center (CERC) equation was calibrated based on the benchmark model. Finally, future wave climate scenarios (Contributions to the Coordinated Ocean Wave Climate Project, COWCliP) derived from CMIP5 (seven GCMs) and CMIP6 (two GCMs) were bias-corrected and used to generate ensembles to analyse future projected changes in the variability of LST along the Gold Coast by comparing historical and future projection model runs. The changes in interannual variability projections are inconclusive with the CMIP5 ensemble indicating a decrease in LST interannual variability while the CMIP6-derived models (ensemble with two members) indicate an increase. To allow for a fair comparison, more models to compose the CMIP6 ensemble are required. As for the seasonal variability, CMIP5-derived models suggest a decrease in LST between February and May and virtually no changes for the rest of the year, decreasing the seasonal variability in LST. Changes in LST and its variability may have flow-on effects for coastal management with changes to the creek dredging programs, potentially reduced input to the by- and back-passing systems on the coast and the dispersion of beach nourishment campaigns. [ABSTRACT FROM AUTHOR]
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- 2023
11. Shoreline Response to the Southern Annular Mode at WEC site: Satellite Analysis.
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Thompson, James, Cartwright, Nick, Etemad-Shahidi, Amir, Vieira da Silva, Guilherme, and O'Grady, Julian
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SHORELINES ,COASTAL ecology ,COASTAL engineering ,CONSTRUCTION contracts ,CLIMATE change - Abstract
Understanding shoreline dynamics is a key step towards the successful management of coastal environments. This study investigates natural shoreline variability at Grassy Beach, focusing on the relationship to the Southern Annular Mode (SAM) climate driver. The present analysis contributes to ongoing investigations into the influence of a nearshore wave energy converter (WEC), installed in 2021, on the local shoreline dynamics. Grassy Beach is a sandy embayment on the southeast coast of King Island in Bass Strait, Australia, with a wave climate dominated by southerly refracted Southern Ocean swells. Shoreline position from 1987 to 2021 (pre-WEC deployment) was determined from 420 Sentinel and Landsat satellite images using the CoastSat Python toolkit. Empirical orthogonal function (EOF) analysis found a seasonal beach rotation signal to be a dominant mode of variability (20% of total variability). The corresponding temporal EOF alternated in sign between winter and summer. These results show shoreline retreat (erosion) occurring in winter at the exposed eastern end and during summer at the western end when waves from the east increase in frequency. The Bass Strait wave climate is influenced by SAM, with more powerful waves likely in Austral autumn and winter when the SAM index is positive. A positive phase of SAM during winter was found to increase shoreline retreat at the eastern end leading to a stronger beach rotation signal describing 24% of the total variability. These results provide new insights into the influence of SAM on shoreline dynamics and highlight the importance of considering relevant climate drivers as an indicator of beach erosion. For nearshore structures such as WECs, it is critical to first assess the site's natural variability and relevant driving factors through a multi-decade spatiotemporal analysis before analysing the coastal impact of such structures. [ABSTRACT FROM AUTHOR]
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- 2023
12. Morphological Response of Submerged Structures on a Highly Dynamic Wave Dominated Beach.
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Strauss, Darrell, Vieira da Silva, Guilherme, Murray, Tom, Mingyuan Ma, Faivre, Gaëlle, Angenent, Evanne, and Alvarez, Fernando
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COASTAL engineering ,COASTAL development ,METEOROLOGY ,WAVES (Physics) - Abstract
Multi-purpose submerged coastal protection structures are increasingly being considered on sandy wave dominated coasts for their relatively low impact on visual and beach amenity compared to traditional emerged structural works such as breakwaters. However, knowledge of submerged coastal protection structure attributes, with respect to their impact on morphological responses, is scarce, mainly due to the difficulty in predicting outcomes in dynamic environments and a reliance on expensive laboratory or numerical modelling experiments combined with a general lack of in-situ monitoring data. The design and performance of multi-purpose submerged coastal protection structures for coastal protection and surf amenity is assessed here using a process-based model. The model is supported by field measurements used to calibrate models of two existing Gold Coast artificial reefs and nearshore beach nourishments and their morphological evolution. Twenty-five scenarios with varying crest width, shape, depth and distance offshore were tested to identify key physical parameters for the effective and efficient design of submerged nearshore protection structures. The open coast beach of the northern Gold Coast was used as a case study site however this research methodology can be used to inform coastal protection strategies for other wave-dominated, sandy beach coastlines with similar geology, geomorphology, tide and wave climate. The impacts of the submerged structures on nearshore waves, hydrodynamics and morphology were determined in several key areas such as the lee of the structure, updrift and downdrift active profile regions. The results demonstrate that validated morphological models can be applied with increasing confidence to develop evidence-based guidelines for defining the key planning, design, and structural parameters of nearshore coastal protection structures to achieve effective coastal protection and enhanced recreational amenity outcomes. [ABSTRACT FROM AUTHOR]
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- 2023
13. A Coastal Erosion Risk Assessment Framework.
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Alvarez, Fernando, De Lucia, Liam, Vieira da Silva, Guilherme, and Javernig, Beau
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EROSION ,RISK assessment ,COASTAL zone management ,CLIMATE change ,COASTAL engineering ,METEOROLOGY - Abstract
With the increased pressure on the coastlines including population growth, development of new infrastructure, wave pattern changes and sea level rise due to climate change, coastal erosion is likely to continue to be one of the primary concerns for coastal communities and coastal managers during the next years and decades. The Gold Coast City Council (City) manages over 50 km of coastline while receiving over 5 million visitors per year and is one of the fastest growing cities in Australia. While often the magnitude of coastal erosion is difficult to predict and manage, the City is developing a framework to monitor beach erosion and assess erosion risk based on a comprehensive coastal monitoring program including hydrographic surveying, shoreline monitoring using video cameras, asset mapping, numerical modelling, consultancy studies and scientific research. To do so, the methodology was divided into six steps: 1) the latest survey is used to define the current beach condition; 2) a series of pre-computed XBeach simulations are used to define expected storm demands for different wave Average Return Intervals (ARI); 3) ARGUS-derived beach widths are used to incorporate the long-term trends; 4) sand volumes stored on the bar are also accounted for, based on the surveys; 5) locations of specific built assets are incorporated; 6) climate change shoreline retreat is included. A score is provided for each section based on their ability to withstand a 5-year ARI storm and a 50-year ARI storm. The outputs of this framework will be used to inform maintenance operations as well as management and strategic decisions. [ABSTRACT FROM AUTHOR]
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- 2023
14. Utilising object detection from coastal surf cameras to assess surfer usage.
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Murray, Thomas P., Greaves, Megan C., Vieira da Silva, Guilherme, Boyle, Oliver J., Wynne, Ketron, Freeston, Ben, Ditria, Luke, Jardine, Paul, Ditria, Ellen, Strauss, Darrell, Tomlinson, Rodger, and Burton, Paul
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SURFING ,COASTAL zone management ,ATMOSPHERIC temperature ,BEACHES - Abstract
Surfing is an increasingly popular sport and recreation that holds significant socio-cultural and economic value for coastal communities worldwide. Recently, coastal cities such as the Gold Coast, Australia have acknowledged the importance of surfing in their local and regional coastal management. As such, the collection of surfer usage data is becoming increasingly important for informed policy decision making. For the first time surfer usage data is collected via a commercial coastal camera network and machine learning object detection techniques. The study site, Currumbin Alley, Gold Coast is a highly valued surf break and services both an advanced point break and inner learner wave. SurfzoneAI, a proprietary machine learning model was applied to 2593 hours (245 days) of video footage from a coastal camera at the site to collect surfer usage data. SurfzoneAI detection outputs for detection class 'surfers surfing' were combined with the open source Simple Online and Realtime Tracking (SORT) tool, to provide surfing ride count and duration data. The artificial intelligence (AI) model detections performed well (> 80% accuracy) for surfer count and surfing ride count data. Approximately 99,000 individual surfing visits were captured along with 617,000 surfing rides. This equated to an estimate of around six to seven surfing waves per visitor. Surfer usage varied throughout the day with visitation increasing through the morning (4-10am) to peak around 10-11am, drop slightly through lunch (12-3pm), a slight uptick in the late afternoon (4-5pm) before dropping again into the evening (5-7pm). As would be expected, there was a significantly higher number of average surfer visitors per hour on the weekends (46) as opposed to weekdays (25). There were no clear linear relationships between environmental data and surfer usage. Average ride durations at Currumbin Alley were of the order of 9-10 seconds which is higher than nearby reef and beach breaks. Future work will focus on improving the machine learning outputs, georectification of surfing rides and further exploration of environmental variables on surfer usage through multivariate statistics. Overall the study showed the usefulness of leveraging off existing commercial coastal camera networks to collect surfer usage data and the power of the AI dataset for informed policy decision making. [ABSTRACT FROM AUTHOR]
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- 2023
15. GAMIFIED APP THAT MAPS COLLECTION POINTS AND PLACES OF ACCUMULATING SOLID WASTE IN THE URBAN ENVIRONMENT OF THE CITY OF MANAUS (AMAZONAS)
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Guedes Da Silva, Leonardo, primary, Otavio Pereira Da Silva, Luiz, additional, Mark Lobo De Oliveira, Jean, additional, and Vieira Da Silva, Guilherme, additional
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- 2022
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16. Estimation of beach erosion using Joint Probability analysis with a morphological model
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Oo, Ye Htet, primary, Vieira Da Silva, Guilherme, additional, Zhang, Hong, additional, Strauss, Darrell, additional, and Tomlinson, Rodger, additional
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- 2022
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17. Climate Control on Natural Headland Bypassing
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Strauss, Darrell R, Vieira da Silva, Guilherme, Tomlinson, Rodger B, Da Silva, Ana Paula, Strauss, Darrell R, Vieira da Silva, Guilherme, Tomlinson, Rodger B, and Da Silva, Ana Paula
- Abstract
This thesis aims to characterize the headland bypassing mechanism in a natural environment and investigate its variability relating it to the potential weather types and climate indices that influence the regional wave climate. The research is focused on Fingal Head (New South Wales, Australia), due to its natural cycles and relevance for regional coastal management. The analysis consists of three main stages: (1) describing the morphological variability updrift and downdrift of the headland, in different timescales through short-term topo-bathymetric surveys from 2018 to 2020 and long-term remote-sensing of shoreline and sandbar position from 1987 to 2020; (2) identifying the distinct atmospheric patterns and climate indices over the last decades associated with the main controlling factors of the sand bypassing in the study area and, (3) simulating headland bypassing events through numerical modelling in order to understand how the specific sea-state generated by the atmospheric systems leads to the triggering of a bypassing pulse. Results revealed that headland bypassing around Fingal Head is governed by two distinct processes controlled by the wave conditions and sediment availability. The sandbar-driven bypassing requires storm waves reaching the study area from southeast in order to trigger the sandbar-trough system formation around the headland while the sediment leaking process develops from similar wave direction approaching the coast but under lower wave heights. Strong low-pressure systems (e.g., Tropical Cyclones and East Coast Lows) positioned in the midlatitudes of the Coral-Tasman Sea basin were observed to generate the ideal sea-states for triggering a bypassing pulse around Fingal Head. The pulses triggered by this weather types have occurred at least 19 times in 33 years, which suggests 1 to 2 years cycles between bypassing events. The variability of the relevant weather types did not show a relationship with climate drivers; however, over a longer, Thesis (PhD Doctorate), Doctor of Philosophy (PhD), School of Eng & Built Env, Science, Environment, Engineering and Technology, Full Text
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- 2022
18. Camacho inlet southern Brazil – Instability causes and user conflicts
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Vieira da Silva, Guilherme, de Carvalho, João Luiz Baptista, and da Fontoura Klein, Antonio Henrique
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- 2011
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19. Headland bypassing timescales: Processes and driving forces
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Silva, Ana Paula da, primary, Vieira da Silva, Guilherme, additional, Strauss, Darrell, additional, Murray, Thomas, additional, Woortmann, Lorena G., additional, Taber, Jonathan, additional, Cartwright, Nick, additional, and Tomlinson, Rodger, additional
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- 2021
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20. 23 - Headland bypassing and overpassing: form, processes and applications
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Klein, Antonio H.F., Vieira da Silva, Guilherme, Taborda, Rui, da Silva, Ana P., and Short, Andrew D.
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- 2020
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21. 15 Priorities for Wind-Waves Research: An Australian Perspective
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Greenslade, Diana, Hemer, Mark, Babanin, Alex, Lowe, Ryan, Turner, Ian, Power, Hannah, Young, Ian, Ierodiaconou, Daniel, Hibbert, Greg, Williams, Greg, Aijaz, Saima, Albuquerque, Joao, Allen, Stewart, Banner, Michael, Branson, Paul, Buchan, Steve, Burton, Andrew, Bye, John, Cartwright, Nick, Chabchoub, Amin, Colberg, Frank, Contardo, Stephanie, Dufois, Francois, Earl-spurr, Craig, Farr, David, Goodwin, Ian, Gunson, Jim, Hansen, Jeff, Hanslow, David, Harley, Mitchell, Hetzel, Yasha, Hoeke, Ron, Jones, Nicole, Kinsela, Michael, Liu, Qingxiang, Makarynskyy, Oleg, Marcollo, Hayden, Mazaheri, Said, Mcconochie, Jason, Millar, Grant, Moltmann, Tim, Moodie, Neal, Morim, Joao, Morison, Russel, Orszaghova, Jana, Pattiaratchi, Charitha, Pomeroy, Andrew, Proctor, Roger, Provis, David, Reef, Ruth, Rijnsdorp, Dirk, Rutherford, Martin, Schulz, Eric, Shayer, Jake, Splinter, Kristen, Steinberg, Craig, Strauss, Darrell, Stuart, Greg, Symonds, Graham, Tarbath, Karina, Taylor, Daniel, Taylor, James, Thotagamuwage, Darshani, Toffoli, Alessandro, Valizadeh, Alireza, Van Hazel, Jonathan, Vieira Da Silva, Guilherme, Wandres, Moritz, Whittaker, Colin, Williams, David, Winter, Gundula, Xu, Jiangtao, Zhong, Aihong, Zieger, Stefan, Greenslade, Diana, Hemer, Mark, Babanin, Alex, Lowe, Ryan, Turner, Ian, Power, Hannah, Young, Ian, Ierodiaconou, Daniel, Hibbert, Greg, Williams, Greg, Aijaz, Saima, Albuquerque, Joao, Allen, Stewart, Banner, Michael, Branson, Paul, Buchan, Steve, Burton, Andrew, Bye, John, Cartwright, Nick, Chabchoub, Amin, Colberg, Frank, Contardo, Stephanie, Dufois, Francois, Earl-spurr, Craig, Farr, David, Goodwin, Ian, Gunson, Jim, Hansen, Jeff, Hanslow, David, Harley, Mitchell, Hetzel, Yasha, Hoeke, Ron, Jones, Nicole, Kinsela, Michael, Liu, Qingxiang, Makarynskyy, Oleg, Marcollo, Hayden, Mazaheri, Said, Mcconochie, Jason, Millar, Grant, Moltmann, Tim, Moodie, Neal, Morim, Joao, Morison, Russel, Orszaghova, Jana, Pattiaratchi, Charitha, Pomeroy, Andrew, Proctor, Roger, Provis, David, Reef, Ruth, Rijnsdorp, Dirk, Rutherford, Martin, Schulz, Eric, Shayer, Jake, Splinter, Kristen, Steinberg, Craig, Strauss, Darrell, Stuart, Greg, Symonds, Graham, Tarbath, Karina, Taylor, Daniel, Taylor, James, Thotagamuwage, Darshani, Toffoli, Alessandro, Valizadeh, Alireza, Van Hazel, Jonathan, Vieira Da Silva, Guilherme, Wandres, Moritz, Whittaker, Colin, Williams, David, Winter, Gundula, Xu, Jiangtao, Zhong, Aihong, and Zieger, Stefan
- Abstract
The Australian marine research, industry, and stakeholder community has recently undertaken an extensive collaborative process to identify the highest national priorities for wind-waves research. This was undertaken under the auspices of the Forum for Operational Oceanography Surface Waves Working Group. The main steps in the process were first, soliciting possible research questions from the community via an online survey; second, reviewing the questions at a face-to-face workshop; and third, online ranking of the research questions by individuals. This process resulted in 15 identified priorities, covering research activities and the development of infrastructure. The top five priorities are 1) enhanced and updated nearshore and coastal bathymetry; 2) improved understanding of extreme sea states; 3) maintain and enhance the in situ buoy network; 4) improved data access and sharing; and 5) ensemble and probabilistic wave modeling and forecasting. In this paper, each of the 15 priorities is discussed in detail, providing insight into why each priority is important, and the current state of the art, both nationally and internationally, where relevant. While this process has been driven by Australian needs, it is likely that the results will be relevant to other marine-focused nations.
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- 2020
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22. Priorities for Wind-Waves Research
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Greenslade, Diana, primary, Hemer, Mark, additional, Babanin, Alex, additional, Lowe, Ryan, additional, Turner, Ian, additional, Power, Hannah, additional, Young, Ian, additional, Ierodiaconou, Daniel, additional, Hibbert, Greg, additional, Williams, Greg, additional, Aijaz, Saima, additional, Albuquerque, João, additional, Allen, Stewart, additional, Banner, Michael, additional, Branson, Paul, additional, Buchan, Steve, additional, Burton, Andrew, additional, Bye, John, additional, Cartwright, Nick, additional, Chabchoub, Amin, additional, Colberg, Frank, additional, Contardo, Stephanie, additional, Dufois, Francois, additional, Earl-Spurr, Craig, additional, Farr, David, additional, Goodwin, Ian, additional, Gunson, Jim, additional, Hansen, Jeff, additional, Hanslow, David, additional, Harley, Mitchell, additional, Hetzel, Yasha, additional, Hoeke, Ron, additional, Jones, Nicole, additional, Kinsela, Michael, additional, Liu, Qingxiang, additional, Makarynskyy, Oleg, additional, Marcollo, Hayden, additional, Mazaheri, Said, additional, McConochie, Jason, additional, Millar, Grant, additional, Moltmann, Tim, additional, Moodie, Neal, additional, Morim, Joao, additional, Morison, Russel, additional, Orszaghova, Jana, additional, Pattiaratchi, Charitha, additional, Pomeroy, Andrew, additional, Proctor, Roger, additional, Provis, David, additional, Reef, Ruth, additional, Rijnsdorp, Dirk, additional, Rutherford, Martin, additional, Schulz, Eric, additional, Shayer, Jake, additional, Splinter, Kristen, additional, Steinberg, Craig, additional, Strauss, Darrell, additional, Stuart, Greg, additional, Symonds, Graham, additional, Tarbath, Karina, additional, Taylor, Daniel, additional, Taylor, James, additional, Thotagamuwage, Darshani, additional, Toffoli, Alessandro, additional, Valizadeh, Alireza, additional, van Hazel, Jonathan, additional, Vieira da Silva, Guilherme, additional, Wandres, Moritz, additional, Whittaker, Colin, additional, Williams, David, additional, Winter, Gundula, additional, Xu, Jiangtao, additional, Zhong, Aihong, additional, and Zieger, Stefan, additional
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- 2020
- Full Text
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23. 15 Priorities for Wind-Waves Research: An Australian Perspective
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Greenslade, Diana, primary, Hemer, Mark, additional, Babanin, Alex, additional, Lowe, Ryan, additional, Turner, Ian, additional, Power, Hannah, additional, Young, Ian, additional, Ierodiaconou, Daniel, additional, Hibbert, Greg, additional, Williams, Greg, additional, Aijaz, Saima, additional, Albuquerque, João, additional, Allen, Stewart, additional, Banner, Michael, additional, Branson, Paul, additional, Buchan, Steve, additional, Burton, Andrew, additional, Bye, John, additional, Cartwright, Nick, additional, Chabchoub, Amin, additional, Colberg, Frank, additional, Contardo, Stephanie, additional, Dufois, Francois, additional, Earl-Spurr, Craig, additional, Farr, David, additional, Goodwin, Ian, additional, Gunson, Jim, additional, Hansen, Jeff, additional, Hanslow, David, additional, Harley, Mitchell, additional, Hetzel, Yasha, additional, Hoeke, Ron, additional, Jones, Nicole, additional, Kinsela, Michael, additional, Liu, Qingxiang, additional, Makarynskyy, Oleg, additional, Marcollo, Hayden, additional, Mazaheri, Said, additional, McConochie, Jason, additional, Millar, Grant, additional, Moltmann, Tim, additional, Moodie, Neal, additional, Morim, Joao, additional, Morison, Russel, additional, Orszaghova, Jana, additional, Pattiaratchi, Charitha, additional, Pomeroy, Andrew, additional, Proctor, Roger, additional, Provis, David, additional, Reef, Ruth, additional, Rijnsdorp, Dirk, additional, Rutherford, Martin, additional, Schulz, Eric, additional, Shayer, Jake, additional, Splinter, Kristen, additional, Steinberg, Craig, additional, Strauss, Darrell, additional, Stuart, Greg, additional, Symonds, Graham, additional, Tarbath, Karina, additional, Taylor, Daniel, additional, Taylor, James, additional, Thotagamuwage, Darshani, additional, Toffoli, Alessandro, additional, Valizadeh, Alireza, additional, van Hazel, Jonathan, additional, Vieira da Silva, Guilherme, additional, Wandres, Moritz, additional, Whittaker, Colin, additional, Williams, David, additional, Winter, Gundula, additional, Xu, Jiangtao, additional, Zhong, Aihong, additional, and Zieger, Stefan, additional
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- 2020
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24. Comunicação pública da ciência por meio da exposição “Plataforma Zebrafish: a construção de uma red”
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Lopes Ferreira, Mônica, primary, Vieira da Silva, Guilherme, primary, and Almeida, Adriana, primary
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- 2019
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25. Longshore wave variability along non-straight coastlines
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Vieira Da Silva, Guilherme, primary, Murray, Thomas, additional, and Strauss, Darrell, additional
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- 2018
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26. Shoreline change analysis and insight into the sediment transport path along Santa Catarina Island north shore, Brazil
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Vieira da Silva, Guilherme, Muler, Mariela, Prado, Michel F. V, Short, Andrew D, da Fontoura Klein, Antonio Henrique, Toldo, Elirio E, Vieira da Silva, Guilherme, Muler, Mariela, Prado, Michel F. V, Short, Andrew D, da Fontoura Klein, Antonio Henrique, and Toldo, Elirio E
- Abstract
This paper presents a shoreline change analysis applied to identify the sediment transport path involving nine adjoining beaches, including dunes and spits, located along the microtidal eastern and northern shores of Santa Catarina Island (Brazil) and extending 50 km from Barra-Moçambique to Daniela. A data set was comprised of aerial images from 1957, 1978, 1998, 2002, 2007, and 2010, and the 2012 shoreline position measured with real-time kinematic GPS, topobathymetric data set, and a 60-year water-level time series. The images were rectified and the shoreline position for each year was extracted. The average errors (ranging from 1 to 9.8 m) of the rectification process as well as the horizontal tide-related errors (varying from 8.3 ± 2.6 m to 14.9 ± 0.6 m) were calculated within a confidence level of 95%. Two complementary approaches were used: (1) general trends analysis using linear regression rate method and (2) shoreline behaviour statistically analysed by Euclidean distance and year-to-year analysis. The results indicate an anticlockwise longshore transport between a series of beaches with variable orientation and separated by headlands, including a dune overpassing from Santinho delivering ∼10,000 m3 y−1 to Ingleses, and headland bypassing leading to the development of three spits along the protected part of the study area that have possibly been nourished by subaqueous sand transport from the updrift beaches. During its development the Ponta das Canas spit grew ∼7000 m3 y−1, controlling the sediment availability downdrift. As the spit grows it traps sediment and the downdrift area retreats; on the other hand, when the spit merges to the coast the sand spreads and the downdrift beaches prograde.
- Published
- 2016
27. Wave run-up on embayed beaches. Study case: Itapocorói Bay, Southern Brazil.
- Author
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Vieira da Silva, Guilherme, Gomes da Silva, Paula, Sangoi Araujo, Rafael, Henrique da Fontoura Klein, Antonio, and Toldo Jr., Elírio E.
- Subjects
BEACH erosion ,COASTAL processes (Physical geology) ,FLOODS ,COASTAL zone management ,BEACHES - Abstract
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- Published
- 2017
- Full Text
- View/download PDF
28. Qualidade de ovos de galinha comercializados em Barreiras, BA, estocados em diferentes condições de temperatura
- Author
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Gusmão de Quadros, Danilo, primary, Ribeiro de Jesus, Thiago, additional, Hideo Kanematsu, Carlos, additional, Magalhães de Sá, Alberto, additional, Vieira da Silva, Guilherme Augusto, additional, Rocha da Silva, Anderson Luiz, additional, and Pereira Andrade, Alexandro, additional
- Published
- 2011
- Full Text
- View/download PDF
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