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10.1016/J.COASTALENG.2019.103507

A rigorous calibration technique (the Generalised Likelihood Uncertainty Estimation) is applied to both models, using a comprehensive dataset of pre- and post-storm topographic measurements collected over four differing storm events at Narrabeen-Collaroy Beach in southeast Australia, as well as at two adjacent embayed beaches.

Calibration data requirements for modelling subaerial beach storm erosion

10.1016/J.COASTALENG.2019.04.004

Finally, several practical coastal engineering applications are presented, demonstrating the use of freely-available satellite imagery to monitor inter-annual embayed beach rotation, rapid storm-induced shoreline retreat and a major sand nourishment.

Sub-annual to multi-decadal shoreline variability from publicly available satellite imagery

10.3390/SU11030725

The objective of the present study is to achieve a better understanding of the possible rotation of embayed beaches using shoreline position data from two beaches on the central Tyrrhenian Sea (Italy) during a 64-year period.

Shoreline Rotation Analysis of Embayed Beaches by Means of In Situ and Remote Surveys

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10.1016/J.GEOMORPH.2019.06.020

Here, for the first time, we employ a total sediment budget approach, examining a sandy and embayed beach located in the north coast of SW England, to investigate inter- and multi-annual embayment scale sediment dynamics over a 10-year period that includes extreme storm erosion and post-storm recovery.

Multi-annual embayment sediment dynamics involving headland bypassing and sediment exchange across the depth of closure

10.1016/j.geomorph.2019.106856

Embayed beaches are widely distributed around the world.

Shoreline evolution in an embayed beach adjacent to tidal inlet: The impact of anthropogenic activities

10.1016/J.MARGEO.2019.02.004

Globally, embayed beaches are common to hilly and mountainous coastlines.

Morphometric classification of swell-dominated embayed beaches

10.3390/JMSE7060177

The majority of these sites were found within the central to southern half of the state, behind embayed beaches, and within leaky sediment compartments, or those that have estuarine sinks.

Interdecadal Foredune Changes along the Southeast Australian Coastline: 1942–2014

10.1016/J.OCECOAMAN.2019.01.001

Embayed beaches play an important role in ensuring the environmental and morphological sustenance of coastal areas.

Shoreline management plan for embayed beaches: A case study at Vengurla, west coast of India

10.1016/J.ECSS.2019.106244

However, the prediction and quantification of wave runup on embayed beaches is strongly influenced by particular characteristics (e.

Exploiting remote imagery in an embayed sandy beach for the validation of a runup model framework

10.1016/J.MARGEO.2018.10.009

This work illustrates the importance of tidal currents in depth of closure calculations and challenges the notion that embayed beaches are generally closed cells, as headland bypassing may be more wide spread than commonly assumed along exposed coastlines globally.

Role of waves and tides on depth of closure and potential for headland bypassing

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Embayed Beach - A rigorous calibration technique (the Generalised Likelihood Uncertainty Estimation) is applied to both models, using a comprehensive dataset of pre- and post-storm topographic measurements collected over four differing storm events at Narrabeen-Collaroy Beach in southeast Australia, as well as at two adjacent embayed beaches. [1] Finally, several practical coastal engineering applications are presented, demonstrating the use of freely-available satellite imagery to monitor inter-annual embayed beach rotation, rapid storm-induced shoreline retreat and a major sand nourishment. [2] The objective of the present study is to achieve a better understanding of the possible rotation of embayed beaches using shoreline position data from two beaches on the central Tyrrhenian Sea (Italy) during a 64-year period. [3] Here, for the first time, we employ a total sediment budget approach, examining a sandy and embayed beach located in the north coast of SW England, to investigate inter- and multi-annual embayment scale sediment dynamics over a 10-year period that includes extreme storm erosion and post-storm recovery. [4] Embayed beaches are widely distributed around the world. [5] Globally, embayed beaches are common to hilly and mountainous coastlines. [6] The majority of these sites were found within the central to southern half of the state, behind embayed beaches, and within leaky sediment compartments, or those that have estuarine sinks. [7] Embayed beaches play an important role in ensuring the environmental and morphological sustenance of coastal areas. [8] However, the prediction and quantification of wave runup on embayed beaches is strongly influenced by particular characteristics (e. [9] This work illustrates the importance of tidal currents in depth of closure calculations and challenges the notion that embayed beaches are generally closed cells, as headland bypassing may be more wide spread than commonly assumed along exposed coastlines globally. [10]