Editorial Board Members’Collection Series: Coastal Morphodynamics and Climate Change

A special issue of Journal of Marine Science and Engineering (ISSN 2077-1312). This special issue belongs to the section "Coastal Engineering".

Deadline for manuscript submissions: closed (15 January 2024) | Viewed by 3169

Special Issue Editors


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Guest Editor
Virginia Institute of Marine Science, College of William and Mary, Williamsburg, VA 23185, USA
Interests: science of collaboration; marine science; coastal morphodynamics; coastal resilience
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Guest Editor
Institute of Water and Environmental Engineering, Department of Hydraulic Engineering and Environment, School of Civil Engineering, Polytechnic University of Valencia, Valencia, Spain
Interests: climate change; water resources; watershed management; hydraulic engineering; renewable energies; coastal engineering; coastal management
Special Issues, Collections and Topics in MDPI journals

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Guest Editor
Coastal and Marine Research Centre, Griffith University, Gold Coast Campus, Southport, QLD 4215, Australia
Interests: coastal oceanography; coastal observations; sediment transport; estuaries; nearshore processes; coastal engineering; coastal erosion; climate change; coastal risk; sandy beach storm impacts; beach recovery; sea level variability; climate variability; coastal protection; beach nourishment; coastal management

Special Issue Information

Dear Colleagues,

The morphodynamics paradigm has been used over the past several decades to explain changes in the shape of the coast in terms of the mutually inter-dependent hydrodynamic, biologic, and anthropogenic processes; seafloor and landscape morphologies; and time-dependent sequences of change.  The shape of the coast and the processes that mold the coast change together as a complex system. There is constant feedback among the multiple components of the system and when the environmental conditions change, all facets of the system also change. The time scales of change range from hours to seasonal to decadal to millennial. Although progressive and sequential changes are the norm, abrupt shifts to different states can also take place when certain equilibrium thresholds are crossed. These abrupt “tipping points” often involve short-lived periods of positive feedback. A prominent example is the coupling of rapid warming of the Arctic with melting sea ice. Climate change is also causing an increasing frequency of “compound events”, such as storm surge combined with torrential rains or river floods. These events are superimposed on progressive rises in relative sea level and are anticipated to push many coastal morphodynamic systems to tipping points beyond which recovery may be impossible.  Complex systems modeling results are urgently needed to anticipate future coastal threats. Innovative engineering solutions will be needed to adapt to changes in coastal landscapes and environmental risks. For this Special Issue, papers on tipping points and cascading physical, ecological, socioeconomic effects, or multi-faceted complex systems are invited. Contributions based on observational or numerically modelled research, as well as review papers, regional case studies, and global projections are welcome.

Prof. Dr. Lynn Donelson Wright
Dr. Rafael J. Bergillos
Prof. Dr. Rodger Tomlinson
Guest Editors

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Keywords

  • coastal erosion
  • sea level rise
  • storm surge
  • coastal resilience
  • tipping points
  • model predictions
  • climate change impacts

Published Papers (1 paper)

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Review

20 pages, 1953 KiB  
Review
Coastal Morphodynamics and Climate Change: A Review of Recent Advances
by Lynn Donelson Wright and Bruce Graham Thom
J. Mar. Sci. Eng. 2023, 11(10), 1997; https://doi.org/10.3390/jmse11101997 - 17 Oct 2023
Cited by 2 | Viewed by 1720
Abstract
The shape of the coast and the processes that mold it change together as a complex system. There is constant feedback among the multiple components of the system, and when climate changes, all facets of the system change. Abrupt shifts to different states [...] Read more.
The shape of the coast and the processes that mold it change together as a complex system. There is constant feedback among the multiple components of the system, and when climate changes, all facets of the system change. Abrupt shifts to different states can also take place when certain tipping points are crossed. The coupling of rapid warming in the Arctic with melting sea ice is one example of positive feedback. Climate changes, particularly rising sea temperatures, are causing an increasing frequency of tropical storms and “compound events” such as storm surges combined with torrential rains. These events are superimposed on progressive rises in relative sea level and are anticipated to push many coastal morphodynamic systems to tipping points beyond which return to preexisting conditions is unlikely. Complex systems modeling results and long-term sets of observations from diverse cases help to anticipate future coastal threats. Innovative engineering solutions are needed to adapt to changes in coastal landscapes and environmental risks. New understandings of cascading climate-change-related physical, ecological, socioeconomic effects, and multi-faceted morphodynamic systems are continually contributing to the imperative search for resilience. Recent contributions, summarized here, are based on theory, observations, numerically modeled results, regional case studies, and global projections. Full article
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