As the statistics of storms (tropical and extra-tropical)
shift with global warming, the wave climates affecting coastlines will
shift. In response, we can expect coastline shapes to change—with
associated intensification and changing locations of large-scale
shoreline erosion zones. Observations from the cuspate capes of the
Carolina coastline, USA, where a shift in wave statistics has been
documented, provide a test of this prediction. Along underdeveloped
cape shorelines, the difference between historic and recent shoreline
change patterns conforms to model predictions. However, on the
developed Cape Fear, long-term shoreline stabilization (through beach
nourishment) precludes the predicted changes in coastline shape. In
this location, model experiments coupled with observations of cumulative
beach-nourishment sand volumes indicates that the response to climate
change exists within the human component of the coupled human/natural
system.
Because shoreline stabilization decisions, made in response to coastline
changes, affect large-scale coastline change, the present and future
evolution of developed coastlines results from coupled physical and human
dynamics. Coupling economic and coastline-evolution models leads to the
conclusion that patterns of coastline change and alongshore distributions of
property values are co-dependent. Analyzing the holistic results of
different coastal management decisions made by different stakeholders along
a common coastline requires taking human/coastline coupling, as well as
wave-climate-change scenarios, into account. A stakeholder-initiated study
of coupled dynamics on the Virginia coastline, USA, provides an example.
Dr. Brad Murray is a geomorphologist with expertise in modeling landscape evolution, focusing largely in recent years on understanding how map-view shapes of coastlines develop, and predicting how these shapes might respond to changing climate and human forcing (i.e., how patterns of shoreline erosion and possible accretion will vary under different storm-climate and shoreline-stabilization scenarios). He earned B.A., M.S., and Ph.D. degrees from the University of Minnesota, Twin Cities. He is currently with the Division of Earth and Ocean Sciences in the Nicholas School of the Environment at Duke University.
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