Foredune Height Research Articles

Dune plant species diversity and function in two barrier island biogeomorphic systems

Barrier island dune systems exhibit strong geographic contrasts in theinteraction between extrinsic disturbance from storm overwash and intrinsicbiogeomorphic recovery processes. To examine how these interactions shape duneplant species diversity, I sampled species cover and topography alongfrequentlystorm-overwashed (South Core Banks, North Carolina) and infrequently overwashed(Sapelo Island, Georgia) barrier islands. The observed compositional anddiversity patterns were in agreement with a complex systems model in whichextrinsic overwash exposure is either reinforced (South Core Banks) or dampened(Sapelo Island) by intrinsic biogeomorphic controls of topography. A largespatial-scale regularity in the distributional pattern of along-shore speciesdiversity was correlated to primary foredune height on South Core. On Sapelo, afine-spatial scale differentiation of species diversity patterns was lessstrongly correlated to topographic metrics. There were no significantdifferences between islands in along-shore alpha diversity (Shannon-Weinerindex). However, Sapelo was more diverse given its smaller area and finer-scalehabitat heterogeneity. I posit that the relevancy of the IntermediateDisturbance Hypothesis is weak when examining diversity patterns along a shoredisturbance gradient. Intrinsic biogeomorphic processes decouple the directcause-and-effect relationship between disturbance and diversity, a basicassumption of IDH. I posit that the Dynamic Equilibrium Model may be a moregenerally applicable conceptual framework. DEM incorporates the interaction ofintrinsic and extrinsic processes that shape habitat heterogeneity, aprerequisite for understanding how complex systems interactions shape diversitypatterns.

Air flow over foredunes and implications for sand transport

AbstractMore than 4000 hourly wind profiles measured on three topographically different foredunes are analysed and discussed. Wind flow over the foredunes is studied by means of the relative wind speed: the ratio between wind speed at a certain location and the reference wind speed at the same height. Relative wind speeds appear to be independent of general wind speed but dependent on wind direction. For perpendicular onshore winds the flow over the foredune is accelerated due to topographic changes and decelerated due to changes in surface roughness. Accelerations dominate over decelerations on the seaward slope. The pattern of acceleration and deceleration in relation to wind direction is more or less comparable for different foredunes, but the magnitudes differ. An increase in foredune height from 6 to 10m leads to an increase in speed‐up near the top of the seaward slope from 110 to 150 per cent during onshore wind, but further increase of foredune height from 10 to 23m appears to have little effect, due to increased roughness and deflection of flow.Topography also influences the direction of the flow. Between beach and top, the flow deflects in the direction of the normal during onshore winds. During offshore winds the flow is deflected to the parallel. Near the dunefoot, deflection is always in the direction of the parallel, and increases with steeper topography. The maximum deflection near the dunefoot was 90°, over a 23 m high dune, observed during offshore winds.Patterns of erosion and sedimentation resulting from winds from different directions can be explained by the observed accelerations and decelerations. Owing to speed‐up on the seaward front of the foredune, sand transport capacity of the wind increases, which results in erosion if vegetation is absent. During strong onshore wind, sand is lifted near the dunefoot and moves over the foredune in suspension. During weaker winds, vertical wind velocities do not exceed fall velocities of the sand grains, and most of the sand is deposited near the dunefoot.