Despite widespread recognition that landforms are complex Earth systems with process-
response linkages that span temporal scales from seconds to millennia and spatial scales …

The mobility of coastal dunes is characterised by bio-geomorphological responses related to
change in boundary conditions, particularly sediment supply, wind and vegetation cover, as …

Coastal dunes, in particular foredunes, support a resilient ecosystem and reduce coastal
vulnerability to storms. In contrast to dry desert dunes, coastal dunes arise from interactions …

The ability of beaches and dunes to recover following an extreme storm is a primary control
of barrier island response to sea-level rise and changes in the frequency and/or magnitude …

Aeolian sediment transport is influenced by a variety of bed surface properties, like moisture,
shells, vegetation, and nonerodible elements. The bed surface properties influence aeolian …

The form, height and volume of coastal foredunes reflects the long‐term interaction of a suite
of nearshore and aeolian processes that control the amount of sand delivered to the …

Evidence from a field study on wind flow and sediment transport across a beach–dune
system under onshore and offshore conditions (including oblique approach angles) …

This paper offers a synthesis of the disparate evidence on the importance of the magnitude
and duration of water level rise in both lacustrine and marine environments in relation to …

Beach–dune systems are dynamic geomorphic environments subject to erosion during
storms and reconstruction during swell‐dominated inter‐storm periods. Wave‐cut scarps are …

Buildings at the beach change the near-bed airflow patterns in the surrounding area. This
induces alterations in wind-induced bed shear stress and wind-induced sediment transport …