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 fetch effect is an increase of the aeolian sediment transport rate with distance downwind
over an erodible surface. The first observations of the fetch effect go back 70years and the …

Contamination of terrestrial and marine environments by plastic waste has been widely
documented. Most research into the distribution of microplastics has focused on water but …

Temporal and spatial changes in wind speed, wind direction, and moisture content are
ubiquitous across sandy coastal beaches. Often these factors interact in unknown ways to …

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 …

A new dune profile model, Duna, is developed and coupled with the existing XBeach model,
in which some key improvements allow a much better behaviour of the intertidal beach and …

Observations of aeolian transport in coastal areas have focused on short-term experiments
because of limitations imposed by instrumentation. This paper uses a case study at …

This review considers the role of nearshore processes and morphological change as a
flexible and dynamic constraint on the supply and transport of sediment between beach and …

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) …

Ephemeral aeolian sand strips are commonplace on beaches. Their formation during high
energy sand transport events often precedes the development of protodunes and their …