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 …

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 …

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

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 …

Surface moisture is an important supply limiting factor for aeolian sand transport, which is
the primary driver of coastal dune development. As such, it is critical to account for the …

The purpose of this study was to quantify relationships between season, sediment
availability, sediment transport pathways, and beach/foredune morphology at Greenwich …

Flow deflection of surface winds is common across coastal foredunes and blowouts. Incident
winds approaching obliquely to the dune toe and crestline tend to be deflected towards a …

Wind flow and sand transport intensity were measured on the seaward slope of a vegetated
foredune during a 16 h storm using an array of sonic anemometers and Wenglor laser …

The collection of a time series coupling hourly wind data (speed and direction) with sand
transport over months has provided new insights into the dynamics of transport events that …