As the largest ecosystem of China, the desert ecosystem and the desertification-prone
region (DPR) occupies 44% of China's land area. The past, present, and the future of …

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 …

Untitled Page 1 Page 2 GEOMORPHOLOGY OF DESERT DUNES Sand dunes cover up to a
quarter of many desert regions. Determining the factors that determine their shape, size and …

For more than four decades remote sensing images have been used to document and
understand the evolution of aeolian sand dunes. Early studies focused on map** and …

The Mediterranean coastal dunes of Israel underwent a land‐use change during the second
half of the 20th century. Due to intense agricultural and pastoral activity, the coastal dunes …

Vegetation is the most common and most reliable stabilizer of loose soil or sand. This
ancient technique is for the first time cast into a set of equations of motion describing the …

The 'Fryberger model'uses standardized wind data to estimate regional aeolian sediment
drift potential (DP), which allows for interpretation and classification of aeolian dune …

Vegetation plays an important role in sha** the morphology of aeolian dune landscapes
in coastal and semi‐arid environments, where ecogeomorphic interactions are complex and …

Coastal dunefields have developed on the west coast of Jutland in Denmark over the past
5000 years. The dunefields are situated in a temperate climate zone with frequent high …

The formation and evolution of coastal dunes result from a complex interplay of eco-
morphodynamic processes. State-of-the-art models can simulate aeolian transports and …