TY - JOUR
T1 - Geomorphology of high-latitude coastal dunes
T2 - A review
AU - Ruz, M. H.
AU - Hesp, P. A.
PY - 2014/4/2
Y1 - 2014/4/2
N2 - The purpose of this review is to assess if there are any specific processes and morphologies distinguishing coastal dunes developed in cold-climate conditions, in order to illustrate how climate can exert a control on coastal dune morphologies. In the Arctic, availability of sand supply and the duration of winter conditions are limiting factors for the development of large coastal dunes. They are small in size, and embryo dunes including nebkha are the dominant and often only coastal dune type. In milder subarctic settings, characterized by a longer surficial ice-free season, a greater variety of coastal dunes are found, mainly foredunes, blowouts and parabolic dunes. In subarctic areas, as along the SE coast of Hudson Bay, niveo-aeolian processes actively affect coastal dune development. These processes do not generally imprint permanent morphologies, although some distinctive sedimentary structures owing to the melting of snow are observed. The coastal dunes of the arctic regions differ from the dunes of subarctic and temperate regions mainly because of their limited spatial and morphological development. Extreme climatic conditions (low precipitation, extreme cold), and very limited vegetation growing season, combined with low sediment supply, explain the fact that only embryo dunes develop in arctic environments.
AB - The purpose of this review is to assess if there are any specific processes and morphologies distinguishing coastal dunes developed in cold-climate conditions, in order to illustrate how climate can exert a control on coastal dune morphologies. In the Arctic, availability of sand supply and the duration of winter conditions are limiting factors for the development of large coastal dunes. They are small in size, and embryo dunes including nebkha are the dominant and often only coastal dune type. In milder subarctic settings, characterized by a longer surficial ice-free season, a greater variety of coastal dunes are found, mainly foredunes, blowouts and parabolic dunes. In subarctic areas, as along the SE coast of Hudson Bay, niveo-aeolian processes actively affect coastal dune development. These processes do not generally imprint permanent morphologies, although some distinctive sedimentary structures owing to the melting of snow are observed. The coastal dunes of the arctic regions differ from the dunes of subarctic and temperate regions mainly because of their limited spatial and morphological development. Extreme climatic conditions (low precipitation, extreme cold), and very limited vegetation growing season, combined with low sediment supply, explain the fact that only embryo dunes develop in arctic environments.
UR - http://www.scopus.com/inward/record.url?scp=85082866352&partnerID=8YFLogxK
U2 - 10.1144/SP388.17
DO - 10.1144/SP388.17
M3 - Review article
AN - SCOPUS:85082866352
SN - 0305-8719
VL - 388
SP - 199
EP - 212
JO - Geological Society Special Publication
JF - Geological Society Special Publication
IS - 1
ER -