This paper introduces a classification of coastal dune systems into tw
o main morphodynamic classes, namely retentive and transgressive dune
systems. Retentive systems include coastal dune types where sand accum
ulation within vegetation is dominant over other processes. In this ca
tegory we include such morphological types as hummock dunes, foredunes
, and retention ridges, including sub-environments such as precipitati
on ridges that form the landward boundary of transgressive dunefields.
Transgressive systems include those coastal dune types where sand tra
nsport is dominant over other processes, and the dunes are unvegetated
and mobile. In this category we include such morphological types as p
arabolic dunes, reversing transverse dunes, barchans, self dunes, tran
sgressive sheet dunefields and headland-bypass dunefields. Components
of the two main morphodynamic types of coastal dune systems range in s
ensitivity from sensitive to robust. Retentive dune systems, being veg
etated, are sensitive and fragile. Mobile dunes that form, the major c
omponent of transgressive dune systems are robust and resilient. This
morphodynamic classification is particularly useful because the two ty
pes of dune systems have diametrically opposed sensitivities and hence
different management requirements.