Analysis of simultaneous measurements of inshore processes and changes
in beach profiles over a nine-month period on the Outer Banks of Nort
h Carolina shows a relationship between storm magnitude and the vertic
al and horizontal erosion of a subaerial beach. The maximum cut during
any tidal cycle was 70 cm, which occurred in the middle of the profil
e. The majority of the erosion occurring during the first 6 hours Of t
he storms and approximately 50 percent of the sand lost during the sto
rms was recovered within the first 12 hours following the storms. wave
height and steepness and the pre-storm beach configuration determined
the extent of the vertical erosion. There is a downward limit to vert
ical erosion, and once this level is reached the maximum changes becom
e horizontal.