Robust regression modeling of shoreline data spanning 1930 to 1990 and
covering 1055 km of the Atlantic coast shows that nearly two-thirds o
f the U.S. east coast shorelines have undergone a significant change i
n the long-term rates of change between 1950 and 1980. The model resul
ts show that 62% of the shorelines have become more erosional or less
accretional. The average timing of these reversals (1967) corresponds
to a peak in the record of extratropical (northeast) storm frequency a
nd magnitude. These results raise questions regarding the applicabilit
y of linear methods for interpreting historical, long-term trends and
for predicting future shoreline positions.