We study the possibility that variations in the volume of the Great Sa
lt Lake (GSL), a large, closed basin lake, may be described as a low-d
imensional nonlinear dynamical system. There is growing evidence for s
tructure in the recurrence patterns of climatic fluctuations that driv
e western United States hydrology. Moreover, the time behavior of such
lakes is generally more regular than that of the climatic forcing. Th
is suggests the possibility that an analysis of the 144-year, biweekly
time series of the GSL volume may shed some light on the underlying d
ynamics of lake variations. Three methods (correlation dimension, near
est neighbor dimension, and false neighbor dimension) of estimating at
tractor dimension are applied and compared. The analysis suggests that
the GSL dynamics may be described by a dimension of about four. Impli
cations of such analyses relative to low-frequency variations and colo
red noise and limitations of such analyses are discussed.