A case study of the application of recent methods of nonlinear time se
ries analysis is presented. The 1848-1992 biweekly time series of the
Great Salt Lake (GSL) volume is analyzed for evidence of low dimension
al dynamics and predictability. The spectrum of Lyapunov exponents ind
icates that the average predictability of the GSL is a few hundred day
s. Use of the false nearest neighbor statistic shows that the dynamics
of the GSL can be described in time delay coordinates by four dimensi
onal vectors with components lagged by about half a year. Local linear
maps are used in this embedding of the data and their skill in foreca
sting is tested in split sample mode for a variety of GSL conditions:
lake average volume, near the beginning of a drought, near the end of
a drought, prior to a period of rapid lake rise. Implications for mode
ling low frequency components of the hydro-climate system are discusse
d.