Conclusions
A methodology for initialization of seasonal-to-
interannual predictions that does not rely on
model spin-up has been developed.
A surface measurement of soil moisture may be
used to correct the entire soil moisture profile.
Assimilation of soil moisture has a positive
impact on the water and energy budgets.
Soil moisture assimilation performs best for
regions with shallower soils; particularly depths
less than 3m.