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Demonstrated
a methodology for generating
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soil
moisture initialisation states.
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Soil
moisture assimilation performs best for
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regions
with shallower soils; particularly
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depths
less than 3m.
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Important
that all of the dominant physical
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processes
in the LSM are identified and
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included
in the covariance forecasting.
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Structure
of the model effects the retrieval
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time
(ie. layered vs catchment deficit).
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