Abstract

Using a stand-alone 1-dim soil and atmospheric boundary layer model, the feasibility of off-line variational soil moisture analysis by assimilation of near-surface atmospheric observations is investigated. The experiments are performed using the soil module and boundary layer formulation taken from the regional forecast model of the German Weather Service. Assimilation experiments indicate that atmospheric information allows to initialize soil humidity to realistic values. Sensitivity studies using an adjoint code show that proper modeling of the soil moisture signal propagation into the atmosphere is crucial for the algorithm. An assessment of errors corrupting the fit resulting from erroneous cloud-cover specification is performed. The errors are found to be small for the case considered thus confirming the usefulness of assimilation of soil moisture for short-term weather forecasts even under non-perfect conditions.

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