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Semi-implicit semi-Lagrangian methods for numerical weather ...

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<strong>Semi</strong>-Implicit<br />

<strong>Semi</strong>-<br />

<strong>Lagrangian</strong><br />

Time-<br />

Stepping<br />

Methods and<br />

Regularized<br />

Fluid<br />

Equations in<br />

Numerical<br />

Weather<br />

Prediction<br />

Sebastian<br />

Reich<br />

Numerical<br />

Weather<br />

Prediction<br />

Basic Facts<br />

Unified Model<br />

Towards a<br />

New Dynamic<br />

Core<br />

Model System and<br />

Basic Ideas<br />

Results<br />

General<br />

Methodology<br />

Concluding<br />

Remarks<br />

General Regularization Procedure<br />

Full Euler Equations<br />

Given a hydrostatic reference state (¯θ, ¯π), the regularized<br />

equations take the abstract <strong>for</strong>m<br />

Dv<br />

Dt = −cpθ∇x˜π ′ ˜θ ′<br />

+ gk<br />

¯θ<br />

Dθ<br />

dt<br />

= 0,<br />

Dρ<br />

Dt = −ρ∇x · v,<br />

Here θ = ¯ θ + θ ′ , π = ¯π + π ′ .<br />

− f k × v = Rv,

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