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Advanced Research WRF (ARW) Technical Note - MMM - University ...

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space via the control variable transform U, i.e.,<br />

x ′ = Uv = UpUvUhv. (9.2)<br />

The expansion U = UpUvUh represents the various stages of covariance modeling: horizontal<br />

correlations Uh, vertical covariances Uv, and multivariate covariances Up.<br />

The components of v are chosen so that their error cross-correlations are negligible, thus<br />

permitting the matrix B to be block-diagonalized. The many varying applications (high/low<br />

resolution, polar/tropical, etc.) of <strong>WRF</strong>-Var require a flexible choice of background error model.<br />

This is achieved via a namelist option “cv options” as defined in Table 9.1.<br />

cv options<br />

Analysis<br />

Increment<br />

Change of<br />

Variable<br />

Vertical<br />

Covariances<br />

Horizontal<br />

Correlations<br />

Control<br />

Variables<br />

2 3 4 5<br />

(original MM5) (NCEP) (Global) (Regional)<br />

x ′ u ′ ,v ′ ,T ′ ,q ′ ,ps ′ (i, j, k)<br />

Up ψ ′ ,χ ′ ,p ′ u,q ′ ψ ′ ,χ ′ u,T ′ u,r ′ ,p ′ su<br />

Uv B = EΛE T RF B = EΛE T<br />

Uh RF Spectral RF<br />

v v(i, j, m) v(i, j, k) v(l, n, m) v(i, j, m)<br />

Table 9.1: The definitions of the various stages of the control variable transform given by (9.2) for<br />

the unified global/regional <strong>WRF</strong>-Var system. Indices (i, j, k) refer to grid-point space, index m<br />

to vertical mode, and l, n to global spectral mode. The variables are: u, v: velocity components;<br />

T : temperature; q: mixing ratio; ps: surface pressure; ψ: streamfunction; χ: velocity potential;<br />

r: relative humidity. The subscript u indicates an unbalanced field. The acronym RF stands<br />

for recursive filter.<br />

Table 9.1 indicates that the only difference between global (cv options=4) and <strong>WRF</strong> regional<br />

(cv options=5) versions of the <strong>WRF</strong>-Var control variable transform is in the horizontal error<br />

correlations Uh. <strong>Note</strong> also, the only difference between the old MM5 background error model<br />

(cv options=2) and <strong>WRF</strong> regional (cv options=5) is in the Up transform. The former imposes a<br />

dynamical balance constraint via an unbalanced pressure control variable (Barker et al., 2004),<br />

whereas in the new regional covariance model, balance is imposed via statistical regression (see<br />

Section 9.3 for details). This choice of control variables is considered more appropriate for the<br />

mass-based <strong>ARW</strong> solver.<br />

68

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