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Select the linear relation between surface geopotential anomaly |
Select the linear relation between surface geopotential anomaly |
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and surface pressure anomaly to be evaluated from |
and surface pressure anomaly to be evaluated from |
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$\frac{\partial \Phi_s}{\partial p_s} = 1/\rho(\theta_{Ref})$ |
$\frac{\partial \Phi_s}{\partial p_s} = 1/\rho(\theta_{Ref})$ |
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(see section \ref{sect:phi-freesurface}). |
(see section \ref{sec:phi-freesurface}). |
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Note that using the default (=TRUE), the constant $1/\rho_0$ is |
Note that using the default (=TRUE), the constant $1/\rho_0$ is |
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used instead, and is not necessary consistent with other |
used instead, and is not necessary consistent with other |
116 |
parts of the geopotential that relies on $\theta_{Ref}$. |
parts of the geopotential that relies on $\theta_{Ref}$. |
176 |
\begin{verbatim} |
\begin{verbatim} |
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cg2dTargetResWunit=1.E-17, |
cg2dTargetResWunit=1.E-17, |
178 |
\end{verbatim} |
\end{verbatim} |
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Sets the tolerance (in units of $\omega$) which the |
Sets the tolerance (in units of $\omega$) which the two-dimensional, |
180 |
two-dimensional, conjugate gradient solver will use to test for convergence |
conjugate gradient solver will use to test for convergence in equation |
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in equation \ref{EQ:eg-hs-congrad_2d_resid} to $1 \times 10^{-17} Pa/s$. |
%- note: Description of Conjugate gradient method (& related params) is missing |
182 |
Solver will iterate until |
% in the mean time, substitute this eq ref: |
183 |
tolerance falls below this value or until the maximum number of |
\ref{eq:elliptic-backward-free-surface} %\ref{eq:eg-hs-congrad_2d_resid} |
184 |
solver iterations is reached. |
to $1 \times 10^{-17} Pa/s$. |
185 |
|
Solver will iterate until tolerance falls below this value or until the |
186 |
|
maximum number of solver iterations is reached. |
187 |
\\ \fbox{ |
\\ \fbox{ |
188 |
\begin{minipage}{5.0in} |
\begin{minipage}{5.0in} |
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{\it S/R CG2D}~({\it cg2d.F}) |
{\it S/R CG2D}~({\it cg2d.F}) |