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| revision 1.5 by cnh, Wed Oct 24 23:14:44 2001 UTC | revision 1.6 by cnh, Thu Oct 25 00:55:28 2001 UTC | |
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| # | Line 268 M_{w} = \pi ( \frac { A_{h} }{ \beta } ) | Line 268 M_{w} = \pi ( \frac { A_{h} }{ \beta } ) |
| 268 | \noindent of $\approx 100$km. This is greater than the model | \noindent of $\approx 100$km. This is greater than the model |
| 269 | resolution in mid-latitudes $\Delta x$, ensuring that the frictional | resolution in mid-latitudes $\Delta x$, ensuring that the frictional |
| 270 | boundary layer is well resolved. | boundary layer is well resolved. |
| 271 | ||
| 272 | \\ | \\ |
| 273 | ||
| 274 | \noindent The model is stepped forward with a | \noindent The model is stepped forward with a |
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