Abstract
A model of the shallow water equations is used as a testbed to compare several initialization strategies and to find points satisifying conditions of "slowness'. Several methods are explored to initialize the low order model: 1) Lorenz's method of successively zeroing tendencies; 2) minimization of the sum of the squares of the tendencies; 3) use of a balance condition. We find that the balance condition produces the smoothest solution on a consistent basis. In addition, Lorenz initialization, the Newton-Kantorovich Theorem, and the Nested Interval Property are used to compute points devoid of gravity waves. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 145-161 |
| Number of pages | 17 |
| Journal | Tellus, Series A: Dynamic Meteorology and Oceanography |
| Volume | 47 A |
| Issue number | 2 |
| DOIs | |
| State | Published - 1995 |
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