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The relationship between streamline pattern and momentum transport has been examined. It is shown, for divergent flow, that it is possible for a streamline pattern with troughs and ridges oriented northeast-southwest to have zonally averaged momentum transports associated with it which are directed equatorward in the Northern Hemisphere.
The relationship between streamline pattern and momentum transport has been examined. It is shown, for divergent flow, that it is possible for a streamline pattern with troughs and ridges oriented northeast-southwest to have zonally averaged momentum transports associated with it which are directed equatorward in the Northern Hemisphere.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 142 | 11 | 2 |
| PDF Downloads | 14 | 9 | 0 |
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