Altimeter measurements of the volume transport through the Drake Passage
From in situ measurements it has been inferred that the variability of flow through the Drake Passage down to 2500m does not depend upon depth (barotropic flow). By making this assumption it is possible to calculate the variability of the volume transport from the surface slope as measured by a rada...
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| Veröffentlicht in: | Advances in space research 1998, Vol.22 (11), p.1549-1552 |
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| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng |
| Online-Zugang: | Volltext |
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