Transport of warm upper circumpolar deep water onto the Western Antarctic Peninsula Continental Shelf

نویسنده

  • D. G. Martinson
چکیده

continental slope. Historically, four mechanisms have been suggested (or assumed): (1) eddies shed from the ACC, (2) flow into the cross-shelf-cutting canyons with overflow onto the nominal shelf, (3) general upwelling, and (4) episodic sweeping of ACC meanders over the shelf. The mooring array showed that for the years of deployment, the dominant mechanism is eddies; upwelling may also contribute but to an unknown 10

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تاریخ انتشار 2012