'Shelf break' presentation slideshows

Climate variability in the Southern Ocean Sector: Relevance to the McMurdo LTER

Climate variability in the Southern Ocean Sector: Relevance to the McMurdo LTER. Martin Visbeck Department of Earth and Environmental Sciences Lamont-Doherty Earth Observatory Columbia University, New York input from: Gerd Krahmann, Arnold Gordon and Stan Jacobs. Topics for discussion.

482 views • 35 slides

Climate variability in the Southern Ocean Sector: Relevance to the McMurdo LTER

Climate variability in the Southern Ocean Sector: Relevance to the McMurdo LTER. Martin Visbeck Department of Earth and Environmental Sciences Lamont-Doherty Earth Observatory Columbia University, New York input from: Gerd Krahmann, Arnold Gordon and Stan Jacobs. Topics for discussion.

355 views • 35 slides

Yvette H. Spitz Oregon State University, CEOAS

Western Arctic Ocean Primary Productivity Changes over the Last Three Decades and in the Future: not a Simple Story. Yvette H. Spitz Oregon State University, CEOAS Carin J. Ashjian (1) , Robert G. Campbell (2) , Michael Steele (3) and Jinlun Zhang (3).

439 views • 26 slides

Continental Margins and Ocean Basins

656 views • 26 slides

The Role of Canyons, Promontories and Topography in DOES

Susan Allen, Department of Earth & Ocean Science University of British Columbia Vancouver, Canada. The Role of Canyons, Promontories and Topography in DOES. Outline. Some definitions Limitation of shelf-break exchange Eddy shedding and instability: capes and promontories

412 views • 25 slides

Modeling Tides for Southern Ocean GLOBEC

317 views • 20 slides

Subtidal Community

Subtidal Community. Soft Bottom SAV (eelgrass). Figure 10.22. Subtidal Zone. The part of the continental shelf that is always covered by water from the low tide mark to the shelf break (150m or 490 ft). Subtidal Zone. Temperature varies from place to place due to its shallowness

556 views • 19 slides

15.2 The Diversity of Ocean Life

998 views • 16 slides

Objectives

184 views • 10 slides

Basin Scale Progress

Basin Scale Progress 10-20 years runs have been performed using the two different vertical coordinate systems (with and without tides) The final production runs are set up and will run over the next month (1980-2010). These runs will have an extended domain, rivers and an updated bathymetry.

277 views • 2 slides