The FOODBANCS project: Introduction and sinking fluxes of organic carbon, chlorophyll-a and phytodetritus on the western Antarctic Peninsula continental shelf

2008 ◽  
Vol 55 (22-23) ◽  
pp. 2404-2414 ◽  
Author(s):  
Craig R. Smith ◽  
Sarah Mincks ◽  
David J. DeMaster
Keyword(s):  
Organic Carbon ◽  
Continental Shelf ◽  
Chlorophyll A ◽  
Antarctic Peninsula ◽  
Western Antarctic Peninsula

scholarly journals Spatial patterns of continental shelf faunal community structure along the Western Antarctic Peninsula

PLoS ONE ◽  
2020 ◽  
Vol 15 (10) ◽  
pp. e0239895 ◽  
Author(s):  
Alan M. Friedlander ◽  
Whitney Goodell ◽  
Pelayo Salinas-de-León ◽  
Enric Ballesteros ◽  
Eric Berkenpas ◽  
...  
Keyword(s):  
Community Structure ◽  
Continental Shelf ◽  
Spatial Patterns ◽  
Antarctic Peninsula ◽  
Western Antarctic Peninsula

scholarly journals Productivity and linkages of the food web of the southern region of the western Antarctic Peninsula continental shelf

2014 ◽  
Vol 122 ◽  
pp. 10-29 ◽  
Author(s):  
Tosca Ballerini ◽  
Eileen E. Hofmann ◽  
David G. Ainley ◽  
Kendra Daly ◽  
Marina Marrari ◽  
...  
Keyword(s):  
Continental Shelf ◽  
Food Web ◽  
Antarctic Peninsula ◽  
Southern Region ◽  
Western Antarctic Peninsula

scholarly journals Transport of warm Upper Circumpolar Deep Water onto the western Antarctic Peninsula continental shelf

Ocean Science ◽  
2012 ◽  
Vol 8 (4) ◽  
pp. 433-442 ◽  
Author(s):  
D. G. Martinson ◽  
D. C. McKee
Keyword(s):  
Continental Shelf ◽  
Antarctic Peninsula ◽  
Deep Water ◽  
Antarctic Circumpolar Current ◽  
Western Antarctic Peninsula ◽  
Dominant Mechanism ◽  
Circumpolar Deep Water ◽  
Marguerite Bay ◽  
Circumpolar Current ◽  
The Antarctic

Abstract. Five thermistor moorings were placed on the continental shelf of the western Antarctic Peninsula (between 2007 and 2010) in an effort to identify the mechanism(s) responsible for delivering warm Upper Circumpolar Deep Water (UCDW) onto the broad continental shelf from the Antarctic Circumpolar Current (ACC) flowing over the adjacent continental slope. Historically, four mechanisms have been suggested: (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 advective diversions of the ACC onto 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 extent. Mechanism 2 played no role, though the canyons have been shown previously to channel UCDW across the shelf into Marguerite Bay. Mechanism 4 played no role independently, though eddies may be advected within a greater intrusion of the background flow.

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