![]() of Georgia Skidaway Institute of Oceanography, USAĭana Savidge – Univ. of Georgia Skidaway Institute of Oceanography, USAĬatherine Edwards – Univ. You can think of a continental shelf as a part of a continent that just happens to be underwater at. But it is still relatively flat, considering that beyond the edge of the shelf, the water depths drop rather suddenly to a few thousand metres. Questions/comments may be directed to Workshop Steering Committee The Norwegian continental shelf, for instance, has water depths that vary between 100 and 400 metres. A CONTINENTAL SHELF is the submerged top of the continents edge, lying between the shoreline and the continental slope that forms a border to a continent. In-person participation is limited to to complete a preregistration formĬlick to see presentations from the 2020 Virtual Pre-Workshop and Poster Sessions The overall goal of this workshop is to convene a globally diverse group of researchers to discuss the state of knowledge of WBC-STCS ecosystems and to identify strategies for coordinating observational and research objectives to advance understanding of these dynamic regions. We believe the time is right to consider these systems as parallel global marine ecosystems and to develop a coherent international strategy to assess their function and contributions to global carbon cycles. Comparative analysis of the physical forcing and biochemical/ecological ramifications between the different ocean/shelf settings has the potential to reveal common and contrasting underlying properties and their sensitivity to climatic perturbations in ways that fragmented attention to individual system idiosyncrasies cannot. In the major ocean basins, energetic western boundary currents (WBC) adjacent to subtropical continental shelves (STCS) interact strongly with bathymetry, resulting in first order consequences to shelf biochemistry and ecosystem response. CLICK TO GO THE REGISTRATION/HOTEL INFORMATION PAGE Continents are the seven main divisions of land on Earth. REGISTRATION FOR THE WORKSHOP IS NOW OPEN. A continental shelf is the edge of a continent that lies under the ocean. We also consider the effects of shifting the prescribed wind forcing profile to the south a simplified representation of future potential changes to. ![]() Each of these parts has its specific geomorphology and marine biology. International Workshop on Western Boundary Current – Subtropical Continental Shelf Interactions May 22-24, 2023 Inclusion of the ridge enhances heat transport onto the continental shelf without the ridge the flow features an along-shelf break westward current that suppresses cross-shelf break fluxes. The shelf area is commonly subdivided into the inner continental shelf, mid-continental shelf, and outer continental shelf. Current: International Workshop on Western Boundary Current – Subtropical Continental Shelf Interactions The term continental shelf is used by geologists generally to mean that part of the continental margin which is between the shoreline and the shelf break or.
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