@article{
 title = {Transport and mixing simulation along the continental shelf edge using a Lagrangian approach Peer reviewed article},
 type = {article},
 year = {1999},
 id = {3c1465db-866c-3431-81a5-e68be0c485b7},
 created = {2020-09-29T09:39:16.242Z},
 file_attached = {false},
 profile_id = {7be7f7a6-afaf-3ffc-92cf-b3439435407e},
 group_id = {6a21fe5b-29d1-3626-b6cf-d66fb0ac7903},
 last_modified = {2020-09-29T09:39:16.242Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {mirandatransport},
 source_type = {article},
 private_publication = {false},
 abstract = {This paper presents the coupling of a biochemical model with two different hydrodynamic models, a 1-D model (Coelho, 1996) and a 3-D model (Santos, 1995), corresponding to two successive work phases. In the first phase the 1-D hydrodynamic model was used to calibrate the biochemical model; the results of this phase made it possible to analyse temporal vertical profiles evolution. Both an Eulerian and a Lagrangian approach were used to transport biochemical properties. In the second phase, the 3-D hydrodynamic model was applied; this gave a regionalscale view of the processes involved. Biochemical properties transport was made with a Lagrangian approach, highlighting the origin of upwelled water. Goban Spur/La Chapelle field data collected during the Ocean Margin Exchange project (Anon., 1996) were used as initial and boundary conditions in hydrodynamic and biochemical models. Our main conclusion is that a 3-D particle-tracking model, coupled with a 3-D hydrodynamic model (with a proper turbulence closure model) and with a biochemical model, can be an excellent tool to quantify exchanges between the continental shelf and deep ocean.},
 bibtype = {article},
 author = {Miranda, R and Leitão, P C and Coelho, H S and Martins, H and Neves, R R}
}

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