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Slope Water Interaction Workshop 23-24 August, 2000 Clark Laboratory, Woods Hole Oceanographic Institution |
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Abstract
Overviews Observations and Models
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23 May - 3 June
1997 Part of this cruise was spent investigating a detrainment feature on the southern flank of Georges Bank- water that was being drawn off the Bank in association with a warm core ring. Three CTD transects of the feature were done, followed by a 3-station MOCNESS transect before a storm and a 2-station partial transect after the storm. CTD-rosette casts occurred before each MOCNESS tow to sample the microzooplankton and phytoplankton (Figure 1). CTD-rosette casts and MOCNESS tows during the earlier part of the cruise sampled various potential source regions (Northeast Peak, Cold Plume, South Flank, Georges Basin, Crest), as part of other cruise projects. Data from the feature include: zooplankton biomass and species distributions from MOCNESS tows (Wishner), predator distributions from the same MOCNESS tows (Sullivan), CTD transects (Wishner and others), microzooplankton and phyoplankton from CTD-rosette casts (Gifford, Sieracki), Safire fluorescence data from MOCNESS tows (Donaghay), and ADCP data (Flagg). AVHRR satellite images (Bisagni) and drifter paths (Beardsley and Limeburner) are also pertinent. The EN301 feature moved in a southwest direction along the south flank over the course of several weeks during spring 1997. Studies of the biology and physical oceanography of this feature will address questions about how important these features are for Bank ecosystem dynamics and whether they are likely to contribute to the hypothesized Bank -Slope - Bank loop for Calanus. From satellite images examined at the August 2000 data workshop, this is a different feature than that studied by the SeaSoar surveys of Lee et al. earlier that same spring. A comparison with the Lee et al. feature and the development of an overall concept of the structure and role of these features was discussed. |