Social associations and habitat selection delineate two subpopulations of west coast transient killer whales (Orcinus orca rectipinnus) in the California Current System. [PDF]
McInnes JD +9 more
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Satellite imagery reveals increasing volatility in human night-time activity. [PDF]
Li T +21 more
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Life strategies in an upwelling world: distribution patterns and niche partitioning of Calanidae copepods in the Benguela Current. [PDF]
Bode-Dalby M +7 more
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A Global Dataset of Bathymetric Features Identified with Prominence and Isobaths Analysis. [PDF]
Souche A, Hartz EH, Schmid DW.
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Mind the gap: Characterizing bias due to population mismatch in two-sample Mendelian randomization. [PDF]
Li J, Morrison J.
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The Spanish Continental Self and upper continental slope cartography.
Sanz-Alonso, J.L. (José Luis) +4 more
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What is the slope of the U.S. continental slope?
Geology, 1996Extensive high-resolution, multibeam bathymetry of five U. S. continental margins provides new, detailed information about the angle of continental slopes in different sedimentary and tectonic settings. The steepest continental slope examined is the passive-carbonate west Florida slope (4.4{degree} regional slope and 12.0{degree} mean local slope). The
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The Shaping of Continental Slopes by Internal Tides
Science, 2002The angles of energy propagation of semidiurnal internal tides may determine the average gradient of continental slopes in ocean basins (∼2 to 4 degrees). Intensification of near-bottom water velocities and bottom shear stresses caused by reflection of semi-diurnal internal tides affects sedimentation patterns and bottom gradients, as indicated by ...
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The variability of mixing at the continental slope
Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1990Abstract The benthic boundary layer on the continental slope is a region in which isopycnal surfaces intersect topography. It is, in consequence, particularly subject to variability caused by reflecting internal gravity waves, as well as by trapped baroclinic slope waves. Observations made using an array of moorings off the west slope
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