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Low-Temperature Hydrothermal Plumes in the Near-Bottom Boundary Layer at Endeavour Segment,Juan de Fuca Ridge
Low-Temperature Hydrothermal Plumes Near-Bottom Boundary Layer Endeavour Segment,Juan Fuca Ridge
2015/7/14
Low-temperature (typically 5–75°C) fluid, commonly referred to as "diffuse" hydrothermal flow, emanates from fractures over a significant portion of the Juan de Fuca Ridge seafloor in the Northeast Pa...
Wind Effects on Currents Observed in Juan de Fuca Submarine Canyon
Wind Effects Juan de Fuca Submarine Canyon Currents Observed
2009/4/3
Juan de Fuca submarine canyon has depths exceeding 200 m extending completely across the continental shelf. Observations of currents in the canyon during winter 1970 showed relatively large currents a...
L’Histoire Physique de la Mer. Part III：On the Motions of Seawater
currents waves tides Seawater movements
2008/12/11
Seawater movements are of three kinds: currents, waves, and tides. Observations were made five times a day for three and one-quarter months in the Strait of Cassis. Mariners' reports of a westward cur...
The Probability Distribution of the Thorpe Displacement within Overturns in Juan de Fuca Strait
Probability Distribution of the Thorpe Displacement Overturns Juan de Fuca Strait
2008/6/4
Vertical mixing in the ocean can sometimes be quantified by measurements of the Thorpe overturning scale, LT. In regions of weak mixing and weak density gradients such measurements may be limited by s...