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Philip L. Richardson

Researcher at Woods Hole Oceanographic Institution

Publications -  112
Citations -  7059

Philip L. Richardson is an academic researcher from Woods Hole Oceanographic Institution. The author has contributed to research in topics: Gulf Stream & Ocean current. The author has an hindex of 47, co-authored 111 publications receiving 6712 citations. Previous affiliations of Philip L. Richardson include United States Coast Guard Academy & University of Rhode Island.

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Observations of the Mindanao Current during the western equatorial Pacific Ocean circulation study

TL;DR: The Western Equatorial Pacific Ocean Circulation Study (WEPOCS) III was conducted from June 18 through July 31, 1988, to observe the low-latitude western boundary circulation there, with emphasis on the Mindanao Current.
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The dispersal of the Amazon's water

TL;DR: For example, NASA's Coastal Zone Color Scanner and with drifting buoys revealed that the discharge of the Amazon is carried offshore around a retroflection of the North Brazil Current and into the North Equatorial Countercurrent towards Africa between June and January each year as mentioned in this paper.
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Two Years in the Life of a Mediterranean Salt Lens

TL;DR: A lens of Mediterranean water (Meddy) was tracked in the eastern North Atlantic for two years with SOFAR floats as mentioned in this paper, moving in an irregular pattern, at speeds of a few cm s−1, and translated 1100 km to the south in two years.
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Eddy kinetic energy in the North Atlantic from surface drifters

TL;DR: One hundred ten satellite-tracked freely drifting buoys measured velocities and trajectories of the near-surface currents in the North Atlantic as discussed by the authors, and a horizontal map of eddy kinetic energy was prepared on a 2°×2° grid between latitudes 20° and 55°N.
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A census of Meddies tracked by floats

TL;DR: In this paper, subsurface float measurements in 27 Mediterranean Water eddies (Meddies) in the Atlantic are grouped together to reveal new information about the pathways of these energetic eddies and how they are often modified and possibly destroyed by collisions with seamounts.