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- W3175452938 abstract "Periodic features observed in the ocean portions of certain ERTS-1 images have been identified with reasonable certainty as surface manifestations of oceanic internal gravity waves. A series of images taken over the New York Bight, commencing with the 16 July 1972 overpass and continuing on into autumn of 1973, has shown the internal waves to be present when summer solar heating stratifies the water sufficiently well to support such oscillations. When fall and winter wind action mixes the shelf water down to the bottom, the waves no longer appear. In the Bight, the wavelengths range from approximately 400 to 1000 m, with the wave field being most sharply delineated near the edges of the continental shelf, at the mouth of the Hudson Canyon. They appear in packets consisting of several waves separated by 10-15 km, which propagate up on the shelf and disappear." @default.
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- W3175452938 date "1974-01-01" @default.
- W3175452938 modified "2023-09-25" @default.
- W3175452938 title "Ocean Internal Waves off the North American and African Coasts from ERTS-1" @default.
- W3175452938 hasPublicationYear "1974" @default.
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