INTERNAL WAVES OF GREAT AMPLITUDE, PART 2 (Interne Wellen Grosser Amplitude)

The principal results deduced from observations of internal waves in the ocean are discussed. Each of the measurements shows either the period or the wave length; hence, it follows that the nature of the detected waves cannot always be determined accurately. Besides it is not always possible to asce...

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Bibliographic Details
Main Author: Krauss,Wolfgang
Other Authors: NAVAL OCEANOGRAPHIC OFFICE WASHINGTON D C
Format: Text
Language:English
Published: 1959
Subjects:
Physical and Dynamic Oceanography
(*OCEAN CURRENTS
ATLANTIC OCEAN)
VORTICES
ATMOSPHERIC MOTION
SALINITY
TEMPERATURE
OSCILLATION
DENSITY
MEASUREMENT
TIDES
WEST GERMANY
*INTERNAL WAVES(MARINE)
TRANSLATIONS
North Atlantic
Online Access:http://www.dtic.mil/docs/citations/AD0693612
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0693612
Description
Summary:The principal results deduced from observations of internal waves in the ocean are discussed. Each of the measurements shows either the period or the wave length; hence, it follows that the nature of the detected waves cannot always be determined accurately. Besides it is not always possible to ascertain whether the observed variations are due to waves, vorticity or turbulence. Standing waves seem to occur at the continental slope. The analysis of periods, in particular, led to the suggestion that internal tides and inertia oscillations may predominate; according to measurements carried out in the Northern Atlantic, the wave lengths vary from 25 to 50 km. The maximal amplitude recorded is 300 meters. Variations of several hundred meters in accordance with the tidal rhythm and possibly, with (still unknown) periods of some importance which may be conditioned by meteorological processes, seem to occur frequently in the North Atlantic. (Author) Trans. of Deutsche Hydrographische Zeitschrift (West Germany) v11 n5 p194-207 1958, by M. Slessers.

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