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...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1959
|
Subjects: | |
Online Access: | http://www.dtic.mil/docs/citations/AD0693612 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0693612 |
id |
ftdtic:AD0693612 |
---|---|
record_format |
openpolar |
spelling |
ftdtic:AD0693612 2023-05-15T17:33:13+02:00 INTERNAL WAVES OF GREAT AMPLITUDE, PART 2 (Interne Wellen Grosser Amplitude) Krauss,Wolfgang NAVAL OCEANOGRAPHIC OFFICE WASHINGTON D C 1959 text/html http://www.dtic.mil/docs/citations/AD0693612 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0693612 en eng http://www.dtic.mil/docs/citations/AD0693612 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography (*OCEAN CURRENTS ATLANTIC OCEAN) VORTICES ATMOSPHERIC MOTION SALINITY TEMPERATURE OSCILLATION DENSITY MEASUREMENT TIDES WEST GERMANY *INTERNAL WAVES(MARINE) TRANSLATIONS Text 1959 ftdtic 2016-02-18T22:23:04Z 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. Text North Atlantic Defense Technical Information Center: DTIC Technical Reports database |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography (*OCEAN CURRENTS ATLANTIC OCEAN) VORTICES ATMOSPHERIC MOTION SALINITY TEMPERATURE OSCILLATION DENSITY MEASUREMENT TIDES WEST GERMANY *INTERNAL WAVES(MARINE) TRANSLATIONS |
spellingShingle |
Physical and Dynamic Oceanography (*OCEAN CURRENTS ATLANTIC OCEAN) VORTICES ATMOSPHERIC MOTION SALINITY TEMPERATURE OSCILLATION DENSITY MEASUREMENT TIDES WEST GERMANY *INTERNAL WAVES(MARINE) TRANSLATIONS Krauss,Wolfgang INTERNAL WAVES OF GREAT AMPLITUDE, PART 2 (Interne Wellen Grosser Amplitude) |
topic_facet |
Physical and Dynamic Oceanography (*OCEAN CURRENTS ATLANTIC OCEAN) VORTICES ATMOSPHERIC MOTION SALINITY TEMPERATURE OSCILLATION DENSITY MEASUREMENT TIDES WEST GERMANY *INTERNAL WAVES(MARINE) TRANSLATIONS |
description |
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. |
author2 |
NAVAL OCEANOGRAPHIC OFFICE WASHINGTON D C |
format |
Text |
author |
Krauss,Wolfgang |
author_facet |
Krauss,Wolfgang |
author_sort |
Krauss,Wolfgang |
title |
INTERNAL WAVES OF GREAT AMPLITUDE, PART 2 (Interne Wellen Grosser Amplitude) |
title_short |
INTERNAL WAVES OF GREAT AMPLITUDE, PART 2 (Interne Wellen Grosser Amplitude) |
title_full |
INTERNAL WAVES OF GREAT AMPLITUDE, PART 2 (Interne Wellen Grosser Amplitude) |
title_fullStr |
INTERNAL WAVES OF GREAT AMPLITUDE, PART 2 (Interne Wellen Grosser Amplitude) |
title_full_unstemmed |
INTERNAL WAVES OF GREAT AMPLITUDE, PART 2 (Interne Wellen Grosser Amplitude) |
title_sort |
internal waves of great amplitude, part 2 (interne wellen grosser amplitude) |
publishDate |
1959 |
url |
http://www.dtic.mil/docs/citations/AD0693612 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0693612 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0693612 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766131646947393536 |