Shelf waves with diurnal tidal frequency at the Greenland shelf edge:

Tidal analysis has been carried out on current measurements at a “cross-shelf” transect off Greenland at 71o N. The diurnal tides manifest themselves mainly as a barotropic continental shelf wave, travelling southward along the shelf slope. This follows from the amplitude distribution of the diurnal...

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Main Author: Lam, F.P.A.
Format: Article in Journal/Newspaper
Language:English
Published: 1999
Subjects:
Online Access:http://resolver.tudelft.nl/uuid:661dc1ea-ab7d-45b8-a274-3dee7891c072
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spelling fttno:oai:tudelft.nl:uuid:661dc1ea-ab7d-45b8-a274-3dee7891c072 2023-05-15T16:26:58+02:00 Shelf waves with diurnal tidal frequency at the Greenland shelf edge: Lam, F.P.A. 1999-01-01 http://resolver.tudelft.nl/uuid:661dc1ea-ab7d-45b8-a274-3dee7891c072 en eng uuid:661dc1ea-ab7d-45b8-a274-3dee7891c072 186410 http://resolver.tudelft.nl/uuid:661dc1ea-ab7d-45b8-a274-3dee7891c072 Deep Sea Research Part I: Oceanographic Research Papers, May, 5, 46, 895-923 article 1999 fttno 2022-04-10T16:16:08Z Tidal analysis has been carried out on current measurements at a “cross-shelf” transect off Greenland at 71o N. The diurnal tides manifest themselves mainly as a barotropic continental shelf wave, travelling southward along the shelf slope. This follows from the amplitude distribution of the diurnal tidal components and from the rotation sense of the tidal ellipses at different cross-slope locations, as calculated with simple two-dimensional models. The well organized cross-slope pattern of the velocity amplitudes is absent in observations further north near 75o N.These observations suggest that the local vanishing of the group velocity, which is caused by topography, is of importance for the existence and local amplification of these continental shelf waves with diurnal tidal frequency. Article in Journal/Newspaper Greenland TU Delft: Institutional Repository (Delft University of Technology) Greenland
institution Open Polar
collection TU Delft: Institutional Repository (Delft University of Technology)
op_collection_id fttno
language English
description Tidal analysis has been carried out on current measurements at a “cross-shelf” transect off Greenland at 71o N. The diurnal tides manifest themselves mainly as a barotropic continental shelf wave, travelling southward along the shelf slope. This follows from the amplitude distribution of the diurnal tidal components and from the rotation sense of the tidal ellipses at different cross-slope locations, as calculated with simple two-dimensional models. The well organized cross-slope pattern of the velocity amplitudes is absent in observations further north near 75o N.These observations suggest that the local vanishing of the group velocity, which is caused by topography, is of importance for the existence and local amplification of these continental shelf waves with diurnal tidal frequency.
format Article in Journal/Newspaper
author Lam, F.P.A.
spellingShingle Lam, F.P.A.
Shelf waves with diurnal tidal frequency at the Greenland shelf edge:
author_facet Lam, F.P.A.
author_sort Lam, F.P.A.
title Shelf waves with diurnal tidal frequency at the Greenland shelf edge:
title_short Shelf waves with diurnal tidal frequency at the Greenland shelf edge:
title_full Shelf waves with diurnal tidal frequency at the Greenland shelf edge:
title_fullStr Shelf waves with diurnal tidal frequency at the Greenland shelf edge:
title_full_unstemmed Shelf waves with diurnal tidal frequency at the Greenland shelf edge:
title_sort shelf waves with diurnal tidal frequency at the greenland shelf edge:
publishDate 1999
url http://resolver.tudelft.nl/uuid:661dc1ea-ab7d-45b8-a274-3dee7891c072
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_source Deep Sea Research Part I: Oceanographic Research Papers, May, 5, 46, 895-923
op_relation uuid:661dc1ea-ab7d-45b8-a274-3dee7891c072
186410
http://resolver.tudelft.nl/uuid:661dc1ea-ab7d-45b8-a274-3dee7891c072
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