On the Torques Due to Tidal Friction of the Oceans and Adjacent Seas

The torques of the frictional forces on the bottoms of the seas are calculated in an approximate inertial system and not in the corotating system used hitherto. In this way, the loss of rotational energy of the Earth – corresponding to the mean torque – can be compared with the value obtained from a...

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Bibliographic Details
Published in:Symposium - International Astronomical Union
Main Authors: Brosche, P., Sündermann, J.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1972
Subjects:
Bering Sea
Online Access:http://dx.doi.org/10.1017/s0074180900098478
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0074180900098478
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spelling crcambridgeupr:10.1017/s0074180900098478 2024-03-03T08:43:15+00:00 On the Torques Due to Tidal Friction of the Oceans and Adjacent Seas Brosche, P. Sündermann, J. 1972 http://dx.doi.org/10.1017/s0074180900098478 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0074180900098478 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Symposium - International Astronomical Union volume 48, page 235-239 ISSN 0074-1809 journal-article 1972 crcambridgeupr https://doi.org/10.1017/s0074180900098478 2024-02-08T08:44:37Z The torques of the frictional forces on the bottoms of the seas are calculated in an approximate inertial system and not in the corotating system used hitherto. In this way, the loss of rotational energy of the Earth – corresponding to the mean torque – can be compared with the value obtained from astronomical observations. The calculations are based on velocities which are computed by numerical integrations of the hydrodynamical equations. Initial results are presented for the North Sea, the Bering Sea and rough models of theworld ocean. Article in Journal/Newspaper Bering Sea Cambridge University Press Bering Sea Symposium - International Astronomical Union 48 235 239
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description The torques of the frictional forces on the bottoms of the seas are calculated in an approximate inertial system and not in the corotating system used hitherto. In this way, the loss of rotational energy of the Earth – corresponding to the mean torque – can be compared with the value obtained from astronomical observations. The calculations are based on velocities which are computed by numerical integrations of the hydrodynamical equations. Initial results are presented for the North Sea, the Bering Sea and rough models of theworld ocean.
format Article in Journal/Newspaper
author Brosche, P.
Sündermann, J.
spellingShingle Brosche, P.
Sündermann, J.
On the Torques Due to Tidal Friction of the Oceans and Adjacent Seas
author_facet Brosche, P.
Sündermann, J.
author_sort Brosche, P.
title On the Torques Due to Tidal Friction of the Oceans and Adjacent Seas
title_short On the Torques Due to Tidal Friction of the Oceans and Adjacent Seas
title_full On the Torques Due to Tidal Friction of the Oceans and Adjacent Seas
title_fullStr On the Torques Due to Tidal Friction of the Oceans and Adjacent Seas
title_full_unstemmed On the Torques Due to Tidal Friction of the Oceans and Adjacent Seas
title_sort on the torques due to tidal friction of the oceans and adjacent seas
publisher Cambridge University Press (CUP)
publishDate 1972
url http://dx.doi.org/10.1017/s0074180900098478
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0074180900098478
geographic Bering Sea
geographic_facet Bering Sea
genre Bering Sea
genre_facet Bering Sea
op_source Symposium - International Astronomical Union
volume 48, page 235-239
ISSN 0074-1809
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0074180900098478
container_title Symposium - International Astronomical Union
container_volume 48
container_start_page 235
op_container_end_page 239
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