0079 6611/98 $32.(X) Dynamics of the long-period tides
Abstract- The long-period tides are a tool for understanding oceanic motions at low frequencies and large scales. Here we review observations and theory of the fortnightly, monthly and pole tide constitutents. Observations have been plagued by low signal-to-noise ratios and theory by the complex lat...
Main Authors: | , , , |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.389.8936 http://ocean.mit.edu/~cwunsch/papersonline/wunschetal_lptides1997.pdf |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.389.8936 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.389.8936 2023-05-15T17:34:12+02:00 0079 6611/98 $32.(X) Dynamics of the long-period tides Carl Wunsch L Dale B. Haidvogel Mohamed Iskandarani R. Hughes The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.389.8936 http://ocean.mit.edu/~cwunsch/papersonline/wunschetal_lptides1997.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.389.8936 http://ocean.mit.edu/~cwunsch/papersonline/wunschetal_lptides1997.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://ocean.mit.edu/~cwunsch/papersonline/wunschetal_lptides1997.pdf text ftciteseerx 2016-09-18T00:43:01Z Abstract- The long-period tides are a tool for understanding oceanic motions at low frequencies and large scales. Here we review observations and theory of the fortnightly, monthly and pole tide constitutents. Observations have been plagued by low signal-to-noise ratios and theory by the complex lateral geometry and great sensitivity to bottom slopes. A new spectral element model is used to compute the oceanic response to tidal forcing at 2-week and monthly periods. The general response is that of a heavily damped (Q ~- 5) system with both the energy input from the moon and the dissipation strongly localized in space. The high dissipation result is probably generally applicable to all low frequency barotropic oceanic motions. Over much of the ocean, the response has both the character of a large-scale and a superposed Rossby wave-like character, thus vindicating two apparently conflicting earlier interpretations. To the extent that free waves are excited they are consistent with their being dominated by Rossby and topographic Rossby wave components, although gravity modes are also necessarily excited to some degree. In general, a modal representation is not very helpful. The most active regions are the Southern Ocean and the western and northern North Atlantic. These results are stable to changes in geometry, topography, and tide period. On a global average basis, the dynamical response of Mm is closer to equilibrium than is Text North Atlantic Southern Ocean Unknown Southern Ocean |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
Abstract- The long-period tides are a tool for understanding oceanic motions at low frequencies and large scales. Here we review observations and theory of the fortnightly, monthly and pole tide constitutents. Observations have been plagued by low signal-to-noise ratios and theory by the complex lateral geometry and great sensitivity to bottom slopes. A new spectral element model is used to compute the oceanic response to tidal forcing at 2-week and monthly periods. The general response is that of a heavily damped (Q ~- 5) system with both the energy input from the moon and the dissipation strongly localized in space. The high dissipation result is probably generally applicable to all low frequency barotropic oceanic motions. Over much of the ocean, the response has both the character of a large-scale and a superposed Rossby wave-like character, thus vindicating two apparently conflicting earlier interpretations. To the extent that free waves are excited they are consistent with their being dominated by Rossby and topographic Rossby wave components, although gravity modes are also necessarily excited to some degree. In general, a modal representation is not very helpful. The most active regions are the Southern Ocean and the western and northern North Atlantic. These results are stable to changes in geometry, topography, and tide period. On a global average basis, the dynamical response of Mm is closer to equilibrium than is |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Carl Wunsch L Dale B. Haidvogel Mohamed Iskandarani R. Hughes |
spellingShingle |
Carl Wunsch L Dale B. Haidvogel Mohamed Iskandarani R. Hughes 0079 6611/98 $32.(X) Dynamics of the long-period tides |
author_facet |
Carl Wunsch L Dale B. Haidvogel Mohamed Iskandarani R. Hughes |
author_sort |
Carl Wunsch L |
title |
0079 6611/98 $32.(X) Dynamics of the long-period tides |
title_short |
0079 6611/98 $32.(X) Dynamics of the long-period tides |
title_full |
0079 6611/98 $32.(X) Dynamics of the long-period tides |
title_fullStr |
0079 6611/98 $32.(X) Dynamics of the long-period tides |
title_full_unstemmed |
0079 6611/98 $32.(X) Dynamics of the long-period tides |
title_sort |
0079 6611/98 $32.(x) dynamics of the long-period tides |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.389.8936 http://ocean.mit.edu/~cwunsch/papersonline/wunschetal_lptides1997.pdf |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
North Atlantic Southern Ocean |
genre_facet |
North Atlantic Southern Ocean |
op_source |
http://ocean.mit.edu/~cwunsch/papersonline/wunschetal_lptides1997.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.389.8936 http://ocean.mit.edu/~cwunsch/papersonline/wunschetal_lptides1997.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766132965709971456 |