The Internal Seiches in Gullmar Fjord. Part II: Contribution to Basin Water Mixing
Open Access
- 1 September 2001
- journal article
- Published by American Meteorological Society in Journal of Physical Oceanography
- Vol. 31 (9) , 2567-2574
- https://doi.org/10.1175/1520-0485(2001)031<2567:tisigf>2.0.co;2
Abstract
The mixing in the basin water (the water below sill level) of Gullmar Fjord has been investigated with the main focus on the contribution from internal seiches. A companion paper reports evidence for dissipation of internal seiche energy in the basin water after near-critical reflection from the bottom. In the present paper the magnitude and variation of basin water mixing is investigated, using the budget method. The results are related to variations of three energy sources, namely (i) the internal seiches, (ii) the internal tides, and (iii) the internal waves generated by the external seiche. The mixing efficiency, defined as the irreversible work against buoyancy forces due to mixing divided by the total mechanical energy loss from the sources mentioned above, is about 7%, similar to results obtained for other fjords. Large variations in mixing are shown to be related to large variations of the energy sources. The internal seiches are found to be important for the mixing, with a contribution t... Abstract The mixing in the basin water (the water below sill level) of Gullmar Fjord has been investigated with the main focus on the contribution from internal seiches. A companion paper reports evidence for dissipation of internal seiche energy in the basin water after near-critical reflection from the bottom. In the present paper the magnitude and variation of basin water mixing is investigated, using the budget method. The results are related to variations of three energy sources, namely (i) the internal seiches, (ii) the internal tides, and (iii) the internal waves generated by the external seiche. The mixing efficiency, defined as the irreversible work against buoyancy forces due to mixing divided by the total mechanical energy loss from the sources mentioned above, is about 7%, similar to results obtained for other fjords. Large variations in mixing are shown to be related to large variations of the energy sources. The internal seiches are found to be important for the mixing, with a contribution t...Keywords
This publication has 16 references indexed in Scilit:
- The Internal Seiches in Gullmar Fjord. Part I: DynamicsJournal of Physical Oceanography, 2001
- Boundary mixing and nutrient fluxes in Mono Lake, CaliforniaLimnology and Oceanography, 1999
- On the variability of Baltic Sea deepwater mixingJournal of Geophysical Research: Oceans, 1998
- Boundary versus internal diapycnal mixing in stratified natural watersJournal of Geophysical Research: Oceans, 1997
- Observed Damping of Barotropic Seiches through Baroclinic Wave Drag in the Gullmar FjordJournal of Physical Oceanography, 1997
- Spatial Variability of Turbulent Mixing in the Abyssal OceanScience, 1997
- A tracer study of mixing in the Santa Cruz BasinJournal of Geophysical Research: Oceans, 1995
- Observations of the second vertical mode of the internal seiche in an alpine lakeLimnology and Oceanography, 1992
- On the Nature of Turbulence in a Stratified Fluid. Part II: Application to LakesJournal of Physical Oceanography, 1991
- Vertical eddy diffusivity in the ocean interiorJournal of Marine Research, 1984