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Observed Damping of Barotropic Seiches through Baroclinic Wave Drag in the Gullmar Fjord
Barotropic Seiches Baroclinic Wave Drag Gullmar Fjord
2008/11/18
Baroclinic wave drag, due to internal wave generation at steep topography, is shown to be a mechanism that effectively subdues barotropic seiches in fjords. A two-layer model for a fjord with a sill a...
The Internal Seiches in Gullmar Fjord. Part I: Dynamics
Internal Seiches Gullmar Fjord Dynamics
2008/8/1
Internal seiche motions with period 1–3 days in Gullmar Fjord are investigated based on mooring data with high vertical and time resolution. The period and structure of the internal seiches are well d...
The Internal Seiches in Gullmar Fjord. Part II: Contribution to Basin Water Mixing
Internal Seiches Gullmar Fjord Basin Water Mixing
2008/8/1
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 ...