Fronts in the Irish Sea¶
Simpson, & Hunter. (1974). Fronts in the Irish Sea. Nature.
Cited by¶
1 citation across 1 artifact.
Each citation links to the sentence it supports in the citing article.
Domain-specific¶
- Tidal Mixing
- The primary mechanism is bottom-boundary-layer shear: tidal currents flowing over the seabed generate turbulence that entrains and mixes the density-stratified water above, with mixing power proportional to the cube of current speed
This sourceThe summer front in the western Irish Sea separating stratified from vertically mixed water. A model accounting for the form and stable position of the shelf-sea tidal front. Simpson and Hunter's 1974 Nature paper on the summer front in the western Irish Sea. A model accounting for the observed form and stable position of the Irish Sea front.
Supported in partVerified against the publisher's abstract
“This feature is the boundary between stratified and vertically mixed regimes”
- The primary mechanism is bottom-boundary-layer shear: tidal currents flowing over the seabed generate turbulence that entrains and mixes the density-stratified water above, with mixing power proportional to the cube of current speed
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Registry ID ref:3d356aa84896 · see in the full table