Parameterizing tidal dissipation over rough topography

By S. Jayne, L. St. Laurent. 2001

414 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/639ab1c5b532c02e28004b241a378c87b60dc16e

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. S. Jayne
2. Samar Khatiwala
3. F. Nimmo
4. H. Simmons
5. Louis St. Laurent
6. K. Polzin
7. E. Chen
8. Gary A. Glatzmaier

In Global and Planetary Change

1. S. Jayne
2. Louis St. Laurent
3. H. Simmons
4. Gary A. Glatzmaier
5. E. Chen
6. F. Nimmo
7. Sonya Legg
8. Samar Khatiwala

In Oceanography

1. S. Jayne
2. Sonya Legg
3. K. Polzin
4. H. Simmons
5. Samar Khatiwala
6. Louis St. Laurent
7. Robert Hallberg
8. F. Nimmo

Citations in the corpus

• Numerical study of the spatial distribution of the M2 internal tide in the Pacific Ocean (2001, methodology): “946 following Kantha [1995] (It was pointed out by one of the reviewers that 0.”
• Numerical modeling of the global semidiurnal tide in the present day and in the last glacial maximum (2004, methodology): “[4] A great advance was the global finite-element solution of Le Provost et al. [1994]. The relatively close agreement of their solution with T/P measurements suggested that highly accurate solutions could be obtained with a purely hydrodynamic model, provided accurate bathymetry and numerical grids”
• Tidal heating in icy satellite oceans (2014, methodology): “Because internal tide generation is largely due to ocean bathymetry (Baines, 1973; Jayne and Laurent, 2001), a property which is completely unconstrained in the context of satellite oceans, we have ignored the effects of a stratified ocean.”
• Tidally driven mixing in a numerical model of the ocean general circulation (2003, methodology): “Previously, the global distribution of energy flux into the internal tides has been examined using observations and tidal models (Egbert and Ray, 2000, 2001; Jayne and St. Laurent, 2001; Niwa and Hibiya, 2001).”
• Generation of internal tides in an ocean of finite depth: analytical and numerical calculations (2003, background): “(1997) and Ledwell et al. (2000) based on measurements of microstructure and tracer dispersion convincingly show that diapycnal mixing (and the implied diffusivity) is strongly enhanced over rough bottom topography.”