Tidal energy in the Bering Sea

Journal of Marine Research

Volumn 64, Issue 6, 2006, Pages 797-818

  Foreman, M G G ^a   Cummins, P F ^a   Cherniawsky, J Y ^a   Stabeno, Phyllis ^b  

^a INSTITUTE OF OCEAN SCIENCES   (Canada)

^b NOAA EARTH SYSTEM RESEARCH LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BAROTROPIC TIDE; CONTINENTAL SHELF; DIURNAL VARIATION; ENERGY BUDGET; ENERGY FLUX; FINITE ELEMENT METHOD; MIXING; PRESSURE GRADIENT; SHELF WAVE; TIDAL POWER; TOPEX-POSEIDON;

BERING SEA; PACIFIC OCEAN;

CLUPEIDAE; DECAPODA (CRUSTACEA); HIPPOGLOSSUS STENOLEPIS; MALLOTUS (FISH); MELANOGRAMMUS;

EID: 33847034024     PISSN: 00222402     EISSN: None     Source Type: Journal    
DOI: 10.1357/002224006779698341     Document Type: Article

References (45)

1. Bennett, A. F. 1992. Inverse Methods in Physical Oceanography. Monographs on Mechanics and Applied Mathematics, Cambridge University Press, Cambridge UK, 346 pp.
2. Bennett, A. F. 2002. Inverse Modeling of the Ocean and Atmosphere, Cambridge University Press, Cambridge UK, 234 pp.
3. Casulli, V. and R. A. Walters. 2000. An unstructured grid, three-dimensional model based on the shallow water equations. Int. J. Num. Methods in Fluids, 32, 331-348.
4. Cerveny, R. S. and J. A. Shaffer. 2001. The moon and El Niño. Geophys. Res. Lett., 28, 25-28.
5. Cherniawsky, J. Y., M. G. G. Foreman, W. R. Crawford and R. F. Henry. 2001. Ocean tides from TOPEX/POSEIDON sea level data. J. Atmos. Oceanic Tech., 18, 649-664.
6. Cummins, P. F., J. Y. Cherniawsky and M. G. G. Foreman. 2001. Internal tide generation along the Aleutian Ridge. J. Mar. Res., 59, 167-191.
7. Cummins, P. F., D. Masson and M. G. G. Foreman. 2000. Stratification and mean flow effects on diurnal tidal currents off Vancouver Island. J. Phys. Oceanogr., 30, 15-30.
8. Egbert, G. D. 1997. Tidal data inversion: interpolation and inference. Prog. Oceanogr., 40, 53-80.
9. Egbert, G. D., A. F. Bennett and M. G. G. Foreman. 1994. TOPEX/POSEIDON tides estimated using a global inverse model. J. Geophys. Res., 99, 24,821-24,852.
10. Egbert, G. D. and S. Y. Erofeeva. 2002. Efficient inverse modelling of barotropic ocean tides. J. Atmos. Oceanic Tech., 19, 183-204.
11. Egbert, G. D. and R. D. Ray. 2000. Significant tidal dissipation in the deep ocean inferred from satellite altimeter data. Nature, 405, 775-778.
12. Egbert, G. D. and R. D. Ray. 2001. Estimates of M2 tidal energy dissipation from TOPEX POSEIDON altimetry data. J. Geophys. Res., 106, 22,475-22,502.
13. Egbert, G. D. and R. D. Ray. 2003. Semi-diumal and diurnal tidal dissipation from TOPEX/POSEIDON altimetry. Geophys. Res. Lett., 30, 1907, doi:10.1029/2003GL017676.
14. Foreman, M. G. G., W. R. Crawford, J. Y. Cherniawsky, R. F. Henry and M. R. Tarbotton. 2000. A high-resolution assimilating tidal model for the northeast Pacific Ocean. J. Geophys. Res. 105, 28,629-28,651.
15. Foreman, M. G. G. and E. T. Neufeld. 1991. Harmonic tidal analysis of long time series. Int. Hydrographic Review, LXVIII(1), 85-108.
16. Foreman, M. G. G., G. Sutherland, and P. F. Cummins. 2004. Tidal dissipation around Vancouver Island: An inverse approach. Cont. Shelf Res., 24, 2167-2185.
17. Foreman, M. G. G., and R. E. Thomson. 1997. Three-dimensional model simulations of tides and buoyancy currents along the west coast of Vancouver Island. J. Phys. Oceanogr., 27, 1300-1325.
18. Godin, G. 1972. The Analysis of Tides, University of Toronto Press, Toronto, 264 pp.
19. Grebmeier, J. M., J. E. Overland, S. E. Moore, E. V. Farley, E. C. Carmack, L. W. Cooper, K. E. Frey, J. H. Helle, F. A. McLaughlin and S. L. McNutt. 2006. A major ecosystem shift in the northern Bering Sea. Science, 311, 1461-1464.
20. Greenberg, D. A., F. E. Werner and D. R. Lynch. 1998. A diagnostic finite element ocean circulation model in spherical polar coordinates, J. Atmos. Oceanic Technol., 15, 942-958.
21. Heiskanen, W. 1921. Über den Einfluß der Gezeiten auf die säkulare Acceleration des Mondes, Ann. Acad. Sci. Fennicae (A), 18, 1-84.
22. Henry, R. F. and R. A. Walters. 1993. A geometrically-based, automatic generator for irregular triangular networks. Commun. Numer. Methods Eng., 9, 555-566.
23. Jeffreys, H. 1921. Tidal friction in shallow seas. Phil. Trans. Roy. Soc. London, A, 221, 239-264.
24. Johnson, W. R. and Z. Kowalik. 1986. Modeling of storm surges in the Bering Sea and Norton Sound. J. Geophys. Res., 91, 5119-5128.
25. Kantha, L. 1995. Barotropic tides in the global oceans from a nonlinear tidal model assimilating altimetric tides. 1. Model description and results. J. Geophys. Res. 100, 25,283-25,308.
26. Kantha, L., C. Tierney, J. Lopez, S. D. Desai, M. E. Parke and L. Drexler. 1995. Barotropic tides in the global oceans from a nonlinear tidal model assimilating altimetric tides. 2. Altimetric and geophysical implications. J. Geophys. Res., 100, 25,309-25,317.
27. Kowalik, Z. 1999. Bering Sea tides, in Dynamics of the Bering Sea, T. R. Loughlin and K. Ohtani, eds., University of Alaska Sea Grant, Fairbanks, 825 pp.
28. 2 barotropic ocean tides: an estimate of bottom friction dissipation from a hydrodynamic model. Prog. Oceanogr., 40, 37-52.
29. Liu, S. K., and J. J. Leendertse. 1982. Three-dimensional model of Bering and Chukchi Sea, Coastal Eng., 18, 598-616.
30. Loder, J. W. and C. Garrett. 1978. The 18.6-year cycle of sea surface temperature in shallow seas due to tidal mixing, J. Geophys. Res., 83, 1967-1970.
31. Lynch, D. R. 1985. Mass balance in shallow water simulations. Communications in Applied Numerical Methods, I, 153-159.
32. Lynch, D. R. and W. G. Gray. 1979. A wave-equation model for finite-element tidal computations. Computers in Fluids, 7, 207-228.
33. Lynch, D. R. and F. E. Werner. 1987. Three-dimensional hydrodynamics on finite elements. Part I: Linearized harmonic model. Int. J. Numerical Methods in Fluids, 7, 871-909.
34. Miller, G. 1966. The flux of tidal energy out of the deep oceans. J. Geophys. Res., 71, 2485-2489.
35. Mofjeld, H. O. 1986. Observed tides on the northeastern Bering Sea shelf. J. Geophys. Res., 91, 2593-2606.
36. Munk, W. 1997. Once again: once again - tidal friction. Prog. Oceanogr., 40, 7-35.
37. Osafune, S. and I. Yasuda. 2006. Bidecadal variability in the intermediate waters of the northwestern subarctic Pacific and the Okhotsk Sea in relation to 18.6-year period nodal tidal cycle. J. Geophys. Res., 111, doi:10.1029/2005JC003277.
38. Parker, K. S., T. C. Royer, and R. B. Deriso. 1995. High-latitude climate forcing and tidal mixing by the 18.6-year lunar nodal cycle and low-frequency recruitment trends in Pacific halibut (Hippoglossus stenolepis), in Climate Change and Northern Fish Populations, R. J. Beamish, ed., Can. Special Pub. of Fisheries and Aquatic Sciences, 121, 447-459.
39. Pugh, D. T. 1996. Tides Surges and Mean Sea-Level. Wiley, N.Y., 472 pp.
40. Ray, R. D. 1998. Ocean self-attraction and loading in numerical tidal models, Mar. Geod., 21, 181-192.
41. Royer, T.C. 1993. High-latitude oceanic variability associated with the 18.6-year nodal tide. J. Geophys. Res., 98, 4639-4644.
42. Smith, W. H. F. and D. T. Sandwell. 1997. Global sea floor topography from satellite altimetry and ship depth soundings, Science, 277, 1956-1962.
43. Stabeno, P. J., D. G. Kachel, N. B. Kachel and M. E. Sullivan. 2005. Observations from moorings in the Aleutian Passes: temperature, salinity and transport. Fisheries Oceanography, 14, 39-54.
44. Sündermann, J. 1977. The semi-diurnal principal lunar tide M2 in the Bering Sea, Deutsche Hydrographische Zeitschrift, 30, 91-101.
45. Yndestad, H. 2004. The cause of Barents Sea biomass dynamics. J. Mar. Sys., 44, 107-124.