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M2 1st mode wavelength from ORCA-4 climatology (Drakkar/LGGE)

Related publications:

Internal tides in the Bay ofBiscay: conversion rates and seasonal effects, Theo Gerkemaaet al., 2004

References

- Osborne, J. J., A. L. Kurapov, G. D. Egbert, P. M. Kosro, 2011: Spatial and Temporal Variability of the M2 Internal Tide Generation and Propagation on the Oregon Shelf. J. Phys. Oceanogr., 41, 2037–2062. DOI: http://dx.doi.org/10.1175/JPO-D-11-02.1

- Internal tides in the Bay of Biscay: conversion rates and seasonal effects, Gerkema, Theo; Lam, Frans–Peter A.; Maas, Leo R. M., Deep-Sea Research Part II, Volume 51, Issue 25-26, p. 2995-3008. DOI: http://dx.doi.org/10.1016/j.dsr2.2004.09.012

- Decay of semi-diurnal internal-tide beams due to subharmonic resonance, Theo Gerkema, Chantal Staquet, and Pascale Bouruet-Aubertot, GEOPHYSICAL RESEARCH LETTERS, VOL. 33, L08604. DOI : http://dx.doi.org/10.1029/2005GL025105, 2006

- Seasonal Variability of Surface and Internal M2 Tides in the Arctic Ocean, B. A. Kagan, A. A. Timofeev, and E. V. SofinaAtmospheric and Oceanic Physics, 2010, Vol. 46, No. 5, pp. 652–662 DOI: 10.1134/S0001433810050105