Abstract
Some aspects of the upper ocean layer dynamics are considered, including the Ekman transport, the relation of the thickness of the quasi-homogeneous layer to the thickness of the layer of rotation of the drift current vector, and the correlation between the level of the turbulent energy dissipation and the thickness of the quasi-homogeneous layer.
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V. P. Tereshchenkov, S. M. Shapovalov, S. A. Dobrolyubov, and E. G. Morozov, “Cruise 9 of R/V Akademik Ioffe,” Okeanologiya 42(2), 315–318 (2002) [Oceanology 42 (2), 298–301 (2002)].
T. K. Chereskin and D. Roemmich, “A Comparison of Measured and Wind-Derived Ekman Transport at 11° N in the Atlantic Ocean,” J. Phys. Oceanogr. 21(6), 869–878 (1991).
J. R. N. Lazier and D. G. Wright, “Annual Velocity Variations in the Labrador Current,” J. Phys. Oceanogr. 23(4), 659–678 (1993).
L. H. Kantha and C. A. Clayson, Numerical Models of Oceans and Oceanic Processes (International Geophysics) (Academic, 2000), Vol. 66.
L. H. Kantha and C. A. Clayson, Small-Scale Processes in Geophysical Fluid Flows (International Geophysics), (Academic, 2000), Vol. 67.
A. B. Kara, P. A. Rochford, and H. E. Hurlburt, “An Optimal Definition for Ocean Mixed Layer Depth,” J. Geophys. Res, Oceans 105(C7), 16 803–16 821 (2000).
I. Lozovatsky, M. Figueroa, E. Roget, et al., “Observations and Scaling of the Upper Mixed Layer in the North Atlantic,” J. Geophys. Res. 110, C05013 (2005), doi:10.1029/2004JC002708.
R. T. Pollard and J. Read, “A Method for Calibrating Shipmounted Acoustic Doppler Profilers and the Limitations of Gyro Compasses,” J. Atmosp. Oceanic Technol. 6(C6), 859–865 (1989).
H. Prandke and A. Stips, “Test Measurements with an Operational Microstructure-Turbulence Profiler: Detection Limit of Ddissipation Rates,” Aquatic Sciences 60(3), 191–209 (1998).
H. Prandke, K. Holtsch, and A. Stips, MITEC Technology Development: The Microstructure-Turbulence Measuring System MSS (Tech. Rep. EUR 19733) (EASTERN, European Commission, Joint Research Center, Ispra, Italy, 2000).
J. E. Price, R. A. Weller, and R. Pinkel, “Diurnal Cycling: Observations and Models on the Upper Ocean Response to Diurnal Heating, Cooling, and Wind Mixing,” J. Geophys. Res. 91(C7), 8411–8427 (1986).
I. Lozovatsky, E. Roget, and H. J. S. Fernando, “Mixing in Shallow Waters: Measurements, Processing, and Applications,” J. of Ocean (University of China, Oceanic and Coastal Sea Research) 4(4), 167–180 (2005).
S. D. Smith, “Coefficients for Sea-Surface Wind Stress, Heat-Flux, and Wind Profiles As a Function of Wind-Speed and Temperature,” J. Geophys. Res. 93(C12) 15 467–15 472 (1988).
S. E. Wijffels, E. Firing, and H. L. Bryden, “Direct Observations of the Ekman Balance at 10° in the Pacific,” J. Phys. Oceanogr. 24, 1666–1679 (1994).
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Original Russian Text © I.D. Lozovatskii, S.M. Shapovalov, E. Roget, 2006, published in Okeanologiya, 2006, Vol. 46, No. 1, pp. 5–13.
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Lozovatskii, I.D., Shapovalov, S.M. & Roget, E. Ageostrophic dynamics of the upper ocean layer: Measurements over the transatlantic section along 53° N. Oceanology 46, 1–9 (2006). https://doi.org/10.1134/S0001437006010012
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DOI: https://doi.org/10.1134/S0001437006010012