This work should be regarded as a natural development of the investiga
tions by Dolzhanskii, Krymov and Manin [Sov. Phys. Usp. 33, 495-520 (1
990); J. Fluid Mech. 241, 705-722 (1992); Russ. J. Comput. Model. 1, 1
07-118 (1993)] of quasi-two-dimensional (Q2D) flows in which the linea
r and weakly nonlinear stability theory based on the 2D hydrodynamic e
quations with the Rayleigh (Ekman) friction term imitating the influen
ce of the bottom on the motion of upper fluid layers was corroborated
with laboratory and observational data. The applicability of the Q2D a
pproach to describe self-oscillating supercritical regimes was even mo
re vague as Batchaev's experiments [Izv. AN SSSR Fit. Atmos. Okeana 25
, 434-439 (1989); Z. Prikl. Mech. Tech. Fit., No. 4, 85-91 (1990)] on
modeling the four vortex self-oscillations in a thin fluid layer by th
e magnetohydrodynamics method (the so called hydrodynamical clock [Obu
khov, Dolzhanskii and Batchaev, Topological Fluid Mechanics, Proceedin
gs of the IUTAM Symposium, Cambridge, 13-18 August 1989 (Cambridge Uni
versity Press, Cambridge, 1989), pp. 304-314]) did not find an appropr
iate theoretical explanation. To remove earlier uncontrolled effects t
he supplementary detailed measurements of the experimental flow charac
teristics were implemented, including the spatial spectral composition
of the external vorticity sources and free surface 2D velocity fields
. Satisfactory agreement is found between experimentally measured flow
characteristics and the results of numerical simulations. The frequen
cy of self-oscillations was found to be greatly susceptible to the spe
ctral composition of the external vorticity sources and fluid layer th
ickness, which should be taken into account in designing laboratory ex
periments to simulate the natural Q2D processes observed in the ocean
and atmosphere. Applicability conditions of the Q2D approach and the i
nfluence of geometrical parameters of vortices on their nonlinear inte
rplay are also discussed. (C) 1996 American Institute of Physics.