Three interconnected prospective problems of the ocean fluid dynamics
are considered: the oscillations of the World ocean general circulatio
n and the climate (''synergetic'' oscillations with multimonthly perio
ds in the system ''large-scale flows - synoptic eddies'', the oscillat
ions with rotation periods of the giant anticyclonic gyres and oscilla
tions of the World ocean ''conveyor belt'' thermohaline circulation wi
th periods of decades and hundreds of years); subsynoptic eddies and o
ther coherent mesostructures; and, finally, mesostructures in the form
of convective plumes above bottom geysers - the so called ''black smo
kers''. The prospects of studies of these problems and necessary new m
ethodology and equipment are discussed.