We develop a Lagrangian model of both one-particleIn this paper ‘particle’ and ‘fluid element’
are synonymous. and two-particle turbulent
diffusion in high Reynolds number and low Froude number stably stratified non-
decaying turbulence. This model is a kinematic simulation (KS) that obeys both the
linearized Boussinesq equations and incompressibility. Hence, turbulent diffusion is
anisotropic and is studied in all three directions concurrently with incompressibility
satisfied at the level of each and every trajectory.
Horizontal one-particle and two-particle diffusions are found to be independent of
the buoyancy (Brünt–Väissälä) frequency N. For
one-particle diffusion we find that
formula here
and
formula here
where i = 1,2 and u′ and L are a r.m.s. velocity and a
length-scale of the energy-containing motions respectively, and
formula here
This capping of one-particle vertical diffusion requires the consideration of the entire
three-dimensional flow, and we show that each and every trajectory is vertically
bounded for all times if the Lagrangian vertical pressure acceleration a3 is bounded
for all times. Such an upper bound for a3 can be derived from the linearized Boussinesq
equations as a consequence of the coupling between vertical pressure acceleration and
the horizontal and vertical velocities.
Two-particle vertical diffusion exhibits two plateaux. The first plateau's scaling is
different according to whether the initial separation Δ0 between the two particles is
larger or smaller than η, the smallest length-scale of the turbulence:
formula here
The second plateau is reached when the two particles become statistically independent,
and therefore
formula here
The transition between the two plateaux coincides with the time when the two particles
start moving significantly apart in the horizontal plane.