0 violently disturbed or confused -- bouřlivý; vzrušený
the turbulent years of war.
The seas are turbulent
Analytic solutions have been derived to model each of the vertical and lateral stages of magma transport in both the laminar and turbulent regimes.
The gradient-transfer approximation is based on the hypothesis of a turbulent flux proportional to the gradient of the concentration.
Turbulent inflow data are provided by a separate zero-pressure-gradient boundary-layer simulation.
Furthermore, such flows cannot be easily distinguished from turbulent flows by qualitative observations.
We regard non-periodic motion as being weakly turbulent.
A new definition of concentration fluctuations in turbulent flows is proposed.
The constraint a2+p2= 1 ensures that the variance of the turbulent velocity is correct.
The evolution of the turbulent velocity field in these air data is far more coherent than were such measurements in water.
