The team directly measured terms in
turbulence model equations, providing insights into the global nature of the mixing (e.g., faster mixing near the edges of the turbulent fluid layer when compared with the core) and identifying the dominant mechanisms governing the flow evolution.
Not exact matches
Equations for shallow atmospheric motions; thermal instability of a fluid layer; atmospheric
turbulence; flow stability; 1 - D mixed layer
models
In this
model the standard set of
equations plus some additional numerical schemes are combined to find the dependence of some variable of interest (in this case, hurricane velocity V) on other variables and parameters, of which one is the
turbulence length scale hl.