More formulas for those willing to take a crack on the wind idea:
http://www.usace.army.mil/publications/eng-manuals/em1110-2-1100/PartIII/Part-III-Chap_4entire.pdf
You would really have to go to the link; posting is not kind to the formulas.
q=BBagnold times (pa/g) times (the square root of [D/d] times u cubed
in which q = the mass transport rate in gm/cm-s, BBagnold = a coefficient, ρa = the mass density of the air =
0.001226 gm/cm3, d = a standard grain size = 0.25 mm, D = grain size in mm, and u* = the shear velocity in
cm/sec;
q=Zzing times (pa/g) times [D/d] to the 3/4 power times u cubed
in which ZZingg = a coefficient, and q, D, d, ρa, and u* are as in the previous expression.
(2) Chapman (1990) provides an evaluation of these and several other equations. The predictive
capability of the seven equations investigated by Chapman (1990), as gauged by the coefficient of
determination, ranged from r2 = 0.63 to r2 = 0.87 (see Table III-4-2).
http://www.usace.army.mil/publications/eng-manuals/em1110-2-1100/PartIII/Part-III-Chap_4entire.pdf
You would really have to go to the link; posting is not kind to the formulas.
q=BBagnold times (pa/g) times (the square root of [D/d] times u cubed
in which q = the mass transport rate in gm/cm-s, BBagnold = a coefficient, ρa = the mass density of the air =
0.001226 gm/cm3, d = a standard grain size = 0.25 mm, D = grain size in mm, and u* = the shear velocity in
cm/sec;
q=Zzing times (pa/g) times [D/d] to the 3/4 power times u cubed
in which ZZingg = a coefficient, and q, D, d, ρa, and u* are as in the previous expression.
(2) Chapman (1990) provides an evaluation of these and several other equations. The predictive
capability of the seven equations investigated by Chapman (1990), as gauged by the coefficient of
determination, ranged from r2 = 0.63 to r2 = 0.87 (see Table III-4-2).