The function estimates the Grashof Number, which describes the ability of a parcel of fluid warmer or colder than the surrounding fluid to rise against or fall with the attractive force of gravity (Gates 1980) . The Grashof Number is estimated as the ratio of a buoyant force times an inertial force to the square of a viscous force.

Grashof_number_Gates(T_a, T_g, beta, D, nu)

Arguments

T_a

numeric Air temperature (C).

T_g

numeric Ground (surface) temperature (C).

beta

numeric coefficient of volumetric thermal expansion, beta = 3.67 x 10-3 C-1 in air and 41.9 x 10-4 C-1 in water.

D

numeric is characteristic dimension (e.g., body diameter) (m)

nu

numeric is the kinematic viscosity, the ratio of dynamic viscosity to density of the fluid (m2 s-1); can calculate from DRYAIR or WETAIR.

Value

numeric Grashof number.

References

Gates DM (1980). Biophysical Ecology. Springer-Verlag, New York, NY, USA.

Examples

  Grashof_number_Gates(T_a   = 30,
                       T_g   = 35,
                       beta = 0.00367,
                       D    = 0.001,
                       nu   = 1.2)
#> [1] 1.248819e-10