From AMS Glossary
- For continuously stratified, nonrotating, dry, inviscid 2D flow over an obstacle of height h, with incoming wind speed U, and upstream Brunt-väisälä frequency N, the quantity U/(Nh) yields a measure of whether there will be an upstream-propagating region of decelerated flow and, hence, is also sometimes referred to as the Froude number. For U/(Nh) >> 1, the flow ascends over the obstacle with no upstream deceleration. For U/(Nh) << 1, a region of upstream flow deceleration forms that may propagate continuously upstream with time. Note that referring to the above relation as the Froude number is not consistent with the classical definition of Fr (see definition 1 above). For consistency with the original definition of Fr, some advocate referring to the relation Nh/U (the inverse of Fr as it is defined herein) as the nondimensional mountain height.
term edited 12 Dec 2014