Geostrophic momentum approximation
From AMS Glossary
geostrophic momentum approximation
The approximation is usually made in conjunction with the assumption that the Coriolis parameter f is a constant, in which case it takes the form
where u, v, and w are the eastward, northward, and upward components of the total wind, ρ is the density, p the pressure, and
the eastward and northward components of the geostrophic wind. In the geostrophic momentum approximation the geostrophic wind is the advected quantity but the advection is by the total (geostrophic plus ageostrophic) wind. When the geostrophic momentum approximation is combined with geostrophic coordinates, the resulting equations are termed the semigeostrophic equations.