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The solution has a pressure force acting on the ridge, which represents the orographic drag.
Zones (windward and leeward) were designated in respect to the central massif whose orographic influences result in a marked precipitation gradient.
The anticyclonic vortex generated by the orographic vortex compression (p > 0) has associated with it a positive free surface deflexion.
The heaviest rainfall occurred through a process called orographic lift in the mountainous interior, leading to hundreds of landslides.
This energy comes from fronts, heating, moistening, or mesoscale convergence boundaries such as outflow and sea breeze boundaries, or orographic lift.
Convective precipitation events (thunderstorms) tend to produce shorter duration storm events than orographic precipitation.
Cirrocumulus lenticularis forms when stable air is forced upward; this is usually due to orographic features, but can occur away from mountains as well.
Marked orographic enhancement over this terrain is evident on radar imagery.
There, the rains were enhanced by moist air rising over the mountain peaks and condensing, a process known as orographic lift.
Such heavy rainfall typically occurs on the island when tropical cyclones approach, owing to orographic enhancement in the mountainous interior.
Mechanisms of producing precipitation include convective, stratiform, and orographic rainfall.
Rainfall can be abundant at times, as mountains very close to the coast create an orographic effect.
Because of orographic lift, precipitation increases with elevation up to 8000 ft where it slowly decreases to the crest.
The effect is enhanced when the moving air mass is uplifted by the orographic effect of higher elevations on the downwind shores.
It forms above the mountain range, usually at the beginning of a chinook wind as a result of orographic lifting over the range.