orographic

At other times of year, the air can be forced up the mountain resulting in orographic rain.

Orographic barriers in the path of a wind force it to rise.

Orographic activity is a factor contributing to the heavy rainfall.

Orographic lift occurs as air masses rise to pass over high ground.

Geographically, it is the source of Orographic precipitation for the capital city.

It is often associated with orographic lift caused by the escarpment.

Their proximity to the ocean and through orographic effect, they receive high rainfall.

Rainfall can be abundant at times, as mountains very close to the coast create an orographic effect.

Precipitation induced by orographic lift occurs in many places throughout the world.

Relief district land is divided into the following major orographic units:

This is because of something called orographic lift.

Shillong receives far less precipitation due to the orographic effect.

The geological constitution is in accordance with the orographic physiognomy.

As air flows over mountain barriers, orographic lift can create a variety of cloud effects.

The major part of the rainfall at Cherrapunji can be attributed to the orographic features.

Surface air circulation is largely influenced by orographic lift.

These are the main cause of the substantial orographic precipitation all over the Indian subcontinent.

As with Virginia, the heaviest rainfall occurred due to orographic lift near a mountain.

These areas are dry because the lie in the orographic rain shadow of the Blue Mountains.

Orographic fog is formed as the air rises up the slope and will often envelope the summit.

This type of precipitation is orographic in nature.

One could still hardly speak of dense topographic, orographic and hydrological information.

Orographic lifting on the eastern and western sides of the Sudd contribute to that condition.

In meteorology this is known as orographic lift.

Due to the orographic rainfall on the surrounding mountain ranges the climate is relatively damp as well.