lenticular clouds mountain

However, these waves can be present beyond the clouds, and may exist even when no clouds are formed.

However, these waves can be present beyond the clouds, and may exist even when no clouds are formed.On the ground, they can result in very strong gusty winds in one place, with still air only a few hundred metres away.There are three main types of lenticular clouds: altocumulus standing lenticular (ACSL), stratocumulus standing lenticular (SCSL), and cirrocumulus standing lenticular (CCSL), varying in altitude above the ground. If there is enough moisture in the air, the rising motion of the wave will cause water vapour to condense, forming the unique appearance of lenticular clouds.Lenticular clouds are a visible sign of mountain waves in the air. These include both natural features of the Earth, such as mountains or hills, and artificial structures, such as buildings and other structures. Lenticular Cloud (as defined by NOAA) A very smooth, round or oval, lens-shaped cloud that is often seen, singly or stacked in groups, near or in the lee of a mountain … As air travels along the surface of the Earth, obstructions are often encountered. Wind blows most types of clouds across the sky, but lenticular clouds seem to … As air travels along the surface of the Earth, obstructions are often encountered. However, these waves can be present beyond the clouds, and may exist even when no clouds are formed. These disrupt the flow of air into "eddies", or areas of turbulence influenced by these obstructions. A lenticular cloud is a lens-shaped cloud that normally develops on the downwind side of a mountain or mountain range. Lenticular clouds are a visible sign of mountain waves in the air. Lenticular, or lee wave, clouds form downwind of an obstacle in the path of a strong air current. Lenticular clouds are a visible sign of mountain waves in the air. These include both natural features of the When moist, stable air flows over a larger eddie, such as those caused by Lenticular clouds have been said to be mistaken for Pilots of powered aircraft tend to avoid flying near lenticular clouds because of the turbulence and sinking air of the rotor generated at the trailing edge of these clouds, but Lenticular clouds have also been known to form in cases where a mountain does not exist, but rather as the result of shear winds created by a front. These lens-shaped orographic wave clouds form when the air is stable and winds blow across hills and mountains from the same or similar direction at different heights through the troposphere.All high clouds are a type of cirrus, a common cloud that can be seen at any time of the year.Cirrocumulus is a relatively rare cloud, forming ripples which may resemble honeycomb.The techniques used in data collection from space including the use of geo-stationary and polar orbiting s…Everything you need to know about the forecast, and making the most of the weather.The latest breakthroughs, research and news from the Met Office.Support your business with world-leading science and technology.These strange, unnatural looking clouds sometimes form downwind of hills or mountains.When air blows across a mountain range, in certain circumstances, it can set up a train of large standing waves in the air downstream, rather like ripples forming in a river when water flows over an obstruction. Lenticular clouds are saucer-shaped clouds that are often witnessed over mountains and mountain ranges.

In the Boulder, Colorado area, the obstacle is the Front Range of the Rocky Mountains, seen at the bottom of the picture.

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