Local Circulation

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Why does air circulate and what are the driving forces for this movement?

Energy from the Sun heats different parts of the Earth differently and this causes pressure differences to develop across the globe.  These pressure differences cause air to move.  The air moves from regions of high pressure to regions of low pressure to try to smooth out the pressure differences.    Air movement occurs on different scales, on a global scale (global circulation of the Earth), over a medium scale (tornadoes) and on a local scale (mountain winds). 

In some zones around the Earth, the winds blow predominantly in one direction and this is known as the prevailing wind direction.  This direction can change with the seasons.  Winds over most areas are variable in direction from day to day.   A wind is named according to the point of the compass from which it blows, i.e., a wind blowing from the north is a north wind.

1. Windmill (c) FreeFoto.com

Energy from the Sun is the most important driving force for winds but there are other forces, which are also important:

 

1. Horizontal Pressure Gradient 

                  - this causes horizontal force on the air mass and generates winds.

2. In absence of other forces, air moves from high to low pressure due to the "pressure gradient force"

We know that winds are generated by differences in air pressure.  The greater the difference in pressure, the stronger the force.  The distance between the area of high pressure and the area of low pressure also determines how fast the moving air is accelerated. Meteorologists refer to the force that starts the wind flowing as the "pressure gradient force".

2. Gravity
          
— this causes vertical pressure differences.  The force of gravity is constant for a given altitude.


3. Coriolis Force
           
— once the wind begins blowing, the rotation of the Earth affects its direction. This is the Coriolis effect.

3. Figure by Schlanger ©

The Corolis effect results in the deflection of all objects to the right in the Northern hemisphere and to the left in the Southern hemisphere. The Coriolis force moves large objects such as airmasses considerable distances.   Small objects, for example ships at sea, are too small to experience significant deflections in their direction due to the Coriolis Force.

4. Friction
          
— this has very little effect on air in the atmosphere, but is more important close to the ground. The effect of friction on air motion decreases as the altitude increases to a point (usually 1-2 km above the ground) where it has no effect at all.  The layer of the atmosphere where friction affects atmospheric motion is referred to as the boundary layer.


5. Centrifugal Force
        
— An object traveling in a circle behaves as if it experiences an outward force. This force, known as the centrifugal force, depends on the mass of the object (the heavier the object, the greater the force), the speed of rotation (the greater the speed of the object, the greater the force), and the distance from the center (the closer an object is to the center, the smaller the force). 

4.  We experience centrifugal force when we ride on a merry-go-round, when we go round a curve in a car or when we make a sharp turn on a bike.

Photo by Patricia Marroquin © http://www.betterphoto.com/gallery/
dynoGallByMember.asp?mem=2083

Land and Sea Breezes

Water has a much greater heat capacity than land and, as a result, it warms up slower than the land and also cools down slower.   So during the day, there are significant temperature differences between a water body such as a lake or the sea and the surrounding ground.   This temperature difference causes pressure differences and, as a result, the development of local winds.  Close to the coast, these winds are known as the sea breeze.

5. Source: http://www.ace.mmu.ac.uk/eae/ ©

A sea breeze develops on sunny days when the land becomes much warmer than the sea.  As the land warms up, the air above it expands and begins to rise. To replace the rising air, cooler air is drawn in from above the sea surface.

6. Source:  http://www.ace.mmu.ac.uk/eae/

At night the water cools down slower than the land and the air circulation reverses and air moves from the land to the sea.  This is called a land breeze.

Mountain and Valley Breezes

Special wind systems develop in mountainous regions. As ground surface and air near the surface warm up more intensively than air farer from the surface, the peak and the slopes of sunlit mountains are warmer than the surrounding air. horizontal temperature gradient develops and the light warm air near the surface of the sunlit mountain surface rises quickly which must be replaced with air coming from elsewhere. This leads to the generation of valley breezes during the day and mountain breezes during the night.

7. a) During the day the air close to the mountain sides becomes warmer than the surrounding air.  This warm air rises up the mountains and is replaced by air from within the valley.  So during the day valley air moves up the mountain sides.  This process leads to clouds and rain in the mountains in the summer, particularly in the late afternoon.  Figure: Vera Schlanger.

7. b) At night mountains cool down and cool air is pulled down by gravity.  In the morning, the coldest air is, therefore, often found within the valley. If the air is moist enough, valley fog may form.  Figure by Vera Schlanger.

So slope winds go up the mountains in the day and down during the night and the moving air has to be replaced with air from elsewhere.  A simplified picture of the air circulation is shown in Figure 8.  However, the air circulation in a typical valley is a bit more complicated than this!

The wind during the day usually comes from the lower and flatter parts of the valley system and then rises up the mountains.  As the name of the wind is always given by the place or direction from where it comes from, we call this wind the valley breeze.  During the night, the air cools and descends along the mountain slopes into the valley.  So the breeze moves in the opposite direction, it comes from the mountains and moves into the valley floor and plains.  As a result, this wind is known as the mountain breeze.

9. a) Valley breeze during the day (large dotted arrow).  Photo: Elmar Uherek.

9. b) Mountain breeze during the night (large dotted arrow).  Virgen Valley, Austria.

10. Local circulation during a valley breeze.

This local circulation scheme is a bit simplistic as mountains are not smooth and have many side valleys. 
Radiation intensity, cloudiness and the large-scale wind over the region all influence the winds over mountains. However, this schme gives a basic idea of the typical wind movements in mountainous areas.

 

Authors: Vera Schlanger & Szabolcs Bella - Hungarian Meteorological Service
Scientific reviewing:  Dr. Ildikó Dobi Wantuch / Dr. Elena Kalmár - Hungarian Meteorological Service, Budapest
Last updated 2003-10-17

Further reading:

http://www.infoplease.com
http://www.ux1.eiu.edu
http://phun.physics.virginia.edu
http://cimss.ssec.wisc.edu
http://www.research.umbc.edu
http://www.doc.mmu.ac.uk/aric/

Modifié le: mardi 25 juin 2019, 18:53