Wind and Deserts
Pressure
The weight of the air above an object exerts a force upon that
object, and this force is called pressure.
Variations in pressure lead to the development of winds that
play a significant role in shaping our daily weather.
Winds flow from areas of high pressure to areas of low
pressure - clockwise in the northern hemisphere
Clouds
A visible aggregate of tiny water (or ice) droplets suspended
in the air
Relative Humidity - 75% relative humidity means that the air
contains three-quarters the amount of water vapor required for
saturation.
Dew point temperature is defined as the temperature to which
the air would have to cool (at constant pressure and constant
water vapor content) in order to reach saturation.
As air rises it tends to cool and water vapor may condense if
saturation is reached
Convective - hot air rises
Convergence - two air masses meet and air column is forced
upwards
Orographic
Interactions in the Atmosphere
Reflection
Scattering - Oxygen and Nitrogen scatter the shorter
wavelengths - sky is blue
Refraction
Diffraction - light bends around an object
If incoming solar radiation is 100 units:
16 units are absorbed by dust, water and ozone;
3 units are absorbed by clouds;
6 units are scattered back by air;
20 units are reflected by clouds;
4 units are reflected by the surface.
30 reflected back to atmosphere - the albedo - reflectivity : if
the albedo decreased, the temperature goes up
Earth receives 51 units
These units heat up the Earth's surface and infrared radiation
is emitted. The Earth's atmosphere absorbs some of this
radiation.
The greater the amount of absorbers (such as carbon dioxide),
the greater the amount of heat absorbed and the higher the
temperature.
Thus, the Earth's atmosphere is relatively transparent to
visible light but absorbs some of the outgoing infrared.
Ozone (O3) absorbs ultraviolet - high energy
Aeolian Sedimentation
Modification of grain shape by the wind
Accumulations
Dune Fields
Erosional Features
The Rock Record