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WEATHER INFORMATION - ABOUT FRONTS
Read about weather fronts and more, to help you understand what's going on outside around you.

 

There are three types of weather fronts:

  • Warm Front
    A warm front is warm air moving into an area of cold air this forces the warm air to rise over the cold air. As the warm air lifts into an area of low pressure clouds form as flat sheets.

  • Cold Front
    A cold front is cold air moving into an area of warm air.
    The cold air pushes under the warm air forcing the warm
    air to rise. The warm air then condenses producing rain.

  • Occluded Front
    An occluded front is were two fronts, a warm and a cold meet. If the cold front cuts under the warm front it is known as a cold occlusion.  If the cold front rises over the warm one it is known as a warm occlusion.  Both types of occluded fronts can bring rain.


 

 


Global Air masses
Globally there are very large areas of high and low pressures. The form bands around the Earth that are parrellel with the line of latitude.
At the equator (0 ) there is a low pressure band with two more, one near the Artic (60 North) and one near the antartic (60 South).
Between the low pressure lie high pressure belts one at 30 North and one at 30 South, just north and south of the tropical latitudes.

As air moves from high to low pressures it produces the global prevailing winds, known as trade winds. The trade winds are strongest
between the high and low pressures with wind speeds relatively low at the pressure belts. The trade winds do not blow in a straght line
towards the poles as they are blown of course by the spinnig of the Earth. In the northern hemisphere the winds are blown to the right
and to the left in the southern hemisphere. Therefore making prevailng winds mainly south westerly in the North.



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The Hadley cell carries heat and moisture from the tropics
to the northern and southern mid-latitudes.

 

** PLEASE DESCRIBE THIS IMAGE **
Thanks to wikibooks
for this great weather information
What Are Hadley Cells?

The low pressure area at the equator is the driving force for the whole current system
of the Earth. As warm air rises at this low pressure area it cools and condenses forming clouds and precipitation. The low pressure then takes cold air from the north and south
to replace the rising air. This cold air is then itself heated pushing the now dry warm air further north and south. This dry air starts to sink back to Earth at the tropics creating the High Pressure areas. This falling dry air makes the areas havea much drier climate forming deserts and savannahs. This dry air is then sucked back towards the equator where the process is repeated. The areas where this cycles of winds happen is known
as the Hadley Cells.

Beijing Anomaly
Scientists scanning the deep interior of Earth have found evidence of a vast water
reservoir beneath eastern Asia that is at least the volume of the Arctic Ocean.
The left figure is a slice through the Earth, taken from the figure on the right, showing the attenuation anomalies within the mantle at a depth of roughly 620 miles. In both images, red shows unusually soft and weak rock believed to be saturated with water, and the blue shows unusually stiff rock (yellow and white show near-average values).

 

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