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Climographs - Coggle Diagram
Climographs
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The hot air rises since it is less dense, and carries the moisture along with it.
As the rising air cools down, it becomes saturated with water vapour.
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size, and gives convectional rainfall daily between 2 and 4 pm once the water droplets
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The cold, denser air at higher altitudes sinks from the sides of the cloud and replaces
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The air that has sunk to the ground heats up again, and the process continues.
Taiga vegetation
Cold areas with sufficient precipitation have coniferous trees. These trees have cone shape and needle like leaves so that snow does not accumulate on them.
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A place like this will have almost permanent ice cover, with small flowering plants and lichens in summer months.
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A place like this will have just one season – hot and wet – throughout the year. This will be good for growth of dense evergreen trees.
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A place like this will have a wet season, and a long, dry season. This will be conducive for growth of grasses.
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A place like this will have a pronounced rainy season – called monsoon. This will be good for growth of deciduous trees that shed their leaves in the dry season.
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A place like this will have cold, wet winters, and hot, dry summers. This will have a characteristic vegetation typical of the region near the Mediterranean Sea.
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A place like this will be extremely dry throughout the year. This will be conducive to the growth of xerophytic plants such adapted to the arid conditions.
A climograph shows the average monthly temperature recorded in a place over a period of one year (as a line graph) along with the average monthly precipitation (as a bar graph).
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