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GGH1501 ASSIGNMENT 2 2018

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ASSIGNMENT 2 GGH

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NAME NYASHA MANYUKE
STUDENT NUMBER 63423693
ASSIGNMENT 02
UNIQUE CODE 718718
MODULE CODE GGH1501
DUE DATE 13 APRIL 2018
COMPULSORY YES

, Predominant Population Standard of living % of labour
Climate type(s) density(persons (GNI per capita force engaged in
2
Per km ppp) agriculture

Brazil Humid and
seasonally humid Below 50 $10,000- $19,999 5-19
tropical climates

DRC Humid and
seasonally humid Below 50 Below $5,000 50 and above
tropical climates

Germany Warm midlatitude $20,000
climate Above 200 and above Below 5

Afghanistan
Dry climates 50 - 99 Below $5000 50 and above




QUESTION 3

Spatial Distribution Pattern of dry climates over the world.

Dry climates are located in bands immediately to the north and south of the low latitude
humid climates. Many dry regions are associated with the subtropical high pressure zone,
for example the Sahara desert in Africa.

The Sahara has one of the world's most severe climates. Typically, the Sahara landscape
experiences extremely limited to virtually no rainfall, powerful and capricious winds and
wide temperature ranges.

Across the desert, the annual average rainfall equals no more than a few inches or less,
much less in many locations. In some areas, no rain at all may fall over several years.
Then, several inches may fall in a torrential downpour. Then, no rain at all may fall for
several more years.

The prevailing wind, which blows from the northeast toward the equator throughout the
year, accounts for the desert's aridness. As the wind moves south westward, the air
warms, dissipating moisture that might otherwise be released as rainfall. Locally, hot winds
often lift sand and dust particles from the desert floor, spinning them upward through
cooler air as dust devils or propelling them south westward as fierce and blinding dust
storms

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