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HIGHER GEOGRAPHY PHYSICAL CORE. ATMOSPHERE. Ø. describe and interpret climate maps, diagrams and graphs. Ø. construct and analyse climate graphs. Ø. describe and explain climate graphs. comment on the accuracy of statements which describe climate patterns. Ø. shown on maps etc. GMTs. - PowerPoint PPT Presentation
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HIGHER GEOGRAPHY
PHYSICAL CORE
ATMOSPHEREATMOSPHERE
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GMTs
describe and interpret climate maps, diagrams and graphs
construct and analyse climate graphs
describe and explain climate graphs
comment on the accuracy of statements which describe climate patternsshown on maps etc.
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By the end of this topic you should be able to:
explain with the aid of an annotated diagram, why Tropical latitudes receive more of thesun’s energy than Polar regions
explain why there is a net gain of solar region in the Tropical latitudes and a net loss towards the poles
describe the role of atmospheric circulation in the redistribution of energy over the globe
describe and explain the earth’s energy exchanges shown on a diagram
describe the factors which affect the amount of sunlight reflected from the earth’s surface
describe and account for the generalised pattern of atmospheric circulation and globalwinds, or ocean currents shown on a world map
describe the variations in world temperature for the last 100 years (shown eg. on a graph)and suggest both physical and human reasons for these variations
describe and explain the origin, nature and weather characteristics of Tropical Maritime (mT)and Tropical Continental (cT) air masses which affect West Africa
with reference to the Inter-Tropical Convergence Zone and the movement of air masses,describe and account for the variations in West African rainfall.
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0º Equator 90º Pole
LP HP
At the Equator the atmosphere is heated Air becomes less dense and rises. Rising air creates low pressure at the equator. Air cools as it rises because of the lapse rate. Air spreads. As air mass cools it increases in density and descends. Descending air creates high pressure at the Poles. Surface winds blow from HP to LP.
SINGLE CELL MODEL
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warm air is less dense therefore lighter air rises in the Tropics this creates a zone of LOW PRESSURE air spreads N and S of the Equator air cools and sinks over the Poles this is a zone of HIGH PRESSURE air returns as surface WINDS to the Tropics
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This was later improved and a three cell modelwas developed.
The single cell model of atmospheric circulationwas developed to explain the transfer of energy
from the Tropics to the Poles.
SINGLE CELL MODEL
Today the three cell model is also considered to bean oversimplification of reality.
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ITCZ = Inter-tropical convergence Zone (Low Pressure)
STH = Sub-tropical High (High Pressure)
HADLEY CELL ITCZ
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0º Equator 90º Pole30º 60º
LP HP LP HP
Hadley Cell
Polar Cell
Ferrel Cell
THREE CELL MODEL
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Warm air rises at the Equator - Inter-Tropical Convergence Zone (ITCZ).
Equatorial air flows to ~30º N then sinks to the surface and returns as a surface flow to the tropics.
This is the Hadley cell. Cold air sinks at the North Pole. It flows S at the surface
and is warmed by contact with land/ocean, by ~60º N it rises into the atmosphere.
This the Polar cell.
Between 60º N and 30º N there is another circulation cell. This is the Ferrel cell.
The Hadley cell and the Polar cell are thermally direct cells.The Ferrel cell is a thermally indirect cell.
ENERGY TRANSFER
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ENERGY TRANSFER
Hadley Cell
Polar Cell
Ferrel Cell
Heat energy is transferred from the Hadley Cell to the Ferrel Cell and from the Ferrel Cell to the Polar Cell.
In this way heat is transferred from the Equator where there is an energy surplus
to the Poles where there is an energy deficit.
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0º Equator 90º Pole30º 60º
LP HP LP HP
conv
erge
nce
dive
rgen
ce
conv
erge
nce
dive
rgen
ce
winds blow from high pressure zones to low pressure zones
WINDS
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CONVERGENCE and …………DIVERGENCE
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