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Specification: Major climate controls 
GGeenneerraall CCiirrccuullaattiioonn
QQuuiicckk RReeccaapp 
 WWee hhaavvee lleeaarrnntt tthhaatt uunneevveenn hheeaattiinngg 
aaccrroossss tthhee eeaarrtthh lleedd ttoo mmoovveemmeenntt ooff aaiirr.. 
 UUnneevveenn hheeaattiinngg iiss ccaauusseedd bbyy aa nnuummbbeerr ooff 
ffaaccttoorrss eegg sseeaassoonnss,, ssuurrffaaccee ccoovveerraaggee eettcc.. 
 MMoovveemmeenntt ooff aaiirr ooccccuurrss bbootthh hhoorriizzoonnttaallllyy 
aanndd vveerrttiiccaallllyy..
AAiirr mmoovveess iinn mmyysstteerriioouuss wwaayyss!! 
GGoollddeenn rruulleess:: 
 AAiirr AALLWWAAYYSS mmoovveess ffrroomm aann aarreeaa 
ooff HHIIGGHH pprreessssuurree ttoo aann aarreeaa ooff 
LLOOWW pprreessssuurree.. ((FFiilllliinngg uupp aa vvooiidd ooff 
lloowweerr aaiirr pprreessssuurree –– tthhiinnkk ooff ddeeffllaattiinngg 
bbaalllloooonnss)) 
 TThhee ggrreeaatteerr tthhee ddiiffffeerreenncceess iinn pprreessssuurree,, 
tthhee ffaasstteerr tthhee wwiinndd wwiillll bbllooww –– pprreessssuurree 
ggrraaddiieenntt.. 
 CCoolldd aaiirr hhoollddss lleessss mmooiissttuurree..
BBaassiicc CCiirrccuullaattiioonn 
Cold polar air 
moves towards 
the warm 
equator. 
Hot tropical air 
moves towards 
the cold poles. 
Remember the differences in the heat supply. 
Remember air moves both horizontally and 
vertically within the confines of the 
atmosphere.
TTrrii CCeellll 
This model shows what we expect to 
happen when air moves. It flows from 
High to Low in each cell, transferring 
heat energy as it moves. 
Bring your diagram 
alive by adding 
these annotations at 
the appropriate 
latitudes.
MMoovveemmeennttss…… 
aatt tthhee eeqquuaattoorr 
Once air starts moving 
from hot and cold 
places, a more 
complicated circulation 
pattern is revealed. 
The effects of pressure 
play an important part 
in pushing or pulling 
air, not to mention the 
spin of the earth. 
At the equator due to intense heating, the air lifts up freely (convection). 
This results in buoyant air spreading out so there is less air at the surface – 
ie LOW PRESSURE. 
This movement vertically encourages cloud growth – rain – hence tropical 
rainforests are found under areas of low pressure.
MMoovveemmeennttss…… 
aatt tthhee ppoolleess 
At the polar regions the 
air is very stable – dry 
and cold. This 
encourages the air to 
sink, creating HIGHER 
pressure at the surface. 
High pressure at the surface is found at regular locations across the globe. 
Under these conditions, different biomes are found – typically deserts. 
The North & South pole are both under high pressure – Cold deserts 
The Sahara and Kalahari deserts are both under high pressure – Hot deserts 
(Desert = Less than 250mm rain per annum)
http://www-tc.pbs.org/wgbh/nova/elnino/anatomy/images/coriolis.gif 
CCoorriioolliiss 
TThhee CCoorriioolliiss ffoorrccee ddeefflleeccttss aaiirr ttoo tthhee rriigghhtt 
iinn tthhee NNoorrtthheerrnn hheemmiisspphheerree ((aanndd ttoo tthhee 
lleefftt iinn tthhee SSoouutthheerrnn hheemmiisspphheerree)) wwhheenn 
vviieewweedd aalloonngg tthhee lliinnee ooff mmoottiioonn.. TThhiiss iiss 
dduuee ttoo tthhee ssppiinn ooff tthhee EEaarrtthh,, iitt iiss tthhiiss 
ffoorrccee tthhaatt pprroovviiddeess tthhee ssuurrffaaccee wwiinnddss 
wwiitthh tthheeiirr ddiirreeccttiioonnss,, ootthheerrwwiissee tthheeyy 
wwoouulldd ffllooww ssiimmppllyy ddiirreecctt NNoorrtthh SSoouutthh..
CCoorriioolliiss aanniimmaattiioonnss 
SScciieennttiissttss ssttrruuggggllee ttoo eexxppllaaiinn CCoorriioolliiss EEffffeecctt 
NNAASSAA nnaarrrraattiioonn
Its all mixed up! 
So far then, we know 
that air moves from 
high to low pressure 
areas (Fig A). 
Polar Cell 
Ferrell Cell 
Hadley 
Cell 
A 
Source areas of high and 
low pressure follow a known 
pattern. 
B 
•Air doesn’t simply move from the equator to the poles and vice versa (Fig A). 
•The spin of the Earth (Coriolis Force) affects direction of winds. 
•There are three large cells that act to transfer heat in the Northern & 
Southern Hemispheres – Polar, Ferrell and Hadley (Fig B.)
TTrrii CCeellll 
This model shows what we expect to 
happen when air moves. It flows from 
High to Low in each cell, transferring 
heat energy as it moves.
Its aallll ttwwiisstteedd!! ~~ PPllaanneettaarryy SSuurrffaaccee WWiinnddss
PPllaanneettaarryy SSuurrffaaccee WWiinnddss 
SSuummmmaarryy 
 TThhee mmoovveemmeenntt ffrroomm hhiigghh ttoo llooww pprreessssuurree 
 PPrreessssuurree GGrraaddiieenntt iiss cchhaannggee iinn aaiirr 
pprreessssuurreess aatt ssuurrffaaccee lleevveell 
 SSuurrffaaccee wwiinnddss ddoo cchhaannggee sseeaassoonnaallllyy 
 TThhee llaanndd aanndd sseeaa aallssoo iinnfflluueennccee tthhee wwiinndd 
ddiirreeccttiioonn oonn aa ssmmaallll ssccaallee 
 22 mmiinnuuttee BBBBCC CCllaassss CClliipp –– HHaarrvveessttiinngg tthhee 
WWiinndd
AAttmmoosspphheerriicc PPrreessssuurree 
 TThhee pprreessssuurree eexxeerrtteedd bbyy tthhee wweeiigghhtt ooff aaiirr iinn tthhee 
aattmmoosspphheerree aatt tthhee ssuurrffaaccee ooff tthhee EEaarrtthh 
 MMeeaassuurreedd iinn MMiilllliibbaarrss ((mmbb)),, iissoobbaarrss jjooiinn ppooiinnttss ooff 
eeqquuaall pprreessssuurree 
 TThhee ggrreeaatteesstt pprreessssuurree iiss ffeelltt oonn tthhee ggrroouunndd 
((aavveerraaggee ooff 11001133mmbb aatt sseeaa lleevveell)) aanndd tthhiiss 
ddeeccrreeaasseess aass aallttiittuuddee iinnccrreeaasseess 
 AAtt tthhee ttoopp ooff mmoouunnttaaiinnss tthheerree iiss lleessss aattmmoosspphheerriicc 
pprreessssuurree
Collaborative SSuummmmaarryy 
UUssiinngg tthheessee wwoorrddss // tteerrmmss,, ccoommpplleettee aa ssuummmmaarryy ooff 
yyoouurr uunnddeerrssttaannddiinngg ffrroomm ttooddaayy’’ss lleessssoonn.. 
SShhaarree wwiitthh yyoouurr nneeiigghhbboouurr aanndd aadddd ssoommeetthhiinngg 
eexxttrraa ttoo yyoouurr ppaarrttnneerr’’ss wwoorrkk ttoo ddeevveelloopp iitt.. 
 CCoorriioolliiss 
 SSuurrffaaccee wwiinnddss 
 HHiigghh pprreessssuurree 
 LLooww pprreessssuurree 
 CCoonnvveerrggiinngg 
 DDiivveerrggiinngg

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GLOBAL CIRCULATION

  • 1. Specification: Major climate controls GGeenneerraall CCiirrccuullaattiioonn
  • 2. QQuuiicckk RReeccaapp  WWee hhaavvee lleeaarrnntt tthhaatt uunneevveenn hheeaattiinngg aaccrroossss tthhee eeaarrtthh lleedd ttoo mmoovveemmeenntt ooff aaiirr..  UUnneevveenn hheeaattiinngg iiss ccaauusseedd bbyy aa nnuummbbeerr ooff ffaaccttoorrss eegg sseeaassoonnss,, ssuurrffaaccee ccoovveerraaggee eettcc..  MMoovveemmeenntt ooff aaiirr ooccccuurrss bbootthh hhoorriizzoonnttaallllyy aanndd vveerrttiiccaallllyy..
  • 3. AAiirr mmoovveess iinn mmyysstteerriioouuss wwaayyss!! GGoollddeenn rruulleess::  AAiirr AALLWWAAYYSS mmoovveess ffrroomm aann aarreeaa ooff HHIIGGHH pprreessssuurree ttoo aann aarreeaa ooff LLOOWW pprreessssuurree.. ((FFiilllliinngg uupp aa vvooiidd ooff lloowweerr aaiirr pprreessssuurree –– tthhiinnkk ooff ddeeffllaattiinngg bbaalllloooonnss))  TThhee ggrreeaatteerr tthhee ddiiffffeerreenncceess iinn pprreessssuurree,, tthhee ffaasstteerr tthhee wwiinndd wwiillll bbllooww –– pprreessssuurree ggrraaddiieenntt..  CCoolldd aaiirr hhoollddss lleessss mmooiissttuurree..
  • 4.
  • 5. BBaassiicc CCiirrccuullaattiioonn Cold polar air moves towards the warm equator. Hot tropical air moves towards the cold poles. Remember the differences in the heat supply. Remember air moves both horizontally and vertically within the confines of the atmosphere.
  • 6. TTrrii CCeellll This model shows what we expect to happen when air moves. It flows from High to Low in each cell, transferring heat energy as it moves. Bring your diagram alive by adding these annotations at the appropriate latitudes.
  • 7. MMoovveemmeennttss…… aatt tthhee eeqquuaattoorr Once air starts moving from hot and cold places, a more complicated circulation pattern is revealed. The effects of pressure play an important part in pushing or pulling air, not to mention the spin of the earth. At the equator due to intense heating, the air lifts up freely (convection). This results in buoyant air spreading out so there is less air at the surface – ie LOW PRESSURE. This movement vertically encourages cloud growth – rain – hence tropical rainforests are found under areas of low pressure.
  • 8. MMoovveemmeennttss…… aatt tthhee ppoolleess At the polar regions the air is very stable – dry and cold. This encourages the air to sink, creating HIGHER pressure at the surface. High pressure at the surface is found at regular locations across the globe. Under these conditions, different biomes are found – typically deserts. The North & South pole are both under high pressure – Cold deserts The Sahara and Kalahari deserts are both under high pressure – Hot deserts (Desert = Less than 250mm rain per annum)
  • 9.
  • 10. http://www-tc.pbs.org/wgbh/nova/elnino/anatomy/images/coriolis.gif CCoorriioolliiss TThhee CCoorriioolliiss ffoorrccee ddeefflleeccttss aaiirr ttoo tthhee rriigghhtt iinn tthhee NNoorrtthheerrnn hheemmiisspphheerree ((aanndd ttoo tthhee lleefftt iinn tthhee SSoouutthheerrnn hheemmiisspphheerree)) wwhheenn vviieewweedd aalloonngg tthhee lliinnee ooff mmoottiioonn.. TThhiiss iiss dduuee ttoo tthhee ssppiinn ooff tthhee EEaarrtthh,, iitt iiss tthhiiss ffoorrccee tthhaatt pprroovviiddeess tthhee ssuurrffaaccee wwiinnddss wwiitthh tthheeiirr ddiirreeccttiioonnss,, ootthheerrwwiissee tthheeyy wwoouulldd ffllooww ssiimmppllyy ddiirreecctt NNoorrtthh SSoouutthh..
  • 11. CCoorriioolliiss aanniimmaattiioonnss SScciieennttiissttss ssttrruuggggllee ttoo eexxppllaaiinn CCoorriioolliiss EEffffeecctt NNAASSAA nnaarrrraattiioonn
  • 12. Its all mixed up! So far then, we know that air moves from high to low pressure areas (Fig A). Polar Cell Ferrell Cell Hadley Cell A Source areas of high and low pressure follow a known pattern. B •Air doesn’t simply move from the equator to the poles and vice versa (Fig A). •The spin of the Earth (Coriolis Force) affects direction of winds. •There are three large cells that act to transfer heat in the Northern & Southern Hemispheres – Polar, Ferrell and Hadley (Fig B.)
  • 13. TTrrii CCeellll This model shows what we expect to happen when air moves. It flows from High to Low in each cell, transferring heat energy as it moves.
  • 14. Its aallll ttwwiisstteedd!! ~~ PPllaanneettaarryy SSuurrffaaccee WWiinnddss
  • 15. PPllaanneettaarryy SSuurrffaaccee WWiinnddss SSuummmmaarryy  TThhee mmoovveemmeenntt ffrroomm hhiigghh ttoo llooww pprreessssuurree  PPrreessssuurree GGrraaddiieenntt iiss cchhaannggee iinn aaiirr pprreessssuurreess aatt ssuurrffaaccee lleevveell  SSuurrffaaccee wwiinnddss ddoo cchhaannggee sseeaassoonnaallllyy  TThhee llaanndd aanndd sseeaa aallssoo iinnfflluueennccee tthhee wwiinndd ddiirreeccttiioonn oonn aa ssmmaallll ssccaallee  22 mmiinnuuttee BBBBCC CCllaassss CClliipp –– HHaarrvveessttiinngg tthhee WWiinndd
  • 16. AAttmmoosspphheerriicc PPrreessssuurree  TThhee pprreessssuurree eexxeerrtteedd bbyy tthhee wweeiigghhtt ooff aaiirr iinn tthhee aattmmoosspphheerree aatt tthhee ssuurrffaaccee ooff tthhee EEaarrtthh  MMeeaassuurreedd iinn MMiilllliibbaarrss ((mmbb)),, iissoobbaarrss jjooiinn ppooiinnttss ooff eeqquuaall pprreessssuurree  TThhee ggrreeaatteesstt pprreessssuurree iiss ffeelltt oonn tthhee ggrroouunndd ((aavveerraaggee ooff 11001133mmbb aatt sseeaa lleevveell)) aanndd tthhiiss ddeeccrreeaasseess aass aallttiittuuddee iinnccrreeaasseess  AAtt tthhee ttoopp ooff mmoouunnttaaiinnss tthheerree iiss lleessss aattmmoosspphheerriicc pprreessssuurree
  • 17. Collaborative SSuummmmaarryy UUssiinngg tthheessee wwoorrddss // tteerrmmss,, ccoommpplleettee aa ssuummmmaarryy ooff yyoouurr uunnddeerrssttaannddiinngg ffrroomm ttooddaayy’’ss lleessssoonn.. SShhaarree wwiitthh yyoouurr nneeiigghhbboouurr aanndd aadddd ssoommeetthhiinngg eexxttrraa ttoo yyoouurr ppaarrttnneerr’’ss wwoorrkk ttoo ddeevveelloopp iitt..  CCoorriioolliiss  SSuurrffaaccee wwiinnddss  HHiigghh pprreessssuurree  LLooww pprreessssuurree  CCoonnvveerrggiinngg  DDiivveerrggiinngg