coriolis force drives movement of water beneath surface
creates ekman spiral if plotted downwards
net transport 90 degrees to right (N hemisphere) or left (S hemisphere) of wind direction
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2
Q
geostrophic current
A
current resulting from the balance of the coriolis and pressure-gradient force
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3
Q
gyres
A
surface only currents in open ocean basins
clockwise in northern hemisphere, anticlockwise in s hemisphere
low pressure bulge of water in the middle of gyres due to geostrophic flow
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4
Q
deep ocean currents
A
NADW and AABW
long term large transfers of energy
large influence on climate
driven by a combination of temperature and salinity = thermohaline circulation
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5
Q
north atlantic deep water (NADW)
A
warm saline water from gulf of mexico pushed northwards by gulf stream
cools so becomes more dense than less saline nordic sea so sinks
maintains flow of north atlantic drift
flows southwards, meeting colder and denser AABW in southern sea
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6
Q
antarctic bottom water (AABW)
A
very cold winds blow offshore from antarctic continent forming polynas (sea ice blown offshore)
sea water supercooled and sea ice forms, rejecting salt into surrounding water
forms extremely cold saline dense water which sinks to the bottom of the Southern ocean
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7
Q
disruption to the nadw
A
melting of the greenland ice sheet introduces large amounts of freshwater, diluting the dense salty water that makes up the NADW, could potentially disrupt NADW and deep ocean circulation
would not disrupt gulf stream as determined by coriolis effect
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8
Q
gulf stream
A
transfer of energy north eastwards from gulf of mexico into the north atlantic drift
causes differential weather conditions between canada and uk at same latitudes