Date post: | 18-Dec-2015 |
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Ocean Structure and Circulation
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Ocean ModelTemperature
De
pth
Surface
Deeper
WarmerColder
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Ocean Model
3
“Warm” shallow surface layer
Cold deep layer
Transition Zone
Ocean Model
4How do the layers form?
SurfaceLayer
DeepWater
TransitionZone
5
Homogeneous Ocean
Taking the Temperature
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ConductivityTemperature Depth
CTD
www.soest.hawaii.edu
Ocean Temperature
Deep Water
• 90% of the total volume of ocean is this cold, deep water. •At depths greater than 1000m, temperature is approximately 4ºC (even in the tropics!!).
windows.ucar.edu
Why do layers form?
Thermocline = Temperature Change
Surface Layer
Transition Zone
7
Mass per unit volume
Lighter1000 kg/m3
Denser1020-1028 kg/m3
hawaiianphotos.net
Because of Density
Lighter100 kg/m3
Denser19,300 kg/m3
Slashfood.com
8
Ocean Density
Surface Layer
Deep Water
• Seawater density is controlled by Temperature and Salinity
•In the ocean, Temperature has a greater effect on density
windows.ucar.edu
Pycnocline = Density ChangePycnocline Transition Zone
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SurfaceLayer
DeepWater
BoundaryTransitionZone
Thermocline & Pycnocline
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SurfaceLayer
DeepWater
Boundary
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Mixed
Warmed and lit by sun
Photosynthesis
Cold, Dark, No Photosynthesis
Less Nutrients
, More Nutrients
Surface Ocean
• Warm• Lit by the sun• Has photosynthesis• Less nutrients
Deep Ocean
• Cold• Dark• No photosynthesis• More Nutrients
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Summary