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Seawater Chemistry & Ocean Stratification
1
Key Points
• The salt in seawater is due in part to water’s unique properties.
• Seawater density is influenced by temperature and salinity.
• The ocean has layers as a result of different densities.
How did the Ocean get so salty?• Through a combination of water’s properties
(universal solvent, adhesion) water “picks up” minerals via erosional and weathering processes
• In other words, water physically and
chemically picks up salts
• Make way to the ocean
Hydrological Cycle (Water Cycle)
4
What types of elements are found in the ocean’s salts?
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How do we measure the amount of salt in the Ocean?
• Salinity vs. Conductivity
• CTD Rosette– Conductivity– Temperature– Density
7
Key Points
• The salt in seawater is due in part to water’s unique properties.
• Seawater density is influenced by temperature and salinity.
• The ocean has layers as a result of different densities.
How is the Ocean Like a Red Velvet
Cake?
Ocean ModelTemperature
De
pth
Surface
Deeper
WarmerColder
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Ocean Model
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“Warm” shallow surface layer
Cold deep layer
Transition Zone
Ocean Model
12How do the layers form?
SurfaceLayer
DeepWater
TransitionZone
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Homogeneous Ocean
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
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Mass per unit volume
Lighter1.000 g/cm 3
Denser1.022 to 1.030 g/cm3
hawaiianphotos.net
Because of Density
Lighter100 kg/m3
Denser19,300 kg/m3
Slashfood.com
http://www.youtube.com/watch?v=w_8mw-1HYFg
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• LOTS AND LOTS OF
PRESSURE
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Main Differences…