Properties of Seawater Oceanography Unit #2
Water (& Hydrogen bonding) Molecules form hydrogen bonds w/ each other.
H20H20H20H20
Water (& Hydrogen bonding) Molecules form hydrogen bonds w/ each other. w/o hydrogen bonds, water freezes at -100° C. w/o hydrogen bonds, water boils at -80° C. High heat capacity. Absorbs great deal of heat when evaporates. Transparent. Red wavelengths absorb first, blue last.
Absorption of Light
Marine Temperatures
Seawater temps vary between about -3° C and 30° C. < 0° C possible because saltwater freezes at colder temps. Ideal organismal temp is between 0°C and 30 °C. Temp ranges: 85°CThermal vents 40°CTropical lagoons 20°CSubtropical surface water 15°CTemperate surface water 5°CSub-polar surface water 0°CPolar surface water -3°CAntarctic bottom water
Salinity Amount of “salt” dissolved in water. Includes inorganic salts, gases, and organics. Expressed in ppt (‰), parts per thousand. Ocean’s salinity ranges from 0‰ to 40‰.
Major Dissoved Ions
Salinity Amount of “salt” dissolved in water. Includes inorganic salts, gases, and organics. Expressed in ppt (‰), parts per thousand. Ocean’s salinity ranges from 0‰ to 40‰. Increase salinity by: Removing water during evaporation Removing water during freezing Decrease salinity by: Add water during precipitation Add water during thawing Add water by river runoff
Seawater’s Density Pure fresh water has a density of 1.0 gm/cm 3 Increasing salinity increases density of water. Decreasing salinity decreases density of water. Temperature effects on water’s density: Water above 4°C, density increases with decreasing temp. Water below 4°C, density decreases with decreasing temp. Densest water is 4°C. Least dense water is 0°C (ICE.) WHY?
Water Freezing
Pressure Sea level pressure = 14.7 lbs/in 2. (atmospheric) Pressure under water increases w/ depth. Every 10 m (33 ft.), adds another atmosphere of pressure.
Pressure