EarthComm Fluids Pages 7-11. Oceans of the World There are 4 large oceans on Earth (Atlantic,...
Transcript of EarthComm Fluids Pages 7-11. Oceans of the World There are 4 large oceans on Earth (Atlantic,...
EarthComm FluidsPages 7-11
Oceans of the WorldThere are 4 large oceans on Earth (Atlantic,
Pacific, Indian, Antarctic)All oceans have land borders (continents), but
all oceans are connected to each otherAbout 70% of the Earth’s surface is covered by
water.
Pacific
Atlantic
Indian
Antarctic
Pacific
Antarctic
Oceans of the World (Continued) The open ocean is very deep: average depth =
4-5 kmNear the bottom of the ocean it is dark, cold,
and has very high pressureDark deep ocean floor
Ocean floor in shallow waters
Ocean zones and Depths
The Warm and the Cold Ocean The ocean is layered by temperature
Upper layer = warmer water – as high as 25oC (~77oF)
Lower layer = colder water – near 0oC (near 32oF)
The Warm and the Cold OceanTemperature
of water decreases sharply between 200m and 1000m below surface
Thermocline – the zone of rapid change from warm water to cold water with increasing depth in the ocean
Similar to temperature difference noticed while treading water (top warmer, near feet colder)
Pycnocline – a layer of water in the ocean characterized by a rapid change of density with depth
Density of ocean water increases as the temperature decreases (toward
floor) Density of ocean water decreases as the
temperature increases (toward surface)
The thermocline and pycnocline happen to be approximately the same thickness in salt water due to the temperature and density characteristics
The Warm and the Cold OceanDensity
changes as depth and temperature of the water changes.
Circulation of Oceans The layer above the thermocline is
continuously circulating (moving) The deeper cold part of the ocean is
continuously circulating
Circulation of Oceans (Continued)
The circulations are different in nature
Oceanographers – scientists who study the Earth’s oceans
They have come up with many theories to account for the circulation of the oceans, and they continue to work on the complicated problem
The Wind Stress Upper layer
circulation is caused mainly by wind stress
Wind Stress – the frictional force exerted on the ocean surface by wind
The blowing wind causes waves on the water’s surface
Wind direction
The Wind Stress (Continued)
As the waves get larger the wind has more effect on them
Waves can cause problems a. Shoreline erosion b. Hazards to
ships
The Coriolis EffectWater in the ocean moves in straight lines
once set in motionEarth rotates underneath the moving water
which actually causes the water to move in a curved path
Coriolis force – the apparent force caused by the Earth’s rotation which serves to deflect a moving body on the surface of the Earth
The overall circulation of the oceans depends on the Coriolis effect