tuesday february 26, 2013 (ocean water circulation)
TRANSCRIPT
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TuesdayFebruary 26, 2013
(Ocean Water Circulation)
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The Launch PadTuesday, 2/26/13
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Announcements
Happy ?? !
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AnnouncementsI will be available after
school today until 4:45.
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Assignment Currently Open
Summative or
Formative?Date Issued Date Due Date Into
GradeSpeedFinal Day
Quiz 19 S4 2/15 2/15 ? FRIDAY
WS – Marine Life Zones and Ocean
ProductivityF17 2/20 2/21 ? FRIDAY
WS – Oceanic Feeding
RelationshipsF18 2/21 2/22 ? FRIDAY
Quiz 20 S5 2/22 2/22 ? 3/8
TELPAS Writing Sample F1 2/25 2/27 FRIDAY
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Recent Events in Science??
Read All About It!??
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Ocean Water CirculationOcean currents are masses of
water that flow from one place to another.
Surface currents develop from friction between the ocean and the wind that blows across the
surface.Surface circulation of the
oceans are cause by many interacting “gyres”, which are
large systems of rotating ocean currents, particularly those
involved with large wind movements.
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Ocean Water CirculationEarth’s oceanic surface circulation is made up of five main gyres.
North Pacific Gyre
The gyres are related to atmospheric circulation.
South Pacific Gyre
North Atlantic Gyre
South Atlantic GyreIndian Ocean Gyre
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Idealized surface circulation
pattern for the Atlantic Ocean. The prevailing winds create
circular-moving loops of water (gyres) at the
surface in both parts of the
Atlantic Ocean basin.
Figure 15.2
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Average ocean surface currents from February to March. The oceans circulation is organized into five major current gyres (large, circular-moving loops of water), which exist
in the North Pacific, South Pacific, North Atlantic, South Atlantic, and Indian Oceans.
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Large ships crossing the ocean have lost entire containers overboard. if the containers release floating items, inadvertent float meters are launched that help oceanographers track ocean surface currents. The map shows the path of drifting
shoes and recovery locations from a spill in 1990.
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Four Main Currents Exist Within Each Gyre
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Surface CirculationGyres are caused by the Coriolis Effect,
an apparent deflection of moving objects caused by the rotation of the earth and the inertia of the mass experiencing the
effect.The Coriolis force is quite small, and its
effects generally become noticeable only for motions occurring over large
distances and long periods of time, such as large-scale movement of air in the atmosphere or water in the ocean.
This force causes moving objects on the surface of the Earth to appear to veer to
the right in the northern hemisphere, and to the left in the southern.
Surface currents are extremely important to Earth’s climate, as they transfer
warmer water from low latitudes into higher latitudes, and thereby move heat
from warmer to cooler areas.
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This false-color satellite image
shows sea-surface
temperatures of the Gulf Stream.Warmer waters
are shown in red and orange,
colder waters in green, blue, and
purple.As the Gulf
Stream meanders northward, some
of its branches pinch off to form
large, circular eddies.
The Gulf Stream
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Importance of Surface CurrentsOcean currents have a significant
influence on climate.When currents from low-latitude
regions move to higher latitudes, they transfer heat from warmer to cooler
areas on Earth.This is how the Gulf Stream keeps
Great Britain and northwestern Europe warmer during the winter than should
be expected for their latitudes.On the other hand, as cold currents
originating in cold, high-latitude regions travel toward the equator, they
tend to moderate the warm temperatures of adjacent land areas.
For example, the cool Benguela current off the western coast of southern
Africa moderates the heat along this coast.
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Importance of Surface CurrentsWinds can also cause vertical water
movements.Upwelling is the rising of cold waters
from deeper layers to replace warmer surface water.
Upwelling is most characteristic along the western coasts of continents
where winds blow toward the equator and parallel to the coast.These winds combined with the
Coriolis effect cause surface waters to move away from the shore, being
replaced by cooler water “upwelling” from below.
This process brings greater concentrations of dissolved nutrients
to the ocean surface.
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Deep Ocean CirculationCirculation in the deeper ocean is a response to density differences of water at varying
depths.Recall that two factors create a dense mass of water: cold water and increased salinity.
Deep-ocean circulation is referred to as thermohaline circulation.
Most water involved in deep-ocean
currents begins in high latitudes at the
surface A simplified model of ocean circulation is
similar to a conveyor belt that travels from the Atlantic Ocean, through the Indian and Pacific Oceans,
and back again
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WorksheetOcean Water Circulation