World’s Oceans

World’s Oceans

      Formed ~3.8 billion years ago

      primarily by volcanic out gassing and comets

      Largest to smallest:   Pacific, Atlantic, Indian

      Covers ~ 70% of earth’s surface

 

Circulation of water…

      Two primary current circulation for ocean water

             Surface currents

             Deep water currents

 

Surface Currents

      Driven Primarily by wind

      Moves surface water around

      Warm water and cold water currents

 

      Surface currents of the Atlantic

             Gulfstream flows along the coast of N. America

                   Warm water current

                   Keeps Europe from icing over

                   Turns into Canaries current along Africa

 

      Current Oil spill in Gulf of Mexico (2010).

             Problems with size of spill and potential fouling of Mississippi, Alabama and

                   Florida

             Florida current could take it into the Gulf Stream

 

      Pacific Ocean Currents

             California current is cold water current found in the NW during the Summer

             Davidson current is a warm water current that dominates coast in winter

 

What are Gyres and what is the cause of them?

      Caused by continental land masses and coriolis effect

 

Coriolis Effect

      Apparent turning of large bodies of fluid on earth due to the rotation of the earth.

             Fluids in N. Hemisphere turn to the right

             Fluids in S. Hemisphere turn to the left.

      Air masses and oceans are deflected by the effect

 

Deep Ocean Currents

      Circulation of water vertically due to density differences

      What two properties could change the density of water?

      What are some places on earth we could see these changes occurring?

 

 

Temperature

      How does temperature affect water density?

             Warmest areas?

             Coldest areas?

      Thermocline:  change of temperature with depth

 

Salinity

      Where is the salinity the greatest?

      Where is it the lowest?

      Why?

      Halocline:  change of salinity with depth

 

Pycnocline:  change of density with depth

 

Why is there layering in the arctic

      Which is more dense fresh water or salt water?

 

Thermohaline circulation 

      Deep ocean circulation

      Mixes ocean waters

End of Lecture Thursday 5/6/10

 

Review:

      Deep water currents

             Move vertically due to density differences

             Salinity and temperature

             Cold/salt water sinks in polar regions (high Latitudes) and “pulls” surface water

             Rises back to surface in Pacific as it warms

      Surface Currents

             move primarily due wind

             Create gyres in ocean

             Warm and cold water currents

             Affected by Coriolis effect

 

More details about currents and gyres

      Why do surface currents actually move.

             Wind is only one factor (more on how winds develop later)

             Coriolis effect is another factor

                   Causes Ekman Spiral

 

      Wind moves surface water fastest

      Water below surface receives energy from layer above and only some of the energy is

             transmitted so slower motion

      Less energy/motion each layer effectively turns the water and net motion is 90o from

             wind direction

 

      Gyres form “hills” of water due to spiral

      Creates geostrophic currents

             A current or flow that is balanced between the Coriolis force and gravitational

                   pull

 

      Boundary Currents

             Rotation of the earth pushes gyres to the west of the ocean basins and creates a

                faster flow on the western edge.

                   Eastern boundary currents:  Move slower

                   Western Boundary currents move faster

             In regions of the eastern boundary currents, upwelling often occurs

                   Vertical movement of water due to surface currents

                   Provides nutrient rich areas with high biodiversity

 

Ocean Life Zones

      Upwelling is important as it provides nutrients to many of the upper life zones we

             find in the oceans

      What controls life in the ocean?

             Light:  (photic = light)

                   Euphotic zone: 

                         near suface--> photosynthesis can occur

                   Dysphoric zone

                         Very low level light

                   Aphotic zone: 

                         no light at all--> is there life?

             Temperature

                   Waves and currents mix water

                   Layer of uniform temperature ~200m thick

                         below zone of mixing temperature drops quickly

                   Thermocline--> change from warm to cold

             Salinity

                   proportion of dissolved salts to pure water

                   Why is the ocean salty?

                   Varies for different regions

                   Salinity based on evaporation rate or freshwater input

                         near surface higher salinity--> creates halocline

                               glacier formation/melting, rain, rivers, evaporation

     

These parameters control life zones in the ocean and the organisms that exist.

      Intertidal zones

             Well mixed water

             Light and warm temperatures

      Pelagic regions

             Open ocean where organisms swim or float

             Different organisms and regions based on temp, light and salinity

 

      Benthic zones

             Benthic zone: ocean bottom

             Deep ocean floor

             Very cold, low oxygen, & few nutrients

             Primarily filter feeders

      …and Mid-ocean ridges

 

Quick overview of Plate tectonics

      Earth surface/crust is divided into sections or plates

      Plates move around and interact with each other

      Ocean contains Most of the earth’s plate boundaries

      2 plates move apartà  divergent boundary à mid-ocean ridges

      2 plate slide by each otherà transform boundaries

      2 plates convergeà can push one plate under another in a process known as

             subduction

 

How are life zones affected by variations in ocean?

      California Current vs Davidson Current

             Ca. Current is eastern boundary current that flows away from continental shelf

             Davidson Current flows towards continental shelf

      Which of these two would produce a strong upwelling?

 

      Temperature variations

             Normal temperature ranges for oceans in pacific

             Surface winds (trade winds) push warm water to the western pacific and create

                   upwelling along N. America and S. American coastline

 

             El Nino Year…

                   Trade winds lessens and allow warm water to migrate to the east side of the

                         pacific.

                   Upwelling dies down

                   Storm tract follows warming current.

 

West Coast Dead Zones

      Low oxygen zones

      Creates areas where organisms suffocate

 

What causes Dead Zones

      Possible Ideas

             Extreme upwelling

                   Deep low oxygen ocean water pulled to surface by stronger than normal

                         winds

                   Possible caused due to global climate change

             Bacterial and Algae mats due to high nitrates

                   Lowering oxygen