3 earth – planet waterbrosenhe/oceanography/3_earth-planet_water.pdf · formation of water on...

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1 Earth Earth – Planet Water Planet Water 71% Nearly ¾ of Earth’s surface is covered by liquid water More covered by solid water Where is it from? Professor Rosenheim EENS/EBIO 223 Introductory Oceanography Formation of Water on Planet Earth Combination of volcanic activity and strong enough gravity field Water vapor, H gas, HCl, CO, CO 2 , and N escaped from the chemically active interior of Earth and were trapped in the atmosphere by gravity – steady state Water vapor condensed on cooling Earth to form water

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Page 1: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Earth Earth –– Planet WaterPlanet Water

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

71%

• Nearly ¾ of Earth’s surface is covered by liquid water

• More covered bysolid water

• Where is it from?

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Formation of Water on Planet Earth

• Combination of volcanic activity and strong enough gravity field

• Water vapor, H gas, HCl, CO, CO2, and N escaped from the chemically active interior of Earth and were trapped in the atmosphere by gravity – steady state

• Water vapor condensed on cooling Earth to form water

Page 2: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Current Ocean Systems

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Non-steady state

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

World Ocean Characteristics

• Area: 361,100,000km2 – 71% of Earth’s surface

• Volume: 1,370,000,000km3 – 97% of Earth’s surface water

• Average Depth: 3,800m• Average Temperature: 3.9oC• Average Salinity: 35%0

Page 3: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Three Conventional Oceans…

• Pacific – bigger than all continents together

• Atlantic – 26% of area covered by oceans

• Indian – slightly smaller than the Atlantic, almost entirely in southern hemisphere

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

…And 2 Other Oceans

• Arctic Ocean – least studied because it is covered by ice

• Southern Ocean – mixing zone for all oceans

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Large Seas• Mediterranean Sea

– Surrounded by Europe and Africa with a small open ocean connection – “middle of land” sea

• Caribbean Sea– Bounded by Antilles Islands (Lesser and Greater) and

the Americas – named after Carib Indians• Other seas

– Bay of Bengal– Persian Gulf– Arabian Sea– Gulf of Mexico

Page 4: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

The Pacific Ocean

• Average Depth– 3940 m

• Volume– 679.6 x 106 km3

• Area– 155.6 x 106 km2

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

The Atlantic Ocean

• Average Depth– 3844 m

• Volume– 313.4 x 106 km3

• Area– 76.8 x 106 km2

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

The Indian Ocean

• Average Depth– 3840 m

• Volume– 269.3 x 106 km3

• Area– 68.5 x 106 km2

Page 5: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

The Arctic Ocean

• Average Depth– 1117 m

• Volume– 17 x 106 km3

• Area– 14.1 x 106 km2

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

The Southern Ocean

• Average Depth– 4500 m

• Volume– 91.5 x 106 km3

• Area– 20.3 x 106 km2

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Mediterranean Sea

• Average Depth– 1500 m

• Volume– 3.75 x 106 km3

• Area– 2.5 x 106 km2

Page 6: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Caribbean Sea

• Average Depth– 2200 m

• Volume– 6.05 x 106 km3

• Area– 2.75 x 106 km2

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

The “Water” HemisphereLeast studied areas of the world

Profound impacts on climate and carbon cycling

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

The “Land” HemisphereMany more records and measurements

Continental climate dominates

Page 7: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Water in Perspective

Oceans98%

Fresh2%

Glaciers69%

Groundw ater30%

Atmosphere1%

Surface fresh0%

Other1%

Rivers2% Sw amps

11%

Lakes87%

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

The Global Water Cycle

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Residence Time

• Ocean Water– 4060 y (1.3x109/3.2x105)

• Atmosphere– 0.04 y (1.5x104/3.96x105)– Atmospheric water is completely exchanged

~26 times per year!

Page 8: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Salt Water• Emitted from primordial volcanoes• Dissolved from continents• Unreactive, stay in solution• Non-steady state accumulation in oceans

(and some lakes)

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Distillation across Isthmus of Panama

Evaporation in N. Atlantic basin is carried over the isthmus of Panama. Salt is left behind.

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Distillation across Isthmus of Panama

N. Atlantic is the saltiest open ocean.

Page 9: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Hypsographic Curve

• Elevation and Depth of Earth’s Surface

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Marine Provinces

• Continental Shelf (0-150m)• Continental Slope (150m-3500m)• Trench (as deep as 11,022 m (Marianas Trench))• Seamount and Mid-ocean ridge (2500m, islands)

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Marine Provinces

Page 10: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Water, Planetary Tilt and Seasonality

• 23.5o tilt causes seasons

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Seasonality in the Hemispheres

• Oceans have different heat capacity than land

• Seasonal effects of Earth’s tilt are different in each hemisphere

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Seasonality in the OceansAustral Summer

Page 11: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Seasonality in the OceansBoreal Summer

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Seasonality through Time

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Eccentricity

• Change in Earth’s elliptical orbit, varies on a 100,000y period

Page 12: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Precession

• Varies on 26,000 y period

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Ice Ages

• Change in “steady state” of Earth’s hydrologic cycle– Flux of seawater to ice becomes greater (Fsw-ice )– Flux of ice to seawater becomes smaller (Fice-sw )

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Obliquity

• Tilt of the axis – varies on 41,000 y period

Page 13: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Scientific Exploration of Planet Water

• Research Vessels R/V JOIDES Resolution – a drilling ship

R/V Flip – a stable measurement platform

R/V Seward Johnson – deploying a submersible

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Measuring the Oceans

• CTD– Conductivity (salinity)– Temperature– Depth

• Rosette sampler– Niskin (Nansen) bottles

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Measuring the Oceans

• Adjustable depth tow nets – sample plankton (microscopic organisms)

Page 14: 3 Earth – Planet Waterbrosenhe/Oceanography/3_Earth-Planet_Water.pdf · Formation of Water on Planet Earth • Combination of volcanic activity and strong enough gravity field •

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Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Measuring the Oceans• Seismic reflection

Professor Rosenheim EENS/EBIO 223

Introductory Oceanography

Measuring in the Oceans

• Scuba

• Submersible

• AUV