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Oceanography
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Oceanography 71% Earth’s surface is water
61% Northern Hemisphere is water 81% Southern Hemisphere is water Average temperature 39o F Average depth 12,451 feet Average land elevation 2772 feet
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Formation of Oceans Earth the Biography: Oceans Volcanic outgassing
Water vapor given off Cooled and condensed Comets colliding with Earth
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Significance of Oceans
Maintaining Earth’s temperature -70o C to 55o C Mercury -180o to 430o C Absorbs heat from sun Currents move hot to cold Air temperature Coastlines more moderate Inland more extremes Water loses / gains heat slower than Land
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Significance of Oceans
Biodiversity Majority of all Earth’s Biomass Source food and oxygen Vast complicated food web Water Cycle Starting point Earth’s water cycle
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Salinity Salts 3.5 % mass of oceans Varies with location Affected by
Mouth river – lower Dead sea – 30% Location in water column Affected by Precipitation Sea ice / Icebergs melting Runoff from land Evaporation Formation of sea ice
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Ocean Temperature Varies with amount solar radiation received
Function of latitude Varies with depth Thermocline Layer of ocean 300 m to 1000 m Rapid change of temperature with depth Creates barrier to marine life
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Density Density = mass per unit volume Seawater density affected by
Salinity Temperature Varies with depth Pycnocline Layer ocean water 300 – 1000 meters Rapid change of density with depth
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Composition Na Mg other Cl Ca S
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Water Columns Photic zone Epipelagic zone Sunlight zone
Depth sunlight penetrates Down to 200 meters Photosynthesis Highest amount of nutrients and energy
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Water Columns Disphotic zone Mesopelagic zone Twilight zone
Scarce light 200 – 1000 meters down High pressures
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Water Columns Aphotic zone Midnight zone Bathypelagic zone
90% of the ocean No light – no photosynthesis Few life forms Extremely high pressures
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Water Zones littoral High tide to low tide Constant motion
Intertidal zone littoral High tide to low tide Constant motion Exposure to large amounts of air
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Water Zones sublittoral From intertidal zone to end continental shelf
Neritic sublittoral From intertidal zone to end continental shelf Oceanic plants High primary production Majority of sea life
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Water Zones Begins at end of continental shelf
Oceanic zone Begins at end of continental shelf Steeper dive to ocean floor Mostly no sunlight Sharks, whales, etc.
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