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Published byKarin Tønnessen Modified over 6 years ago
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Warmup Pick up a notes handout! I will give you class time tomorrow to finish your Oceans & Seas Mapping QUIZ ON FRIDAY!!!! It will be all multiple choice! Yay! What to study: Oceans of the World Reading & Question Sheet, Notes: Physical Oceanography Notes I will allow you to make a note card to use on the quiz!
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Earth’s Oceans
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Oceans Oceanography- the study of Earth’s oceans
Water could have originated one of two ways on Earth: Comets hitting Earth Volcanic Eruptions emitting gasses
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Oceans Modern Oceanography Sonar Satellites
Today we can use SONAR and satellites to study the oceans. Satellites such as the Topex/Poseidon monitor the ocean’s surface temperatures, currents, and wave conditions. Satellites Modern Oceanography Sonar
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Oceans cover approximately 71% of the Earth’s surface
Ocean Water Oceans cover approximately 71% of the Earth’s surface
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Ocean Water Oceans cover about: 61% of the northern hemisphere
81% of the southern hemisphere Northern Hemisphere Southern Hemisphere
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Chemical Properties of Seawater
Ocean water is made up of several different elements that make it “salty”
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Chemical Properties of Seawater
Salinity is a measure of the amount of dissolved salts in seawater. Salinity is measured in grams of salt per kilograms of water, or parts per thousand (ppt)
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Chemical Properties of Seawater
The average salinity of seawater is 35 ppt or 3.5%
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Chemical Properties of Seawater
Salinity can be increased by: Weathering and erosion of rock Volcanic activity Evaporation Salinity can be decreased by: Precipitation Runoff Iceberg and sea ice melting
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Ocean Layers The ocean can be divided into 3 layers based on temperature Surface layer Transitional thermocline Bottom layer Surface Layer Thermocline Bottom Layer
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Thermocline - a zone of rapid temperature change
Thermocline - a zone of rapid temperature change. As depth INCREASES temperature DECRESES
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Water Density Water density is affected by temperature and salinity
Cold water is more dense and sinks to the bottom Warm water is less dense and rises Salinity Higher salinity leads to increased density Higher density water sinks.
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Currents Density Currents- caused by
the differences in temperature and salinity in deep water Surface Currents- caused by winds.
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Gulf Stream From North America to Europe, follows the
“Westerlies” as a Surface Current. 300x flow of Amazon Cold+salt = dense water In the North Atlantic Ocean, the water becomes so dense - begins to sink down through less salty and less dense water: Density Current
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Gyres - circular ocean currents caused by landmasses
Coriolis effect – ocean currents in the northern hemisphere are deflected to the right and currents in the southern hemisphere are deflected to the left Upwelling - Vertical movement of ocean water
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Tides Tides - the periodic rise and fall of ocean levels
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Neap Tides Spring Tides
Occur when the Sun, Moon and Earth form a right angle. High tides are lower, low tides higher than normal Spring Tides Occur when Sun, Moon and Earth are aligned High tides are higher and low tides lower than normal
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Ocean Waves Wavelength- distance from one point to the same point on the next wave Crest- top of a wave Trough- bottom of a wave Wave- rhythmic movement that carries energy through matter or space
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Breakers- waves whose bottom is moving slower than the top due to friction
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