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Water and Weather. Chapter Seven: Oceans. 7.1 Introduction to Oceans 7.2 Waves 7.3 Shallow Marine Environments 7.4 The Ocean Floor. Investigation 7A. Global Winds and Ocean Currents. How do temperature and salinity cause ocean layering?. 7.1 Introduction to Oceans.
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Chapter Seven: Oceans • 7.1 Introduction to Oceans • 7.2 Waves • 7.3 Shallow Marine Environments • 7.4 The Ocean Floor
Investigation 7A Global Winds and Ocean Currents • How do temperature and salinity cause ocean layering?
7.1 Introduction to Oceans • Ocean water is about 3.5 percent salt. • The word salinityis a measure of the dissolved salts in water. • Most of the salt in ocean water is sodium chloride.
7.1 Introduction to Oceans • In some places, special ponds called salt evaporation ponds harvest salt from the ocean.
7.1 Introduction to Oceans • The salt in the oceans comes from: • minerals in the ocean floor • gases released by volcanoes, and • rivers that carry dissolved minerals out to sea.
7.1 Importance of oceans • Oceans are an important source of water for the water cycle. • Oceans spread energy and heat from the hot equator to the colder poles. • Phytoplankton produce most of the oxygen in the atmosphere.
7.1 Earth’s energy • The oceans are able to store heat energy. • The water on Earth prevents the planet from getting too hot or too cold.
7.1 Oceans and Earth’s climate • The climates on the coastline are milder than they are inland because ocean-warmed air masses move over the oceans toward the land.
7.1 Surface currents and gyres • The Sun’s unequal heating of Earth and the Coriolis effect cause permanent global wind patterns. • Surface ocean currents to form large rotating systems called gyres.
7.1 Oceans and Earth’s climate • Deep ocean currentsmove below the surface of the ocean. • They are slower than surface ocean currents.