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Waves are a result of wind.
As wind blows longer and harder, more waves will be produced.
Surface currents move warm water toward the poles and cold water toward the equator. An example of a warm surface current would be the Gulf
Stream.
Tides are the daily rise and fall of sea level due to the gravitational attraction between the Moon, Sun, and Earth.

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New and full moons create
spring tides: highest high tide, lowest low tide
First and third quarter moons create neap tides: lowest high tide, highest low tide
High tides are found on whatever side of the Earth the
Moon is on due to gravity. The exact opposite side of the Earth will also have high tide due to
inertia.
The tidal bulges follow the Moon where ever it goes.
The difference between sea level at high tide and sea level at low tide is called the tidal range.

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High oceanic productivity occurs in areas of upwelling in the ocean, particularly along continental shelves
The coastal upwelling in these regions is the result of deep oceanic currents colliding with sharp coastal shelves, forcing
nutrient-rich cool water to the surface and pushing surface waters offshore.

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The ocean is the largest reservoir of heat at the Earth’s surface.
The stored heat in the ocean drives much of the Earth’s weather.
This stored heat also cases the climate near the ocean to be
milder than the climate of the interior of continents.
Since water absorbs and releases heat energy relatively slowly, water has a moderating effect on climate, and it also helps organisms regulate their body temperature. This high heat
capacity causes a body of water to stay warmer or cooler longer than the surrounding earth and air.

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Why are there land and sea breezes? Because land heats up and cools down much faster than the water, creating
temperature and
pressure differences.
Warm air is less dense and rises over the land during the day, creating an onshore breeze from the sea.
Cool air is more dense and sinks over the land at night, creating an
offshore breeze from the land.

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The submerged extension of the continent below sea level is the continental margin.
Mid-ocean ridges, trenches, volcanic island arcs, and seamounts are the result of tectonic activity.
Chemosynthesis does not require sunlight. This occurs at hydrothermal vents near mid-ocean ridges.
Photosynthesis is how plants and cyanobacteria (bluegreen algae) near the ocean surface produce oxygen.

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El Niño is marked by warmer water in the
Pacific off the coast of South America. It alters weather patterns in the United States and around the world.
During La Niña conditions (normal) , the tradewinds blow toward the west across the tropical Pacific, away from South America.
These winds pile up warm surface water in the west Pacific, so that the sea surface is about
1-2 feet (about 0.5 meter) higher at Indonesia than at Ecuador (in South America).
The sea-surface temperature is about 8 degrees Celsius higher in the west, with cool temperatures off South America, due to an
upwelling of cold water from deeper levels.
This cold water is nutrient-rich, supporting high levels of primary productivity, diverse marine ecosystems, and major fisheries.
During El Niño, the tradewinds relax in the central and western Pacific. Surface water temperatures off South America warm up, because there is less upwelling of the cold water from below to cool the surface. This cuts off the supply of nutrients, resulting in a drastic decline in the food chain, including commercial fisheries in this region.

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Evidence shows that human activities, including
intense fishing around the world, are altering ocean ecosystems beyond their natural state.
A recent study which has mapped the total human impact on the seas for the first time has revealed that the picture is far worse than the scientists imagined.
40% of the world's oceans have been heavily affected by human activities, including fishing,
coastal development, and
pollution from shipping.