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China plunges into ocean research
China plunges into ocean research

... pushed greater volumes of warm water into the region and, ultimately, into the deeper ocean. The process has helped to stall the rise in global temperatures, which have remained relatively constant since 1998, but exactly what is happening in the deep ocean remains unclear. Hu says that data from th ...
Landforms of the Ocean
Landforms of the Ocean

... • The ocean floor contains all of the geographic features that can be found on the continents: Mountains, volcanoes, plains, valleys, and canyons. • These underwater landforms are many times taller, deeper, longer, and wider than those on dry land. ...
Sea Floor Spreading The Mid-ocean Ridge
Sea Floor Spreading The Mid-ocean Ridge

... mountain chain running down the center of the Atlantic ocean. ...
Table 7.6. Common features of the seafloor and coastline
Table 7.6. Common features of the seafloor and coastline

... Island chain. A group of islands formed by the same geological process (also called an archipelago). Isthmus. A narrow strip of land connecting two larger landmasses. Lagoon. A shallow body of quiet water almost completely cut off from the open ocean by coral reefs, barrier islands, or barrier beach ...
Cascading of high salinity bottom waters from the Arabian/Persian
Cascading of high salinity bottom waters from the Arabian/Persian

... Cascading (aka shelf convection) is a specific type of buoyancy driven current in which dense water is formed over the continental shelf and then descends down the slope to a greater depth. The cascades of dense water down continental slopes provide a mechanism for shelf–ocean exchange in many parts ...
Properties of sea-water and their distribution in the oceans
Properties of sea-water and their distribution in the oceans

... • potential temperature: the temperature of a parcel of water after it has been raised adiabatically from some depth to the surface, θ=func(S,T,P). – adiabatic: without heat exchange with environment – water sinks  pressure increases  water compresses  energy increases  water warms (example: T(5 ...
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Oceanography
Oceanography

... features – Deep – Ocean Trench – when two plates come together and one goes into the mantle. – Abyssal Plains – Flat deep features – Seamounts/Guyouts – submerged volcanic peaks. ...
Multiple-Choice Questions - Raleigh Charter High School
Multiple-Choice Questions - Raleigh Charter High School

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weather - Bibb County Schools
weather - Bibb County Schools

... 1. WEATHER – the condition of the atmosphere, including temperature, precipitation, and cloud cover, at a particular time and place. 2. METEOROLOGIST – a scientist who studies the weather. 3. PRECIPITATION – the movement of water, in solid or liquid form, from the atmosphere back to the surface of t ...
Ocean Topography
Ocean Topography

... due to erosion by waves, winds, and atmospheric processes. ...
Ocean The World Ocean Ocean Floor Features
Ocean The World Ocean Ocean Floor Features

... Diversity of Ocean Life 1 recognize how marine organisms can be classified. 2 differentiate between plankton and nekton. 3 describe the area of the ocean in which most benthic organisms live. 4 list the factors used to divide the ocean into marine zones. Ocean Productivity 1 list the factors that in ...
Geography Lesson Tectonics Tuesday * The largest earthquakes
Geography Lesson Tectonics Tuesday * The largest earthquakes

... i. Subduction  Zones   ii. Ocean  trenches  (10k)   iii. Continental  shelves   iv. Benoit  Zones   v. Folding     vi. Andesitic  volcanoes   (Andes  Mountains)   which  are  also   composite  volcanoes.   ...
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... Width ranges from 1m to 3.2 km ...
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Hydrologic Cycle Note

... leaves behind salts and other impurities as it evaporates. As the evaporated moisture rises, it declines in temperature at the average rate of 1°C/100m. Moving air masses carry the vapour over the land. Condensation: Water vapour is changed to a liquid (or solid). A critical temperature called “dewp ...
Test 3 - Course World
Test 3 - Course World

... deep-sea garden of hot springs and towering spires they nicknamed the 'Lost City’. "If this were on land," Duke University geologist Jeff Karson said, "it would be a national park." The scientists spotted the formations on Dec. 4 more than 3,200 feet below the frigid, stormy Atlantic during a month- ...
Focus Question - WordPress.com
Focus Question - WordPress.com

... How can seafloor structures provide evidence that Earth is constantly in motion? ...
ocean currents and weather
ocean currents and weather

... THAT COLONIAL SHIPS COULD USE IT TO THEIR ADVANTAGE IN SAILING THE ATLANTIC. ...
SOL 5.6 Interrelationships in Earth/Space Systems (Oceans)
SOL 5.6 Interrelationships in Earth/Space Systems (Oceans)

... Spring tides occur when the Earth, Sun, and Moon are in line. This is during the full moon or new moon. During this time the tides are strong causing extremely high tides and extremely low tides. ...
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... • Includes the shallow waters above the continental shelf, which extends out about 300 km. • This zone contains the nutrients carried into oceans and rivers. • This zone is shallow so therefore light reaches all the way to the ocean floor. • Organisms such as algae, fish, mussels, crabs, barnacles, ...
Unit Three Worksheet – Meteorology/Oceanography
Unit Three Worksheet – Meteorology/Oceanography

... sunlit surface layer and the colder, dark, dense bottom layer and is characterized by temperatures that decrease rapidly with depth Measure of the amount of salts dissolved in seawater Periodic rise and fall of sea level caused by the gravitational attraction among Earth, the moon, and the sun Upwar ...
Solar - Weather
Solar - Weather

... – The air over the land will also heat quickly. – Warm air rises, starting a convection current. – This brings moist ocean air inland. • Ocean air holds a lot of water vapor. • Warm air can also hold more water vapor. – When air cools, it may no longer be able to hold on to all of the water vapor, f ...
Constructive and Destructive Landforms
Constructive and Destructive Landforms

...  Air and water often cause this.  Oxidation (rust) and acid rain. ...
monsters of the deep
monsters of the deep

... relationships between these organisms have not been well-studied. Cold-seep communities are surrounded by a much larger ocean environment. Very little is known about interactions between cold-seep communities and organisms in other ocean habitats. Ocean habitats are usually categorized into zones: I ...
The Oceans
The Oceans

... depth is immense, reaching 5,850 pounds per square inch. In spite of the pressure, a surprisingly large number of creatures can be found here. Sperm whales can dive down to this level in search of food. Most of the animals that live at these depths are black or red in color due to the lack of light. ...
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Ocean



An ocean (from Ancient Greek Ὠκεανός, transc. Okeanós, the sea of classical antiquity) is a body of saline water that composes much of a planet's hydrosphere. On Earth, an ocean is one of the major conventional divisions of the World Ocean, which covers almost 71% of its surface. These are, in descending order by area, the Pacific, Atlantic, Indian, Southern, and Arctic Oceans. The word sea is often used interchangeably with ""ocean"" in American English but, strictly speaking, a sea is a body of saline water (generally a division of the world ocean) partly or fully enclosed by land.Saline water covers approximately 72% of the planet's surface (~3.6×108 km2) and is customarily divided into several principal oceans and smaller seas, with the ocean covering approximately 71% of Earth's surface. The ocean contains 97% of Earth's water, and oceanographers have stated that only 5% of the World Ocean has been explored. The total volume is approximately 1.35 billion cubic kilometers (320 million cu mi) with an average depth of nearly 3,700 meters (12,100 ft).As it is the principal component of Earth's hydrosphere, the world ocean is integral to all known life, forms part of the carbon cycle, and influences climate and weather patterns. It is the habitat of 230,000 known species, although much of the oceans depths remain unexplored, and over two million marine species are estimated to exist. The origin of Earth's oceans remains unknown; oceans are thought to have formed in the Hadean period and may have been the impetus for the emergence of life.Extraterrestrial oceans may be composed of water or other elements and compounds. The only confirmed large stable bodies of extraterrestrial surface liquids are the lakes of Titan, although there is evidence for the existence of oceans elsewhere in the Solar System. Early in their geologic histories, Mars and Venus are theorized to have had large water oceans. The Mars ocean hypothesis suggests that nearly a third of the surface of Mars was once covered by water, and a runaway greenhouse effect may have boiled away the global ocean of Venus. Compounds such as salts and ammonia dissolved in water lower its freezing point, so that water might exist in large quantities in extraterrestrial environments as brine or convecting ice. Unconfirmed oceans are speculated beneath the surface of many dwarf planets and natural satellites; notably, the ocean of Europa is estimated to have over twice the water volume of Earth. The Solar System's giant planets are also thought to have liquid atmospheric layers of yet to be confirmed compositions. Oceans may also exist on exoplanets and exomoons, including surface oceans of liquid water within a circumstellar habitable zone. Ocean planets are a hypothetical type of planet with a surface completely covered with liquid.
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