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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. ...
4. Sea level changes and application of Oxygen isotopes
4. Sea level changes and application of Oxygen isotopes

... oxygen as the air continues to move poleward into colder regions. As the moisture reaches the upper latitudes, the falling rain or snow is made up of more and more water molecules containing light oxygen. •Water vapor gradually loses18O as it travels from the equator to the poles. Because water mole ...
An Introduction to Strategic Environmental Assessment
An Introduction to Strategic Environmental Assessment

... economic, biophysical) into strategic decision-making, to facilitate the move towards sustainability. ...
oceans - TeacherWeb
oceans - TeacherWeb

... continental edge to the ocean floor that connects the continental shelf and the oceanic crust • It usually begins at 430 feet (130 meters) depth and can be up to 20 km wide. ...
oceans
oceans

... • Wegener was a meteorologist…what did he know anyway!!! ...
A New Carbon-Based Algal Biomass Proxy for Photoacclimation
A New Carbon-Based Algal Biomass Proxy for Photoacclimation

... Photoacclimation changes the intracellular chlorophyll-a concentration (Chl), and is not currently taken into account by standard ocean color algorithms. Chl production is a process enhanced under high nutrient and low light conditions (e.g. winter and spring in the Mediterranean Sea). Historically, ...
The Earth`s Oceans - PAMS-Doyle
The Earth`s Oceans - PAMS-Doyle

... more dense • Deep currents usually flow in the opposite direction of surface currents • The densest water in the world is found in Antarctic, this current flows northward toward the equator at the same time warm current flow toward Antarctic ...
Content review with outline and thought questions
Content review with outline and thought questions

... offers a stable substrate (rock) that is regularly emersed and immersed by tidal water. This causes systematic variations in temperature, salinity, and sunlight exposure that depend on the stage of the tide. Furthermore, predation pressure, competition for space, and degree of desiccation change as ...
Marine Sediments
Marine Sediments

... • In warm, tropical oceans, like that shown in (A), large numbers of corals and other marine animals and plants make skeletons out of calcite and other carbonate minerals. These skeletons and carbonate mud make a rock called limestone like the one shown in (B) from San Salvador Island in the Bahama ...
Ocean Topography
Ocean Topography

...  Invented in the 1920s  Primary instrument for measuring depth  Reflects sound from ocean floor ...
Ocean and Climate
Ocean and Climate

... impacting climate. The role of ocean is limited to the surface layers  Atmospheric currents (winds) are largely unbounded. Oceans are laterally bounded by continents (except for southern ocean where fluid can pass around the globe) ...
Ocean noise pollution
Ocean noise pollution

... because it represented a continuous threat, in contrast to sporadic booms. For North Atlantic shipping, the project drew up more than two dozen maps. All their scales went from red (115 decibels at the top) to orange and yellow, and then to green and blue (40 decibels at the bottom). The maps presen ...
Ocean Basins
Ocean Basins

... separate pieces of crust move due to convection of heat in underlying layer (Mantle) plates can move in different directions, and collide Collisions a) two continental plates collide, form high mountain ranges e.g., Himalayas b) two ocean plates collide, form island arc and submarine trench e.g., Al ...
Chapter 13 Exploring the Oceans
Chapter 13 Exploring the Oceans

...  Sodium chloride (NaCl)  Most common dissolved ...
Integrated assessment and ecosystem overviews: North Sea
Integrated assessment and ecosystem overviews: North Sea

... Top down ...
Ocean Circulation - Physics Resources
Ocean Circulation - Physics Resources

... • Discuss why it is important to study ocean currents. Include in your discussion ways that plants, animals, and humans use ocean currents. • Why does a wind driven current not flow in the same direction as the wind that causes it? ...
faf-all
faf-all

... • The magnitude of change in the AMOC, which affects regional climate (GC on regional climate information). • The ocean’s role in determining patterns of SST change (GC on climate sensitivity) and ocean temperature change near to ice-shelves (GCs on regional sea level rise and changes in cryosphere) ...
OCR ASA Level Geography Exploring Oceans Learner Resource 1
OCR ASA Level Geography Exploring Oceans Learner Resource 1

... Guyots were seamounts that extended above sea level, wave erosion flattened the ridge. As the mount moved long the plate away from the ridge, through the process of sea floor spreading, the mount subsided below the level of the sea. ...
2016-2017 Ocean resource exploration climate
2016-2017 Ocean resource exploration climate

... cold water to the ocean surface.  Surface winds blow parallel to the land because of the Coriolis effect.  Cold, deep water continually replaces the surface water that is pushed away from the coast.  This cold water causes cool summers and fog in San Francisco. ...
monsters of the deep
monsters of the deep

... hydrogen sulfide) and oil seep out of sediments. These areas, known as cold seeps, are commonly found along continental margins, and (like hydrothermal vents) are home to many species of organisms that have not been found anywhere else on Earth. Typical features of communities that have been studied ...
Intro to Oceanography - pams
Intro to Oceanography - pams

... Basic Facts… • The five major oceans/depths are Atlantic (3.92km), Indian (3.96km), Pacific (4.0km), Arctic (1.2km) and Southern (5.0km). • A sea is part of an ocean that is nearly surrounded by land. • Seven Seas are all considered part of a global ocean. ...
Plate Tectonics Part 1
Plate Tectonics Part 1

... coming out of hydrothermal vents: – Contain iron, copper, zinc and sulfur – The minerals precipitate out of solution as the water cools (sometimes adding to the vents structure) – Environment provides energy source for chemosynthetic organisms ...
Ocean Landforms
Ocean Landforms

... We will begin our journey where land meets the ocean. Do you know where we are? Yes. At the beach. Beaches are the fastest changing part of the ocean. They change with every wave. Back to Map ...
oceanlandforms
oceanlandforms

... We will begin our journey where land meets the ocean. Do you know where we are? Yes. At the beach. Beaches are the fastest changing part of the ocean. They change with every wave. Back to Map ...
Surface Currents
Surface Currents

... surface and pushes water away from an area. Deeper colder water then rises to replace it. often occurs along coastlines. brings cold, nutrient-rich water from deep in the ocean to the ocean’s surface. ...
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Sea



A sea is a large body of salt water that is surrounded in whole or in part by land. More broadly, the sea (with the definite article) is the interconnected system of Earth's salty, oceanic waters—considered as one global ocean or as several principal oceanic divisions. The sea moderates Earth's climate and has important roles in the water cycle, carbon cycle, and nitrogen cycle. Although the sea has been travelled and explored since prehistory, the modern scientific study of the sea—oceanography—dates broadly to the British Challenger expedition of the 1870s. The sea is conventionally divided into up to five large oceanic sections—including the IHO's four named oceans (the Atlantic, Pacific, Indian, and Arctic) and the Southern Ocean; smaller, second-order sections, such as the Mediterranean, are known as seas.Owing to the present state of continental drift, the Northern Hemisphere is now fairly equally divided between land and sea (a ratio of about 2:3) but the South is overwhelmingly oceanic (1:4.7). Salinity in the open ocean is generally in a narrow band around 3.5% by mass, although this can vary in more landlocked waters, near the mouths of large rivers, or at great depths. About 85% of the solids in the open sea are sodium chloride. Deep-sea currents are produced by differences in salinity and temperature. Surface currents are formed by the friction of waves produced by the wind and by tides, the changes in local sea level produced by the gravity of the Moon and Sun. The direction of all of these is governed by surface and submarine land masses and by the rotation of the Earth (the Coriolis effect).Former changes in the sea levels have left continental shelves, shallow areas in the sea close to land. These nutrient-rich waters teem with life, which provide humans with substantial supplies of food—mainly fish, but also shellfish, mammals, and seaweed—which are both harvested in the wild and farmed. The most diverse areas surround great tropical coral reefs. Whaling in the deep sea was once common but whales' dwindling numbers prompted international conservation efforts and finally a moratorium on most commercial hunting. Oceanography has established that not all life is restricted to the sunlit surface waters: even under enormous depths and pressures, nutrients streaming from hydrothermal vents support their own unique ecosystem. Life may have started there and aquatic microbial mats are generally credited with the oxygenation of Earth's atmosphere; both plants and animals first evolved in the sea.The sea is an essential aspect of human trade, travel, mineral extraction, and power generation. This has also made it essential to warfare and left major cities exposed to earthquakes and volcanoes from nearby faults; powerful tsunami waves; and hurricanes, typhoons, and cyclones produced in the tropics. This importance and duality has affected human culture, from early sea gods to the epic poetry of Homer to the changes induced by the Columbian Exchange, from Viking funerals to Basho's haikus to hyperrealist marine art, and inspiring music ranging from the shanties in The Complaynt of Scotland to Rimsky-Korsakov's ""The Sea and Sinbad's Ship"" to A-mei's ""Listen to the Sea"". It is the scene of leisure activities including swimming, diving, surfing, and sailing. However, population growth, industrialization, and intensive farming have all contributed to present-day marine pollution. Atmospheric carbon dioxide is being absorbed in increasing amounts, lowering its pH in a process known as ocean acidification. The shared nature of the sea has made overfishing an increasing problem.
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