henrichs-sinking particles
... phytoplankton and zooplankton reflect changes in the pelagic food web. Sinking plankton (a component of “sinking particles”) collected by sediment traps mainly reflects the extent of grazing on primary production by zooplankton, and productivity variations over time. The material collected by the se ...
... phytoplankton and zooplankton reflect changes in the pelagic food web. Sinking plankton (a component of “sinking particles”) collected by sediment traps mainly reflects the extent of grazing on primary production by zooplankton, and productivity variations over time. The material collected by the se ...
Key terms
... -know how areas of high and low atmospheric pressure are produced and the names for each of these regions (ITCZ or doldrums, horse latitudes) -know that winds blows from areas of high pressure to low pressure and that winds are named for the direction that they come from Sample Essay Questions: 1. D ...
... -know how areas of high and low atmospheric pressure are produced and the names for each of these regions (ITCZ or doldrums, horse latitudes) -know that winds blows from areas of high pressure to low pressure and that winds are named for the direction that they come from Sample Essay Questions: 1. D ...
Deep Sea Hydrothermal Vent Communities
... Why are the vents important? • Oasis of life, about 300 species have been identified. A new organisms is discovered every 10 days. • Doesn’t depend on photosynthesis- perhaps life didn’t begin by photosynthesis, but through chemosynthesis. • May provide information on the formation of life. • Think ...
... Why are the vents important? • Oasis of life, about 300 species have been identified. A new organisms is discovered every 10 days. • Doesn’t depend on photosynthesis- perhaps life didn’t begin by photosynthesis, but through chemosynthesis. • May provide information on the formation of life. • Think ...
sustained ocean observations from merchant marine vessels
... management techniques designed and optimized for these platforms we could open up an entirely new dimension to ocean observation. The following material was presented to the US NSF last year. They suggested we contact SCOR who in turn liked the idea very much, but felt it would be wise to get JCOMM’ ...
... management techniques designed and optimized for these platforms we could open up an entirely new dimension to ocean observation. The following material was presented to the US NSF last year. They suggested we contact SCOR who in turn liked the idea very much, but felt it would be wise to get JCOMM’ ...
Effects of Climate Change on Marine Ecosystems Chen-Tung Arthur Chen
... pH vertical profiles of seawater in the South China Sea. To date, anthropogenic CO2 emissions have already decreased surface water pH by roughly 0.1 units of pH. By 2050, pH is predicted to decrease further by approximately an additional 0.1 unit. Of course, ocean acidification in addition to seawat ...
... pH vertical profiles of seawater in the South China Sea. To date, anthropogenic CO2 emissions have already decreased surface water pH by roughly 0.1 units of pH. By 2050, pH is predicted to decrease further by approximately an additional 0.1 unit. Of course, ocean acidification in addition to seawat ...
Summary of lesson - TI Education
... Move to page 1.2 and read the information given. Earth's crust is divided into 7 major plates that are in continuous motion. Ridges and trenches define the edges of the plates. The Mid-Atlantic Ridge is the underwater mountain range running from Iceland to Antarctica. At the Mid-Atlantic Ridge, plat ...
... Move to page 1.2 and read the information given. Earth's crust is divided into 7 major plates that are in continuous motion. Ridges and trenches define the edges of the plates. The Mid-Atlantic Ridge is the underwater mountain range running from Iceland to Antarctica. At the Mid-Atlantic Ridge, plat ...
Plate Tectonics - Net Start Class
... km thick and behaves plastically (solid that flows) because of extreme temperature. 1. This layer acts as a lubricating fluid allowing the plates to move. 2. Convection currents – the mantle close to the hot outer core heats, becomes less dense and rises. As it rises, it spreads and cools. In coolin ...
... km thick and behaves plastically (solid that flows) because of extreme temperature. 1. This layer acts as a lubricating fluid allowing the plates to move. 2. Convection currents – the mantle close to the hot outer core heats, becomes less dense and rises. As it rises, it spreads and cools. In coolin ...
Summary of lesson - TI Education
... Move to page 1.2 and read the information given. Earth's crust is divided into 7 major plates that are in continuous motion. Ridges and trenches define the edges of the plates. The Mid-Atlantic Ridge is the underwater mountain range running from Iceland to Antarctica. At the Mid-Atlantic Ridge, plat ...
... Move to page 1.2 and read the information given. Earth's crust is divided into 7 major plates that are in continuous motion. Ridges and trenches define the edges of the plates. The Mid-Atlantic Ridge is the underwater mountain range running from Iceland to Antarctica. At the Mid-Atlantic Ridge, plat ...
Lecture 7. Marine Sediments
... brilliantly blue, white in places with clouds and ice, sometimes swirling with storms. ...
... brilliantly blue, white in places with clouds and ice, sometimes swirling with storms. ...
Features of the Ocean Floor
... Both are generally associated with hot spots. Seamounts rise above the surface and form islands such as Hawaii and the Canary Islands. ...
... Both are generally associated with hot spots. Seamounts rise above the surface and form islands such as Hawaii and the Canary Islands. ...
GEOS 110 Fall 2011 Test 2 Study Guide Test cover`s Chapters: 5
... 55. In what way is the earth dynamic rather than static for its internal heat, magnetic field, solid mantle, continent configuration and ocean basin shape? 56. Where does melting take place in the Earth? 57. What is the state of the Mantle? 58. Where is new lithosphere made? 59. Where is ocean litho ...
... 55. In what way is the earth dynamic rather than static for its internal heat, magnetic field, solid mantle, continent configuration and ocean basin shape? 56. Where does melting take place in the Earth? 57. What is the state of the Mantle? 58. Where is new lithosphere made? 59. Where is ocean litho ...
GEOS 110 Fall 2013 Test 2 Study Guide
... 55. In what way is the earth dynamic rather than static for its internal heat, magnetic field, solid mantle, continent configuration and ocean basin shape? 56. Where does melting take place in the Earth? 57. What is the state of the Mantle? 58. Where is new lithosphere made? 59. Where is ocean litho ...
... 55. In what way is the earth dynamic rather than static for its internal heat, magnetic field, solid mantle, continent configuration and ocean basin shape? 56. Where does melting take place in the Earth? 57. What is the state of the Mantle? 58. Where is new lithosphere made? 59. Where is ocean litho ...
Parent Signature_____________________ Ocean Unit
... include a) geological characteristics (continental shelf, slope, rise); b) physical characteristics (depth, salinity, major currents); and c) biological characteristics (ecosystems). Key Ideas and Terms: There are 4 major oceans on Earth. They are: The Atlantic Ocean, the Pacific Ocean, The Arctic O ...
... include a) geological characteristics (continental shelf, slope, rise); b) physical characteristics (depth, salinity, major currents); and c) biological characteristics (ecosystems). Key Ideas and Terms: There are 4 major oceans on Earth. They are: The Atlantic Ocean, the Pacific Ocean, The Arctic O ...
Chapter 19
... global ocean the body of salt water that covers nearly three-fourths of Earth’s surface • The global ocean contains more than 97% of all of the water on Earth. • The global ocean is divided into five major oceans. These major oceans are the Atlantic, Pacific, Indian, Arctic, and Southern Oceans. sea ...
... global ocean the body of salt water that covers nearly three-fourths of Earth’s surface • The global ocean contains more than 97% of all of the water on Earth. • The global ocean is divided into five major oceans. These major oceans are the Atlantic, Pacific, Indian, Arctic, and Southern Oceans. sea ...
Chapter 3
... This leads to the flooding of the neighbouring areas. As it floods, it deposits layers of fine soil and other material called sediments along its banks. This leads to the formation of a flat fertile floodplain. The raised banks are called levees. As the river approaches the sea, the speed of the flo ...
... This leads to the flooding of the neighbouring areas. As it floods, it deposits layers of fine soil and other material called sediments along its banks. This leads to the formation of a flat fertile floodplain. The raised banks are called levees. As the river approaches the sea, the speed of the flo ...
Ocean Bottom - PAMS-Doyle
... less than the average of 35 o/oo Lower salinity where freshwater rivers enter the ocean Salinity is higher where there is greater evaporation and in polar regions where only fresh water freezes Animals using certain salts to build their shells can lower salinity ...
... less than the average of 35 o/oo Lower salinity where freshwater rivers enter the ocean Salinity is higher where there is greater evaporation and in polar regions where only fresh water freezes Animals using certain salts to build their shells can lower salinity ...
The coelacanth and biotechnology
... ◆ The oceans pose threats through floods, storms, sea level change and coastal erosion. More than half the world’s population lives near the sea. Oceans are used for waste disposal. Most waste eventually ends up in the oceans, with the result that marine pollution is a global problem – every part of ...
... ◆ The oceans pose threats through floods, storms, sea level change and coastal erosion. More than half the world’s population lives near the sea. Oceans are used for waste disposal. Most waste eventually ends up in the oceans, with the result that marine pollution is a global problem – every part of ...
Spatial Distribution
... = particulate organic matter that originates in the ocean Formed by collisions of debris and large particles, or decaying material, with bacteria and protists attached. Sinks to bottom, carrying nutrients away from surface. ...
... = particulate organic matter that originates in the ocean Formed by collisions of debris and large particles, or decaying material, with bacteria and protists attached. Sinks to bottom, carrying nutrients away from surface. ...
Ocean Landforms - Net Start Class
... •They are more than 84,000 kilometers (52,000 miles) in length and they extend through the North and South of the ...
... •They are more than 84,000 kilometers (52,000 miles) in length and they extend through the North and South of the ...
STUDY GUIDE CHAPTER 3 TEST 2009
... To prevent oil spills How can picking up trash on a beach help? (fig.8, pg 108) Makes the beach safer for plants and animals List the oceans in order of size. Begin with the largest. Pacific atlantic Indian arctic The physical change of liquid water to water vapor is called evaporation If sunlight ...
... To prevent oil spills How can picking up trash on a beach help? (fig.8, pg 108) Makes the beach safer for plants and animals List the oceans in order of size. Begin with the largest. Pacific atlantic Indian arctic The physical change of liquid water to water vapor is called evaporation If sunlight ...
Living Shipwrecks: Science Under the Sea
... Blue colour is reflected in all directions, making the sea look blue. The brighter the sunlight, the bluer the sea looks. Particles, suspended in the water, can also reflect light, altering the blueness – that is why the sea looks turquoise when the cliffs and the beach are made of chalk or clay. ...
... Blue colour is reflected in all directions, making the sea look blue. The brighter the sunlight, the bluer the sea looks. Particles, suspended in the water, can also reflect light, altering the blueness – that is why the sea looks turquoise when the cliffs and the beach are made of chalk or clay. ...
Marine Ecology, Ecosystems, Marine Factors, Seawater Chemistry
... invertebrate larva that will eventually end up near the coast. ...
... invertebrate larva that will eventually end up near the coast. ...
Are the oceans Rising NY Times 2010Hazard Variability
... heads the Sea Level Research Laboratory at the University of Pennsylvania. “I think the more important question is whether it’s due to anthropogenic (human-made) activity.” As Horton points out, rising sea levels aren’t a new natural phenomenon. Around 20,000 years ago as the last ice age relinquish ...
... heads the Sea Level Research Laboratory at the University of Pennsylvania. “I think the more important question is whether it’s due to anthropogenic (human-made) activity.” As Horton points out, rising sea levels aren’t a new natural phenomenon. Around 20,000 years ago as the last ice age relinquish ...
Sea floor spreading and the effects it has on the world In partnership
... Sea floor spreading has a major effect on the world. In partnership with Seth Danielson. The process of sea floor spreading of divergent tectonic plates causes the separation of continents on either side of a spreading zone. The both the largest and highest largest mountainous ridge on the planet i ...
... Sea floor spreading has a major effect on the world. In partnership with Seth Danielson. The process of sea floor spreading of divergent tectonic plates causes the separation of continents on either side of a spreading zone. The both the largest and highest largest mountainous ridge on the planet i ...
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.