File
... Narrow, high-pressure belts, centered around 30°N and S latitude, Calm waters with little wind or current and relatively dry air So-called because 16th-century sailors often threw their horses overboard to conserve drinking water because their ships slowed down so much. ...
... Narrow, high-pressure belts, centered around 30°N and S latitude, Calm waters with little wind or current and relatively dry air So-called because 16th-century sailors often threw their horses overboard to conserve drinking water because their ships slowed down so much. ...
OCEAN BASIN FLOOR - ES-Emerald(2010
... found near the center of the most ocean basins. It is characterized by extensive faulting and numerous volcanic structures that have developed on the newly formed ...
... found near the center of the most ocean basins. It is characterized by extensive faulting and numerous volcanic structures that have developed on the newly formed ...
Biomes
... Marine Habitats • Estuaries: shelf ecosystem where fresh water from streams or rivers mix with ocean water – Intertidal habitat: area that is exposed to air at low tide but under water at high tide – Salt marshes: in the intertidal zone – Mangrove swamps: occur in tropical and subtropical intertida ...
... Marine Habitats • Estuaries: shelf ecosystem where fresh water from streams or rivers mix with ocean water – Intertidal habitat: area that is exposed to air at low tide but under water at high tide – Salt marshes: in the intertidal zone – Mangrove swamps: occur in tropical and subtropical intertida ...
Ch 58 Notes
... Marine Habitats • Estuaries: shelf ecosystem where fresh water from streams or rivers mix with ocean water – Intertidal habitat: area that is exposed to air at low tide but under water at high tide – Salt marshes: in the intertidal zone – Mangrove swamps: occur in tropical and subtropical intertida ...
... Marine Habitats • Estuaries: shelf ecosystem where fresh water from streams or rivers mix with ocean water – Intertidal habitat: area that is exposed to air at low tide but under water at high tide – Salt marshes: in the intertidal zone – Mangrove swamps: occur in tropical and subtropical intertida ...
Lecture 5: Oceans & Tides
... Surface winds move over water Coriolis effect causes movement of water at an angle to the wind (to right in northern hemisphere) Water movement drags water beneath, and to right of water above Result: Shifting of water movement - Ekman Spiral (actually friction binds water together and all water mov ...
... Surface winds move over water Coriolis effect causes movement of water at an angle to the wind (to right in northern hemisphere) Water movement drags water beneath, and to right of water above Result: Shifting of water movement - Ekman Spiral (actually friction binds water together and all water mov ...
Ocean - Scholastic
... he ocean covers about 71 percent of the earth. The shallow part of the ocean lies above the continental shelf, which extends from the shoreline to the edge of each continent. Beyond that, the ocean can be more than six miles deep. Sunlight reaches to about 492 feet (150 m) beneath the water’s surf ...
... he ocean covers about 71 percent of the earth. The shallow part of the ocean lies above the continental shelf, which extends from the shoreline to the edge of each continent. Beyond that, the ocean can be more than six miles deep. Sunlight reaches to about 492 feet (150 m) beneath the water’s surf ...
Primary productivity
... • Phosphates • Iron – Amount of sunlight • Varies daily and seasonally • Sunlight strong enough to support photosynthesis occurs only to a depth of 100 meters (euphotic zone) Locations of maximum photosynthetic productivity • Margins of the oceans – Abundant supply of nutrients from land – Water sha ...
... • Phosphates • Iron – Amount of sunlight • Varies daily and seasonally • Sunlight strong enough to support photosynthesis occurs only to a depth of 100 meters (euphotic zone) Locations of maximum photosynthetic productivity • Margins of the oceans – Abundant supply of nutrients from land – Water sha ...
Centre for Interdisciplinary Marine Science Kiel University Kiel
... How can we develop environmentally friendly methods for aquaculture? ...
... How can we develop environmentally friendly methods for aquaculture? ...
Boundaries are an increasingly prominent feature of ocean policy
... that regulating the open sea is a relatively new undertaking. He says agencies have been cautious about zoning a territory so characteristically different than land. “But what we are seeing in Oregon is something that is playing out in many nearshore ocean areas around the world: the demand for ocea ...
... that regulating the open sea is a relatively new undertaking. He says agencies have been cautious about zoning a territory so characteristically different than land. “But what we are seeing in Oregon is something that is playing out in many nearshore ocean areas around the world: the demand for ocea ...
Ocean 11 - Course World
... spectacular 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 dur ...
... spectacular 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 dur ...
Seafloor Spreading - Paramus Public Schools
... – Divergent Plate boundaries • Deep Sea Trenches – Narrow Elongated depression in seafloor with very steep sides – Convergent Plate boundaries ...
... – Divergent Plate boundaries • Deep Sea Trenches – Narrow Elongated depression in seafloor with very steep sides – Convergent Plate boundaries ...
13.3 Ocean Water Chemistry
... a. Temperatures at the surface of the ocean vary with locations and seasons. Gases vary as well. b. Temperature of Ocean Water i. The surface of the ocean absorbs energy from the sun 1. Near the equator, surface water reaches 25°C ii. Warm water is less dense than cold water 1. Warm water forms a th ...
... a. Temperatures at the surface of the ocean vary with locations and seasons. Gases vary as well. b. Temperature of Ocean Water i. The surface of the ocean absorbs energy from the sun 1. Near the equator, surface water reaches 25°C ii. Warm water is less dense than cold water 1. Warm water forms a th ...
File
... water can increase ocean salinity. • In hotter areas, evaporation of water can increase ocean salinity. ...
... water can increase ocean salinity. • In hotter areas, evaporation of water can increase ocean salinity. ...
Classification of living things
... Distribution of species on Earth The land has more species because it has greater environmental variability than the ocean Most ocean species are benthic because of greater environmental variability compared to pelagic environments ...
... Distribution of species on Earth The land has more species because it has greater environmental variability than the ocean Most ocean species are benthic because of greater environmental variability compared to pelagic environments ...
JJB_South African marine biogeography
... (inversely correlated with nutrients) • SUBSTRATUM also important (particularly offshore). • Other factors determine ecological dominance of species (e.g. wave action, depth/light etc., biological interactions). ...
... (inversely correlated with nutrients) • SUBSTRATUM also important (particularly offshore). • Other factors determine ecological dominance of species (e.g. wave action, depth/light etc., biological interactions). ...
Physical Oceanography
... Tectonics can change the level of the seafloor, thus changing sea levels. ...
... Tectonics can change the level of the seafloor, thus changing sea levels. ...
1.- Título 2.- Theoretical cross section of the oceans Oceans
... habitats such as seamounts, cold water coral reefs, hydrothermal vents, cold seeps, submarine canyons, open slopes and basins. With such a diversity of habitats and features the seabed is thought to be home to 98% of all marine species, and more species may live in deep seabed environments than in a ...
... habitats such as seamounts, cold water coral reefs, hydrothermal vents, cold seeps, submarine canyons, open slopes and basins. With such a diversity of habitats and features the seabed is thought to be home to 98% of all marine species, and more species may live in deep seabed environments than in a ...
INTRODUCTION TO MARINE ECOLOGY
... • Benthic organisms are those that live in or on the ocean floor • More than 98% of known marine species are benthic • The vast majority of benthic species live within the shallow continental shelf ...
... • Benthic organisms are those that live in or on the ocean floor • More than 98% of known marine species are benthic • The vast majority of benthic species live within the shallow continental shelf ...
CoML Annual Report to the Scientific Committee on Oceanic Research
... than expected and that the vast majority of species are previously unknown, low-abundance organisms theorized to play an important role in the marine environment as part of a “rare biosphere.” The ICoMM team discovered more than 20,000 kinds of bacteria in a single liter of seawater when they expect ...
... than expected and that the vast majority of species are previously unknown, low-abundance organisms theorized to play an important role in the marine environment as part of a “rare biosphere.” The ICoMM team discovered more than 20,000 kinds of bacteria in a single liter of seawater when they expect ...
Ocean WebQuest Task Sheet PLEASE REMEMBER TO WRITE IN
... 4. What do you call the circular patterns in which the world’s oceans travel? currents 5. What body of water can these patterns be compared to? rivers 6. What else causes currents to flow? energy from the sun 7. Do all currents have the same characteristics? no 8. What makes them different?salinity, ...
... 4. What do you call the circular patterns in which the world’s oceans travel? currents 5. What body of water can these patterns be compared to? rivers 6. What else causes currents to flow? energy from the sun 7. Do all currents have the same characteristics? no 8. What makes them different?salinity, ...
OCEAN BASINS, GEOGRAPHY AND GEOLOGY OF THE OCEANS
... PLATES –lithospheric "rock"plates 100km that are the upper crust –continental, oceanic or both. Float on upper mantle as they are less dense (like suds on top of bath or dish water). CONTINENTAL MARGINS – (draw a cross section) The shape often reflects the age and the activity that has occurred alon ...
... PLATES –lithospheric "rock"plates 100km that are the upper crust –continental, oceanic or both. Float on upper mantle as they are less dense (like suds on top of bath or dish water). CONTINENTAL MARGINS – (draw a cross section) The shape often reflects the age and the activity that has occurred alon ...
Ocean WebQuest Task Sheet PLEASE REMEMBER TO WRITE IN
... 4. What do you call the circular patterns in which the world’s oceans travel? Coriolis effect 5. What body of water can these patterns be compared to? Rivers. 6. What else causes currents to flow? Energy from the sun also causes currents to flow. 7. Do all currents have the same characteristics? no ...
... 4. What do you call the circular patterns in which the world’s oceans travel? Coriolis effect 5. What body of water can these patterns be compared to? Rivers. 6. What else causes currents to flow? Energy from the sun also causes currents to flow. 7. Do all currents have the same characteristics? no ...
Introduction - Coastal Climate Wiki
... also gets saltier due to evaporation or sea ice formation. ...
... also gets saltier due to evaporation or sea ice formation. ...
Marine habitats
The marine environment supplies many kinds of habitats that support marine life. Marine life depends in some way on the saltwater that is in the sea (the term marine comes from the Latin mare, meaning sea or ocean). A habitat is an ecological or environmental area inhabited by one or more living species.Marine habitats can be divided into coastal and open ocean habitats. Coastal habitats are found in the area that extends from as far as the tide comes in on the shoreline out to the edge of the continental shelf. Most marine life is found in coastal habitats, even though the shelf area occupies only seven percent of the total ocean area. Open ocean habitats are found in the deep ocean beyond the edge of the continental shelf.Alternatively, marine habitats can be divided into pelagic and demersal habitats. Pelagic habitats are found near the surface or in the open water column, away from the bottom of the ocean. Demersal habitats are near or on the bottom of the ocean. An organism living in a pelagic habitat is said to be a pelagic organism, as in pelagic fish. Similarly, an organism living in a demersal habitat is said to be a demersal organism, as in demersal fish. Pelagic habitats are intrinsically shifting and ephemeral, depending on what ocean currents are doing.Marine habitats can be modified by their inhabitants. Some marine organisms, like corals, kelp, mangroves and seagrasses, are ecosystem engineers which reshape the marine environment to the point where they create further habitat for other organisms.