Reviewing for Science
... Wavelength is the space between one crest to the next crest or one trough to the next trough. Wave height the space from the resting position or surface level to the crest. The ocean waves does not move the actual water. The water stays pretty much in the same place. Breakers: when the energy of the ...
... Wavelength is the space between one crest to the next crest or one trough to the next trough. Wave height the space from the resting position or surface level to the crest. The ocean waves does not move the actual water. The water stays pretty much in the same place. Breakers: when the energy of the ...
Paleooceanography and Sea
... ocean water locally, temperature anomalies like El Niño, local gravity wells of ice sheets and land masses, and regional salinity levels that alter the water's density. – Measurement of these levels is further complicated by changes in land height as the Earth's crust moves up or down from tectonic ...
... ocean water locally, temperature anomalies like El Niño, local gravity wells of ice sheets and land masses, and regional salinity levels that alter the water's density. – Measurement of these levels is further complicated by changes in land height as the Earth's crust moves up or down from tectonic ...
Slide 1
... In addition to having wind blown surface currents the oceans also have deep currents. Deep currents are far below the surface and move more slowly than surface currents. Deep currents form as cold, dense water from the polar regions sinks and flows beneath the warmer surface waters. The movement of ...
... In addition to having wind blown surface currents the oceans also have deep currents. Deep currents are far below the surface and move more slowly than surface currents. Deep currents form as cold, dense water from the polar regions sinks and flows beneath the warmer surface waters. The movement of ...
8_Ocean126_2006
... Lava cooling underwater forms pillow lavas – Solidifies rapidly because of contact with cold seawater; this also slows flow – Water pressure keeps gases in magma “solution” during cooling ...
... Lava cooling underwater forms pillow lavas – Solidifies rapidly because of contact with cold seawater; this also slows flow – Water pressure keeps gases in magma “solution” during cooling ...
Sea Level Change and Climate - University of Hawaii at Hilo
... O (0.24%) has 8 protons and 8 neutrons, 16O (99.76%) has 8 protons and 10 neutrons Subtle differences in how these atoms behave in the world. 16O is lighter and therefore more easily evaporated. δ18O is a measure of the relative abundance of these two isotopes. Positive values have more 18O and nega ...
... O (0.24%) has 8 protons and 8 neutrons, 16O (99.76%) has 8 protons and 10 neutrons Subtle differences in how these atoms behave in the world. 16O is lighter and therefore more easily evaporated. δ18O is a measure of the relative abundance of these two isotopes. Positive values have more 18O and nega ...
Rocky Coasts
... • The animals living in the intertidal zones must be able to withstand being underwater and above water for prolonged periods. • Barnacles attach themselves to the rocks as a base and use it as leverage to sweep the surrounding area for plankton. ...
... • The animals living in the intertidal zones must be able to withstand being underwater and above water for prolonged periods. • Barnacles attach themselves to the rocks as a base and use it as leverage to sweep the surrounding area for plankton. ...
Oceans - Geophile.net
... • Upwelling is the upward motion of water. – This motion brings cold, nutrient rich water towards the surface. ...
... • Upwelling is the upward motion of water. – This motion brings cold, nutrient rich water towards the surface. ...
Ocean Currents - WordPress.com
... ◦ The first research ship to study oceans ◦ Investigated ocean currents, water temperature, and chemical composition of the oceans ◦ Used sonar to map the seafloor features of the South Atlantic Ocean (including the Mid-Atlantic Ridge) ◦ Continually monitors ocean surface temperatures, currents, and ...
... ◦ The first research ship to study oceans ◦ Investigated ocean currents, water temperature, and chemical composition of the oceans ◦ Used sonar to map the seafloor features of the South Atlantic Ocean (including the Mid-Atlantic Ridge) ◦ Continually monitors ocean surface temperatures, currents, and ...
Law Content
... through the services they provide Recognize the need to protect and conserve the ocean’s biodiversity and ecosystems Learn how to sustainably utilize biodiversity and ecosystems Understand the concept of seaeconomy and MSP, in light of the applicable legal framework being fragmented (UNCLOS, UNESCO, ...
... through the services they provide Recognize the need to protect and conserve the ocean’s biodiversity and ecosystems Learn how to sustainably utilize biodiversity and ecosystems Understand the concept of seaeconomy and MSP, in light of the applicable legal framework being fragmented (UNCLOS, UNESCO, ...
Unit 2 Vocabulary Review
... a measure of the amount of dissolved salts in a given amount of liquid ...
... a measure of the amount of dissolved salts in a given amount of liquid ...
Unit 2 Vocabulary Review
... a measure of the amount of dissolved salts in a given amount of liquid ...
... a measure of the amount of dissolved salts in a given amount of liquid ...
Oceans: Chapters 19, 20, and 21
... 29. What is the major cause of tides. 30. If high tide is at 4:00pm today, at about what time will high tide occur tomorrow? 31. The curving of the path of ocean currents and wind belts is called _____. 32. What is the cause of deep currents? 33. Calling a tsunami a tidal wave is misleading because ...
... 29. What is the major cause of tides. 30. If high tide is at 4:00pm today, at about what time will high tide occur tomorrow? 31. The curving of the path of ocean currents and wind belts is called _____. 32. What is the cause of deep currents? 33. Calling a tsunami a tidal wave is misleading because ...
Ocean Topography presentation
... How do submarine canyons form? Thought to be fast moving currents and underwater landslides. ...
... How do submarine canyons form? Thought to be fast moving currents and underwater landslides. ...
Ocean Water Chemistry
... • Exists as gas, liquid, & solid on Earth’s surface • Remarkably high heat capacity (specific heat) makes it slow to heat and slow to cool • Very high solvent power (dissolves everything!) • Molecule is “dipolar” (hydrogen[+], oxygen [-]) • Expands when freezes (ice floats, role in erosion) • Water ...
... • Exists as gas, liquid, & solid on Earth’s surface • Remarkably high heat capacity (specific heat) makes it slow to heat and slow to cool • Very high solvent power (dissolves everything!) • Molecule is “dipolar” (hydrogen[+], oxygen [-]) • Expands when freezes (ice floats, role in erosion) • Water ...
Hazards Chapter3b
... … the Islands rarely if ever experience an earthquake (did just have a 6.6 on 10/15/06), since 1819 have experienced about 40 tsunami episodes … location makes it a target ...
... … the Islands rarely if ever experience an earthquake (did just have a 6.6 on 10/15/06), since 1819 have experienced about 40 tsunami episodes … location makes it a target ...
PPT
... Compression waves (Pwaves): travel by squeezing and expanding medium they travel through. They can travel through both solids and liquids (e.g., sound waves). Shear waves (S-waves): travel by shearing medium they pass through. S-waves can travel only through solids since particles need to be bonded ...
... Compression waves (Pwaves): travel by squeezing and expanding medium they travel through. They can travel through both solids and liquids (e.g., sound waves). Shear waves (S-waves): travel by shearing medium they pass through. S-waves can travel only through solids since particles need to be bonded ...
Theory of Plate Tectonics
... Evidence from mapping the sea floor: When explorers began to map the ocean floor, they discovered undersea mountain running north to south down the length of the Atlantic Ocean, which they named the Mid-Atlantic Ridge. ...
... Evidence from mapping the sea floor: When explorers began to map the ocean floor, they discovered undersea mountain running north to south down the length of the Atlantic Ocean, which they named the Mid-Atlantic Ridge. ...
PDF file - Around the Americas
... 2009 and has successfully sailed through the Northwest Passage, continued down the east coast, around Cape Horn and is sailing along the west coast returning finally to Seattle in June 2010. It will visit approximately 40 ports along its journey. North and South America are continent-islands surroun ...
... 2009 and has successfully sailed through the Northwest Passage, continued down the east coast, around Cape Horn and is sailing along the west coast returning finally to Seattle in June 2010. It will visit approximately 40 ports along its journey. North and South America are continent-islands surroun ...
Mapping the Ocean Floor
... the rift valley, a deep V-shaped notch. From this valley, new oceanic crust is constantly being extruded from Earth's mantle by processes not yet fully understood. In the case of the Mid-Atlantic rift valley, one sheet flows east and the other west, each moving at about half an inch per year. ...
... the rift valley, a deep V-shaped notch. From this valley, new oceanic crust is constantly being extruded from Earth's mantle by processes not yet fully understood. In the case of the Mid-Atlantic rift valley, one sheet flows east and the other west, each moving at about half an inch per year. ...
Aquatic Science Final Review (Semester 1)
... 4.What is a renewable resource? Give examples. What is a nonrenewable resource? Give examples. ...
... 4.What is a renewable resource? Give examples. What is a nonrenewable resource? Give examples. ...
Chemical and Physical Properties of Seawater
... Equator is warmer than poles – more heat energy absorbed here Less dense hot air rises Cooler air replaces it Wind is formed! Remember, winds to not travel straight, they are bent by Coriolis Effect ...
... Equator is warmer than poles – more heat energy absorbed here Less dense hot air rises Cooler air replaces it Wind is formed! Remember, winds to not travel straight, they are bent by Coriolis Effect ...
Part2-Summary of Sediments
... - Sediment layers are thickest near the continents, the source of lithogenous material, and thinner farther out to sea. - If you determine that the seds are lithogenous, next check grain size: are they fine, medium or coarse? Sediments are coarsest near the continental source: the farther from the s ...
... - Sediment layers are thickest near the continents, the source of lithogenous material, and thinner farther out to sea. - If you determine that the seds are lithogenous, next check grain size: are they fine, medium or coarse? Sediments are coarsest near the continental source: the farther from the s ...
Sea Floor Spreading
... The heat from Earth's interior is released to the surface as heat flow. Current models indicate that heat moves to the surface with magma in convective motion. Most of the heat is carried to regions of mid-ocean ridges. Heat flow measurements at ocean ridges can be 8X greater than other parts of Ear ...
... The heat from Earth's interior is released to the surface as heat flow. Current models indicate that heat moves to the surface with magma in convective motion. Most of the heat is carried to regions of mid-ocean ridges. Heat flow measurements at ocean ridges can be 8X greater than other parts of Ear ...
Oceanography
... 7. breaker – high wave crest that has been pulled down by gravity 8. surf – area between the breaker zone and the shore 9. white caps – wave crests breaking into white foam ...
... 7. breaker – high wave crest that has been pulled down by gravity 8. surf – area between the breaker zone and the shore 9. white caps – wave crests breaking into white foam ...
Ch. 22 The Water Planet
... characteristics of water masses that help scientists study oceans and their ...
... characteristics of water masses that help scientists study oceans and their ...
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.