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the contribution of bering sea water to the arctic ocean
the contribution of bering sea water to the arctic ocean

... Beaufort Sea gyral. The temperature maximum may be observed near the North Pole, as evidenced by the atypical station in G (the station in Fig. 1 located closestto the NorthPole).It is present to some extent over the interior of the Beaufort Sea, and it occasionally may occur in an isolated locality ...
Scott McDowell, Ph.D. The Reality of Rogue Waves
Scott McDowell, Ph.D. The Reality of Rogue Waves

... 1995 – North Sea, midway between Scotland and Norway. The stationary Draupner oil production platform, heavily instrumented with engineering sensors, yielded the first scientific confirmation of rogue waves, with a maximum height of 84 ft. 1995 – North Atlantic. The cruiser liner RMS Queen Elizabeth ...
Changing Earth
Changing Earth

... • Australia divided into three parts in Cretaceous (50 mya) • North America – several epeiric seas – most recent ended ~65 mya • Europe and Asia separated by Turgai Sea until ~30 mya ...
274 - CIESM
274 - CIESM

... eventually die due to the lack of light necessary for photosynthetic processes, but their carbon load was transported to depths. The results from optical measurements showed that POC was generally low, but with a peak at 300 m depth at M600, not corresponding with either Chl a concentration or diato ...
lecture notes
lecture notes

...  Sand is easily erosed because it is small and not cohesive  As energy decreases, particles are deposited according to size (weight) with the largest first and smallest last  More energy is required to erode than transport a particle Sedimentation in the ocean ...
Absolute Chronology of Deep-Sea Sediments and the Deposition of
Absolute Chronology of Deep-Sea Sediments and the Deposition of

... the last 14,200 years, making the rate of calcareous matter. If the observations from the accuniulation of lutite 73 mg per cmz in 1,000 English Channel are valid for ocean water, a water column of I cmz cross section in average years. ...
The Effects of Wind Forcing on Surface Currents on the Continental
The Effects of Wind Forcing on Surface Currents on the Continental

... tracking, search and rescue, harmful algal bloom monitoring, navigation, and ecosystem assessment. At present, ocean current measurements are not as readily available as winds, in large part due to the expense and difficulty of measuring ocean currents. Drifters have found to be influenced by the wi ...
File
File

...  Oil has made a HUGE difference in our lives – nearly 1/3 of the world’s oil comes from offshore fields in our oceans.  Oil accounts for almost half of the world’s sea trade  Oil comes from the skeletal remains of phytoplankton and zooplankton that settled to the sea floor, mixed with mud and sil ...
the Report
the Report

... and composition, as well as the organisms living in them, have continued to change and evolve. Today, millions of species and numerous ecosystems inhabit the oceans, from coastal areas to abysses more than 11,000 metres deep. Within their 1.4 billion cubic kilometres of water and 370 million square ...
Lecture 4 - Physical Factors - Aquatic
Lecture 4 - Physical Factors - Aquatic

... Upwelling  effects  -­‐  Ocean  chlorophyll  concentra6on   and  surface  temperature  off  the  California  coast   Phytoplankton  blooms   (orange  color  on  leq  image)   correspond  to  cool  regions   (blue  color  on  right  image).   ...
The Underwater World
The Underwater World

... It is in the offshore zone that incoming waves feel bottom and curl over as breakers or surf. The foreshore zone is regularly exposed to high and low tides. On the landward edge of the foreshore is the beach scarp, usually a rise of several feet caused by the eroding action of stronger waves. The ba ...
Submarine Geology
Submarine Geology

... deducing the minor changes of position of shorelines, and for estimating the amount of material removed from the land surfaces by the various processes of erosion. In this connection we need to know how deep wave-base is, and how effective waves and currents actually are, as scouring forces . The co ...
Marine Biomes
Marine Biomes

...  Biome : Large ecosystem with dominant life forms  Marine biomes make up the largest percentage of aquatic ...
Ecosystem Services of the Deep Ocean
Ecosystem Services of the Deep Ocean

... within it, have been designated as APEIs (Wedding et al., 2013). Other protections in international waters include the recent “biodiversity beyond national jurisdiction” (BBNJ) instrument that the United Nations is developing (Blasiak and Yagi, 2016). Marine Reserves (MRVs), another type of MPA wher ...
Oceanography – EXAM 2 Review Questions
Oceanography – EXAM 2 Review Questions

... D) the distance between the trough of a wave and the still water level. E) the distance over which the wind blows without interruption. 81) The largest wind-generated waves tend to be associated with the: A) equatorial doldrums. B) horse latitudes. C) polar regions. D) trade winds. E) westerlies. 82 ...
RepRisk Special Report - Centre for Environmental Rights
RepRisk Special Report - Centre for Environmental Rights

... However, probes in the 1970s revealed hydrothermal vents that provide nutrients and energy for an abundance of life. In recent years, over 500 previously unknown species have been discovered in deep-sea areas, some of which are of major interest to medical science. Extracting minerals from shallow d ...
Advance program as of June 27-2012
Advance program as of June 27-2012

... potential mining operations while ensuring that environmental sustainability is not compromised. Such legislation is still under development and scientific research plays a critical role in these efforts by providing support such as much needed baseline information, a robust monitoring program, and ...
A pinch of salt. A World of Science, 7, 21 - TEOS-10
A pinch of salt. A World of Science, 7, 21 - TEOS-10

... form deep water currents. Over thousands of years, these currents travel around the world until they reach areas of upwelling which bring them to the surface. Once at the surface, the sun-warmed, rain-freshened currents head back to the poles where the formation of ice allows the cycle to continue. ...
Investigation B, Ocean Bottom Topography
Investigation B, Ocean Bottom Topography

... Driving Question: How does ocean depth vary with distance from the shore? ...
Continental Drift
Continental Drift

... with respect to each other when the rate of sea floor formation differs near them, or even along their extension ‘parallel’ to the ridge. The most recent islands along the south Atlantic and Hawaiian arcs (and others around the world) are frequently actively volcanic (another indication of active up ...
Oceanography Review for Final
Oceanography Review for Final

... How does the density of ice compare to the density of liquid water?    Ice is less dense than water  In general, how does density of cold water compare with the density of warm water?    Generally, above 4oC, the density of cold water is greater than the density of warm water  In general, how does d ...
Warm ocean current reaches surprisingly far south in the
Warm ocean current reaches surprisingly far south in the

... currents in the water just north of the ice shelf front. A year later the instrumentation was recovered ecovered and the results are sensational enough to be published in Nature communications. Wind driven The new observations can also explain what drives the southward flow of warm water: it is driv ...
Chapter 6
Chapter 6

... Rotation of the Earth strongly influences winds. Coriolis deflection is the apparent deviation of objects moving across Earth’s surface. – Objects are deflected to the right of direction of travel in the northern hemisphere, – Objects are deflected to the left of direction of travel in the southern ...
Exam in BI3061 Biological Oceanography
Exam in BI3061 Biological Oceanography

... 30. Phytoplankton functional types (PFTs). What statement is correct? A. The 7 major PFTs are defined according to their biogeochemical role, light sensitivity, behaviour, and qualitative importance in specific geographical regions B. The 7 major PFTs are based on primary production characteristics ...
TSUNAMIS (full script)
TSUNAMIS (full script)

... They can be caused by earthquakes, landslides on the seafloor, land slumping into the ocean, large volcanic eruption or meteorite impact in the ocean. 75% of tsunamis are caused by earthquakes, they caused the movement of the overlying water. 8% of tsunamis are caused by underwater landslides. Only ...
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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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