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Ocean Zones Ch14 - Stephanie Dietterle Webpage
Ocean Zones Ch14 - Stephanie Dietterle Webpage

... – As water in a tide pool is warmed by the sun, the water begins to evaporate with the remaining water being more salty – Organisms that live in a tide pool much be able to withstand the changes in temp and salinity • Example: sea urchin ...
chapter 8 ocean in the earth system
chapter 8 ocean in the earth system

... dissolved load of rivers is 119 parts per million, as compared to 35 parts per thousand for typical ocean water; that is, the ocean is about 300 times saltier than most rivers. Chloride and sodium ions, the most common constituents of seawater, are very limited in river water. And the carbonate ion, ...
Microplastics in Seawater: Recommendations from the
Microplastics in Seawater: Recommendations from the

... Most studies have been from surface water using neuston nets (Hidalgo-Ruz et al., 2012); manta and bongo nets have also been used at the sea surface. Since most plastics are buoyant they are likely to accumulate at the sea surface. Another instrument, that is widely deployed on a global scale and th ...
South China Sea - The Oceanography Society
South China Sea - The Oceanography Society

... of the sea surface and appear as bands of light and dark patterns that form a two-dimensional snapshot at a fixed point in time of the wave positions in the South China Sea. While the in situ measurements acquired during each of the field programs produced data on the nonlinear internal waves with a ...
Teacher Resources - Fish Eye Project
Teacher Resources - Fish Eye Project

... Ø Can  you  list  the  main  challenges  of  living  at  vents?   Answer:  High  pressure,  less  oxygen,  lack  of  day  light,  water  acidity,  water  temperature   Ø Can  you  find  a  few  strategies  that  organisms  have  to ...
Document
Document

... Scotland. And together with the team of scientists from the Scottish Association for Marine Science I study the effects of hypoxia in Scottish sea loch which is called Loch Etive. This is a multi-silled fjord with restricted circulation, basically consisting of two basins – one lower well ventilated ...
Ecological values of the 12 miles zone of Bonaire
Ecological values of the 12 miles zone of Bonaire

... the water structure is highly stratified in the upper 1200 meters; weakly stratified between 1,200 and 2,000 meters and uniform below 2000 meters (Gyory et al. 2005; Lutz and Ginsburg 2007). Through much of the Caribbean there is a permanent thermocline (a steep temperature gradient) at a depth of a ...
Upper Arctic Ocean water masses harbor distinct
Upper Arctic Ocean water masses harbor distinct

... Abstract. The ubiquity of heterotrophic flagellates (HFL) in marine waters has been recognized for several decades, but the phylogenetic diversity of these small (ca. 0.8–20 µm cell diameter), mostly phagotrophic protists in the upper pelagic zone of the ocean is underappreciated. Community composit ...
28. Miocene Evaporates in Red Sea Cores, Their Relevance to the
28. Miocene Evaporates in Red Sea Cores, Their Relevance to the

... 60-65 km of offset can only be determined as postCretaceous. Taking the Miocene/Pliocene boundary at 5 m.y., this implies that the mean velocity along the Dead Sea shear zone over the last 5 m.y. is 0.8 to 0.9 cm/yr.The whole 105-km offset may have been effected continuously at this rate but it is o ...
Atmosphere-Ocean Coupling and Surface Circulation of the Ocean
Atmosphere-Ocean Coupling and Surface Circulation of the Ocean

... at high latitudes move equatorward. Complex and littleunderstood feedback loops characterize these processes and assure that any change in the behavior of the atmosphere or ocean will have profound consequences for the circulation of both systems. The hypersensitive interrelationships between the at ...
Modelling the tides and their impacts on the vertical stratification
Modelling the tides and their impacts on the vertical stratification

... reduced along nearly straight lines parallel to the bathymetry. Two hours later (Figure 4b), the sea surface height was reduced to almost half of the previous value. Four hours after high tide (Figure 4c), the amplitude was almost uniform across the bank. The negative signal offshore indicated a tid ...
WORD - ozeanklima.de
WORD - ozeanklima.de

... Oceans do not take account of boundaries, legal systems do. The present legal approach is based on the condition, human activity and impact on human, as defined by the term 'pollution'. The concept derives from managing territories on the continents. While they are static, the oceans are in permanen ...
MAPA TOPOBATIMTRICO EN RELIEVE
MAPA TOPOBATIMTRICO EN RELIEVE

... and their origin more widely. After making different hypothesis about their formation, he finally concluded that submarine canyons do not respond to one single cause, but to several causes which can play a significant role in their origin and development: subaereal erosion, turbidity currents, fault ...
Types of seismic waveS
Types of seismic waveS

... Secondary waves (S-waves) are shear waves that are transverse in nature. These waves arrive at seismograph stations after the faster moving P waves during an earthquake and displace the ground perpendicular to the direction of propagation. Depending on the propagational direction, the wave can take ...
GSA-Charlotte 2012
GSA-Charlotte 2012

... 1.6, 2 and 2.6 Ga. In addition, the apparent correspondence of supercontinents with ice ages, and their break-up with major evolutionary events, suggested a controlling connection between supercontinents, climate and life, which they suggested was a consequence of the profound effect of the supercon ...
North Atlantic ecosystem sensitivity to Holocene shifts in Meridional
North Atlantic ecosystem sensitivity to Holocene shifts in Meridional

... Bryden, 1982]. The NAC follows the boundary between the North Atlantic subpolar gyre (SPG) and the subtropical gyre (STG), and its density and flow are modulated by the SPG [Hátún et al., 2005]. During periods when the SPG is enhanced (elongated E-W with strong outgrowth into the eastern Atlantic), t ...
Quantifying sea surface temperature ranges of the Arabian Sea for
Quantifying sea surface temperature ranges of the Arabian Sea for

... δ 18 O – salinity relationship in the northern Indian Ocean. Using atmospheric fluxes corresponding to Last Glacial Maximum (LGM) conditions in a multibox model, the authors conclude that there was no important change within the δ 18 O – salinity relationship during this period compared to the prese ...
Exploring the distance between nitrogen and
Exploring the distance between nitrogen and

... Part of the sampling for this study was performed in mesocosms designed to study acidification effects. In the Baltic, the water was collected as integrated samples (depth 0–10 m) in Storfjärden near Tvärminne field station (59◦ 51.500 N, 23◦ 15.500 E) on 6 August 2012. The collection was performed ...
Lesson I: Why the Oceans are Important!
Lesson I: Why the Oceans are Important!

... • The oceans contain 99 percent of the living space on the planet. The Pacific Ocean is 25% larger than all the land areas combined. • Coral is used in place of bone grafts, its structure is close to that of human bone. • The average depth of the ocean is 3800 meters (about 2 miles) • The deepest pl ...
SOUTHWEST NEW BRUNSWICK SEA CUCUMBER (CUCUMARIA
SOUTHWEST NEW BRUNSWICK SEA CUCUMBER (CUCUMARIA

... other sea cucumber species commonly harvested elsewhere. Adults attach to the bottom using tube feet, filter feed plankton from the water column, and are thought to exhibit low rates of movement. The eggs and larvae of sea cucumber are pelagic. There is very limited information on the life history c ...
Ecosystems and Biodiversity in Deep Waters and High Seas
Ecosystems and Biodiversity in Deep Waters and High Seas

... expression of any opinion whatsoever on part of UNEP or contributory organizations concerning the legal status of any country, territory, city or area in its authority, or concerning the delimitation of its frontiers or boundaries. Moreover, the views expressed do not necessarily represent the decis ...
mare nostrum - Association of European Border Regions
mare nostrum - Association of European Border Regions

... www.env.duth.gr/eet ...
earth science 140 - College of DuPage
earth science 140 - College of DuPage

... temperature (SST). Also relate the angles of solar energy receipt to the patterns of light distribution with increasing depth that you learned in the previous unit. ...
Tidal Energy and Large-Scale Fish Farming, Benefits
Tidal Energy and Large-Scale Fish Farming, Benefits

... The devastating tsunamis December 26, 2004 at the shores of Indian Ocean killing more than 200’000 people and in Honshu, Japan March 11, 2011 with more than 20’000 fatalities and political consequences from the Fukushima catastrophe are still remembered. Despite expensive tsunami warning systems sum ...
Analysis of wave heights and wind speeds in the Adriatic Sea
Analysis of wave heights and wind speeds in the Adriatic Sea

... more developed sea state, these waves should persist longer on the sea surface than less developed, steeper waves that tend to diminish more quickly. These findings are in line with those found in the reviewed literature. From the wind polar plot it can be noticed that the strongest winds are record ...
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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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