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CSIR - National Institute of Oceanography
CSIR - National Institute of Oceanography

... North Indian Ocean, particularly along Indian coasts. Observations and models have shown that circulation needs to be looked at holistically across the basin because the winds at a location influence not only the local current, but have an impact on the current at remote locations at a later time th ...
Arctic Fisheries and International Law
Arctic Fisheries and International Law

... • Characteristics compared to more southerly areas: – Data, knowledge and insight in ecosystems limited – Currently no large-scale commercial fisheries and - in the high seas portion - no fisheries at all High seas pockets: Central Arctic Ocean, Banana Hole, Loophole and Donut Hole 1 or 2 pockets of ...
Climatic Consequences of Long-term Global Salination of Ocean
Climatic Consequences of Long-term Global Salination of Ocean

... The long-term salination of two major osmolyte systems, the ocean and the inner environment of vertebrates has been compared. The average osmolality of today’s sea (1.09 Osm) is more than three times higher than that of the blood of land vertebrates (~0.3 Osm). Of the two major strategies for ionic ...
08_chapter 1
08_chapter 1

... there are small to insignificant effects from glacial eustasy due to mass distribution. Similarly, the effects on the water column are seen only to be in the order of decimeters at the most (Nakiboglu and Lambeck, 1991; Momer, 1994). The major effects are instead, the dynamic redistribution of water ...
11. Prodi Oseanografi (S-1)
11. Prodi Oseanografi (S-1)

... zones, shelf continent, open sea, island regimes and marine territorial, marine protection and conservation, problem solving of international sea dispute. OS1110 Oceanography (2) Syllabus This course provides an overview about the important of oceanography dealing with marine resource exploitation. ...
Seawater - Odyssey Expeditions
Seawater - Odyssey Expeditions

... scientists have recently speculated that comets entering the Earth's atmosphere may be another important source of water for the oceans. Most of the dissolved chemical constituents or salts found in seawater have a continental origin. It seems that these ...
Spirula
Spirula

... mouths, and huge stomachs that help them survive in a habitat with limited food. • The environmental conditions of the deep sea have been relatively stable for more than 100 million years, and as a result, several organisms have changed very little from when they first evolved. © 2006 Thomson-Brooks ...
Plankton - Cabrillo Marine Aquarium
Plankton - Cabrillo Marine Aquarium

... A thermocline in the ocean is a region of rapid temperature change with depth. Where there is a strong thermocline, there is little vertical mixing of water since cold water is heavier and stays below warmer surface water. ...
6th Grade Great Barrier Reef
6th Grade Great Barrier Reef

... There are a few places, such as Iceland and the Azores, where the ridge pokes above the ocean's surface. ...
Mining Industry - Cluster Maritime Français
Mining Industry - Cluster Maritime Français

... apply an integrated, global approach,and it indeed provides an optimum sharing of technical risk between the public and private sectors, where each participant contributes its own particular knowledge and expertise. On that basis, scientists working on the Ifremer research vessel “L’Atalante” collec ...
Chapter 4 - McGraw Hill Higher Education
Chapter 4 - McGraw Hill Higher Education

... Related or supporting concepts: - Early mariners, and even scientists, had no idea how deep the oceans are or how rugged their bathymetry is. - In about 85 B.C. Posidonius, a Greek geographer, used a large rock tied to a rope to measure a depth of 2 km (1.2 mi) in the Mediterranean Sea. - Soundings, ...
chapter 3 - McGraw Hill Higher Education
chapter 3 - McGraw Hill Higher Education

... c. are typically seismically and/or volcanically active, and d. tend to be relatively narrow. - Continental shelves are very flat edges of the continental crust covered by marine waters. The average maximum depth of the shelves is 130 m (427 ft) and their average width is 65 km (40 mi). While these ...
Innovative, non-destructive techniques and methodologies
Innovative, non-destructive techniques and methodologies

... communities are facing a major challenge: to work together with the aim to develop science driven, innovative, non-destructive technologies designed to work in shallow and very shallow waters and able to support high resolution survey, early detection and mapping of archaeological sites and prehisto ...
Ocean Acidification: The Other CO2 Problem
Ocean Acidification: The Other CO2 Problem

... weaker shells in nearly all species studied. If acidity gets high enough, ocean water becomes corrosive and literally dissolves the organism’s shells. This may lead to their extinction. Ocean acidification could result in a “global osteoporosis,” harming not only commercially important shellfish, su ...
Deep convection in the Irminger Sea forced by the Greenland tip jet
Deep convection in the Irminger Sea forced by the Greenland tip jet

... there are 10 major events from mid-December to mid-March. As there are often significant events in late autumn and early spring, as well as numerous mild events throughout the winter, we parameterized this by applying 14 equally strong events over 120 days (each event lasts 4 days and they are space ...
Marine Pollution
Marine Pollution

... from ballast tanks can spread harmful algae and other invasive species. 5. Atmospheric Pollution: Wind blows dust and debris, including plastic bags, seaward from landfills and other areas. Climate change is raising ocean temperatures and raising levels of carbon dioxide in the atmosphere. These ris ...
Strand: Interrelationships in Earth/Space Systems
Strand: Interrelationships in Earth/Space Systems

... characteristics of the ocean environment. Key concepts include geological characteristics (continental shelf, slope, rise); physical characteristics (depth, salinity, major currents); biological characteristics (ecosystems); and public policy decisions related to the ocean environment (asses ...
Magnitude 7.1 MOLUCCA SEA
Magnitude 7.1 MOLUCCA SEA

... Magnitude 7.1 MOLUCCA SEA Saturday, November 15, 2014 at 02:31:40 UTC ...
Oceans - SolPass
Oceans - SolPass

... 37. In the ocean, as depth increases: (choose all that apply) a. *temperature decreases b. *pressure increases c. *the amount of light decreases 38. Ocean water is a mixture of: a. *air and salts (especially sodium chloride) b. soil and sugar 39. The salinity of the ocean depends on: (choose all tha ...
Word - SolPass
Word - SolPass

... characteristics of the ocean environment. Key concepts include geological characteristics (continental shelf, slope, rise); physical characteristics (depth, salinity, major currents); biological characteristics (ecosystems); and public policy decisions related to the ocean environment (asses ...
The role of operational ocean forecasting in e
The role of operational ocean forecasting in e

... changes in climate have been observed. These include changes in arctic temperatures and ice, widespread changes in precipitation amounts, ocean salinity, wind patterns and aspects of extreme weather including droughts, heavy precipitation, heat waves and the intensity of tropical cyclones. Global av ...
Oceans - SolPass
Oceans - SolPass

... 37. In the ocean, as depth increases: (choose all that apply) a. temperature decreases b. pressure increases c. the amount of light decreases 38. Ocean water is a mixture of: a. air and salts (especially sodium chloride) b. soil and sugar ...
Word - SolPass
Word - SolPass

... Plant-like plankton (phytoplankton) produce much of the Earth’s oxygen and serve as the base of the ocean ecosystem. Plankton flourish in areas where nutrient rich water upwells from the deep. Phytoplankton are eaten by animal-like plankton, swimming organisms, and those things that live on the oc ...
Non-Radioactive Ocean Pollution
Non-Radioactive Ocean Pollution

... the world's population with a vital source of food. Unfortunately, despite their importance, these vast bodies of seawater have long been regarded as too large to ever be harmed or threatened by human activities. Yet the marine environment is delicate and, especially now, highly fragile because of t ...
exploring the ocean floor - Brighten Academy​Middle School
exploring the ocean floor - Brighten Academy​Middle School

... Extends from the base of the continental rise into deep ocean basins. Among Earth’s flattest and smoothest regions an the least explored. Formed by particles of sediment slowly drifting onto the deep ocean floor. Most abyssal plains occur in the Atlantic and Indian oceans. Cover about 40% of the oce ...
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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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