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Surface currents: See the map in your main notes for the surface
Surface currents: See the map in your main notes for the surface

... rises, becoming less dense. Dense cool air moves in and replaces the rising warm air, forming winds. Different amounts of solar energy are absorbed at different latitudes. The tropics receive direct sun; the rest of Earth receives indirect sun. ...
Chapter 13: PELAGIC COMMUNITIES
Chapter 13: PELAGIC COMMUNITIES

... the dynasties of land vertebrates. Seawater may seem to be an ideal habitat, but living in it does present difficulties. These most successful vertebrates have structures and behaviors to cope. Among them are adaptations of movement, shape, and propulsion. Active fish usually have streamlined shapes ...
Ocean life - Oakton Community College
Ocean life - Oakton Community College

... Ocean temperature Surface water temperature varies with the amount of solar radiation received • Lower surface temperatures are found in highlatitude regions • Higher temperatures found in low-latitude ...
Mineral Resources from the Ocean
Mineral Resources from the Ocean

... tropical to semitropical oceans of the world today as the result of precipitation by biological organisms ranging from mollusks to corals and plants. There is little exploitation of the modern limestones as they are forming in the oceans. However, the continents and tropical islands contain vast seq ...
Life in the Oceanic Realms - Indian Academy of Sciences
Life in the Oceanic Realms - Indian Academy of Sciences

... home to some of the most diverse and unique life forms. This article is an attempt to introduce some of the fundamentals of biological oceanography and marine biology to describe life in the sea. I’d like to be under the sea, In an octopus’s garden in the shade, We would be warm below the storm, In ...
Ocean life
Ocean life

... • Most of Earth’s biomass ...
EarthScience-Climate and Insolation review
EarthScience-Climate and Insolation review

... c. Air over the land will heat up quickly during the day, and cool quickly during the night. d. Warm (low density) air rises. Cold (dense) air sinks. e. Convection- the transfer of heat energy within the atmosphere, the hydrosphere, and Earth’s interior results in the formation of regions of differe ...
Document
Document

... Is there Life in the Deep Oceans? Deep Life? ...
Hydrothermal Vents - The Corn Group Unicorn Web Site
Hydrothermal Vents - The Corn Group Unicorn Web Site

... focusing lens with a potent laser to examine minerals, gases and liquids – even seawater itself. Pasteris' group and their MBARI colleagues are using Raman spectroscopy to see what carbon dioxide in either a pure liquid or a complex solid phase will do on the sea floor. They also are examining the f ...
This paper not to be cited without prior refernce to the
This paper not to be cited without prior refernce to the

... A general conclusi on is that the climatic conditio ns of the Barents Sea depend mainly on the activity and property in the inflowin g water from the west. Climatic variatio ns can therefor e be recorded in the sections crossing the inflowin g water masses. 3. Variatio ns in standard sections The lo ...
Ocean Currents of the Eastern Gulf of Mexico Robert H. Weisberg
Ocean Currents of the Eastern Gulf of Mexico Robert H. Weisberg

... system, which is always present. Materials entrained in the LC can quickly flow through the Florida Straits in proximity to the Florida Keys and the east coast. 2. The WFS circulation is driven mainly by winds and surface heating. The currents have well defined means and a seasonal cycle and these a ...
The history of marine biology may have begun as
The history of marine biology may have begun as

... and later in Florida on the Gulf of Mexico. She began her studies with marine botany based on her belief that vegetation is the foundation of any ecosystem. Although she struggled to balance her studies and starting a family, Earle earned her PhD from Duke University , becoming well known in the mar ...
15.2 Diversity of Ocean Life & 15.3 Oceanic Productivity
15.2 Diversity of Ocean Life & 15.3 Oceanic Productivity

... • Production of organic compounds from inorganic substances through photosynthesis or chemosynthesis • Photosynthesis – use of light energy to convert water and CO2 into glucose molecules • Chemosynthesis – process by which certain microorganisms create organic molecules from inorganic nutrients usi ...
Marine Ecosystems - National Geographic
Marine Ecosystems - National Geographic

... Salt Marshes and Mudflats are low, wet, muddy areas that lie at the interface between the land and sea. They are either periodically or continuously saturated by salt water. This requires the organisms in this ecosystem to adjust to changes in water depth, salinity, and temperature. Salt marshes are ...
Semester 1 Review - Lemon Bay High School
Semester 1 Review - Lemon Bay High School

... 51. What type of tidal patterns exists on the west coast of the United States, which receives two high tides and two low tides of varying heights per day? 52. Tidal height is compared to what reference level? 53. Most of the world's ocean coasts have a(n) _____ tidal pattern. 54. Where was the first ...
Ocean WebQuest Task Sheet PLEASE REMEMBER TO WRITE IN
Ocean WebQuest Task Sheet PLEASE REMEMBER TO WRITE IN

... 10. Besides cold water what does the Humboldt current normally bring to the surface? minerals and other nutrients that feed huge schools of fish. http://www.secretsatsea.org/story/3a.html 11. For what are currents responsible? actual transport of water from one place to ...
PDF: Printable Press Release
PDF: Printable Press Release

... the hull shifts the center of gravity to control pitch, rotating it from side to side controls roll. Smith says that gliders bring several potential benefits to ocean research. For one, because they’re propelled by buoyancy changes rather than an energy-hungry motor, they can remain in the water for ...
Chapter Outline
Chapter Outline

... offers a stable substrate (rock) that is regularly emersed and immersed by tidal water. This causes systematic variations in temperature, salinity, and sunlight exposure that depend on the stage of the tide. Furthermore, predation pressure, competition for space, and degree of desiccation change as ...
Talking points --- The High Seas: Common Heritage
Talking points --- The High Seas: Common Heritage

... the 1990s to determine which marine areas States have jurisdiction over, and which are areas of international responsibility. Since then, several agreements have been made to regulate specific activities, like seabed mining and fishing for highly migratory and straddling fish stocks. Under these tre ...
File
File

... Ocean Waters Contain Many Environments.  The Earth’s oceans can be divided into several different ...
Practice Final Exam – Oceanography – Spring 2011 Part A – The
Practice Final Exam – Oceanography – Spring 2011 Part A – The

... 34) The vertical difference between high and low tides is called the: A) ebb tide. B) flood tide. C) tidal bore. D) tidal height. E) tidal range. 35) The most common tidal pattern around the world is: A) diurnal tides. B) mixed tides. C) proxigean tides. D) semidiurnal tides. E) spring tides. 36) In ...
Ocean WebQuest Task Sheet PLEASE REMEMBER TO WRITE IN
Ocean WebQuest Task Sheet PLEASE REMEMBER TO WRITE IN

... http://www.ocean.udel.edu/extreme2002/ 23. Dive in mission to the abyss: go to seafloor geology then click on the Quicktime video to see a real undersea volcano. Click on The Deep Ocean, Mid-Ocean Ridge, Plate Tectonics and Hydrothermal Vents. Pay attention and take notes on things you’d like to in ...
Chapter 14
Chapter 14

... • Pelagic zone – open ocean of any depth • Benthic zone – includes any sea-bottom surface • Abyssal zone – a subdivision of the benthic zone • Deep • Extremely high water pressure • Low temperatures ...
Sea Floor Spreading
Sea Floor Spreading

... Without radioactive heating Earth’s core would be cold ...
henrichs-sinking particles
henrichs-sinking particles

... phytoplankton and zooplankton reflect changes in the pelagic food web. Sinking plankton (a component of “sinking particles”) collected by sediment traps mainly reflects the extent of grazing on primary production by zooplankton, and productivity variations over time. The material collected by the se ...
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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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