• Study Resource
  • Explore
    • Arts & Humanities
    • Business
    • Engineering & Technology
    • Foreign Language
    • History
    • Math
    • Science
    • Social Science

    Top subcategories

    • Advanced Math
    • Algebra
    • Basic Math
    • Calculus
    • Geometry
    • Linear Algebra
    • Pre-Algebra
    • Pre-Calculus
    • Statistics And Probability
    • Trigonometry
    • other →

    Top subcategories

    • Astronomy
    • Astrophysics
    • Biology
    • Chemistry
    • Earth Science
    • Environmental Science
    • Health Science
    • Physics
    • other →

    Top subcategories

    • Anthropology
    • Law
    • Political Science
    • Psychology
    • Sociology
    • other →

    Top subcategories

    • Accounting
    • Economics
    • Finance
    • Management
    • other →

    Top subcategories

    • Aerospace Engineering
    • Bioengineering
    • Chemical Engineering
    • Civil Engineering
    • Computer Science
    • Electrical Engineering
    • Industrial Engineering
    • Mechanical Engineering
    • Web Design
    • other →

    Top subcategories

    • Architecture
    • Communications
    • English
    • Gender Studies
    • Music
    • Performing Arts
    • Philosophy
    • Religious Studies
    • Writing
    • other →

    Top subcategories

    • Ancient History
    • European History
    • US History
    • World History
    • other →

    Top subcategories

    • Croatian
    • Czech
    • Finnish
    • Greek
    • Hindi
    • Japanese
    • Korean
    • Persian
    • Swedish
    • Turkish
    • other →
 
Profile Documents Logout
Upload
Neritic Zone - SmartScience
Neritic Zone - SmartScience

... water temperature stays stable this allows many types of plant and animal species to thrive in the ...
Climate and fish - Havforskningsinstituttet
Climate and fish - Havforskningsinstituttet

... this area. At the same time, we are seeing changes in their overwintering patterns, so it appears that there is a chance of herring resuming their old pattern of migration and return to their former feeding grounds. ...
MIT Sea Grant College Program
MIT Sea Grant College Program

... AUTOMATED UNDERWATER VEHICLES The work of MIT Sea Grant funded Doherty Associate Professor in Ocean Utilization, Pierre Lermusiaux, was recently featured on the MIT News site in an article by David L. Chandler: ...
Unit 9 Day 1 Notes
Unit 9 Day 1 Notes

... 1. Discuss the origin of the oceans and describe the distribution of oceans and seas 2. Describe the composition of sea water and variations in salinity concentrations 3. Explain ocean layering and effects of 4. Describe variations in ...
Journey to the bottom of the ocean (1)
Journey to the bottom of the ocean (1)

... Seamount rises above water ...
Hydrothermal Vents
Hydrothermal Vents

... Vents are often far apart. They often exist for just a few decades or years. New vents are populated very quickly. ...
Poor Wegener - Issaquah Connect
Poor Wegener - Issaquah Connect

... Wegener’s continental drift idea wasn’t accepted. ...
Where did the water for the oceans come from?
Where did the water for the oceans come from?

... • Less dense - 2.7 g/cm3 ...
biome sydney 4
biome sydney 4

... pelagic zone is where one can find wales because it is very far away from the land in contrast to the intertidal zone, and tends to be very cold due to its deepness. – Next is the Benthic Zone which is below the pelagic zone. Temperature drops drastically from the last zone and the depth increases. ...
Ch 15 Earth`s Oceans
Ch 15 Earth`s Oceans

... 6. What is the relationship between the wave speed in deep water and wavelength? Wave speed increases cold with wavelength. 7. Describe how an ocean wave becomes a breaker at the shoreline.As ocean waves reach the shallow water near shorelines, ...
Key Action 3: Sustainable Marine Ecosystems
Key Action 3: Sustainable Marine Ecosystems

... Marine Ecosystems’ Main MAST III (FP4) projects with relevance to the new FP5, EESD KA3 topics. Important note: the projects below were not aimed specifically to nor funded under the headings of FP5. Therefore their association to those headings is only orientative and has no official character. For ...
Chapter 2
Chapter 2

... mantle material rises up through the rift • This molten rock pushes the oceanic crust up to form the mid-ocean ridge and new oceanic crust • Therefore the rifts are known as spreading ...
Chapter 10: Siliciclastic Marine Environments The Shelf
Chapter 10: Siliciclastic Marine Environments The Shelf

... •Wide diversity and abundance of normal marine fossil organisms •Diagnostic association of trace fossils More specific characteristics are related to deposition under tidedominated or storm-dominated conditions. ...
ocean currents - Team Strength
ocean currents - Team Strength

... hydrosphere is what separates us from the other planets.  Earth’s vast quantities of water make life as we know it possible  About 70% of Earth’s surface is covered in water - most of which is found in the oceans ...
1 Sounding the Deep
1 Sounding the Deep

... • Results in strong regional differences in the amplitude of tides, the evenness of the expected two high and two low tides per lunar day (e.g., in Pacific NW, there is only one strong low tide per day, while the other “low” tide is nearly as high as the high tides ...
Oceanography Chapter 4 Bathymetry
Oceanography Chapter 4 Bathymetry

... Shelf Break – makes the abrupt transition from continental shelf to continental slope ♦ water depth – 140 m (460 ft) ♦ exceptions in Antarctica/Greenland (300-400) Submarine Canyons ♦ Cut into shelf and slope ♦ Some as big as Grand Canyon ♦ How? Originally thought that they may have formed from sea ...
Chapter 31 Conclusions on Other Human Activities
Chapter 31 Conclusions on Other Human Activities

... The network of shipping routes covers the whole ocean. There are particular choke points, where large numbers of ships pass through relatively limited areas, with consequent increases in the risks of both disasters and chronic pollution problems. The impending opening of the Panama Canal to larger s ...
OCEAN BASINS, GEOGRAPHY AND GEOLOGY OF THE OCEANS
OCEAN BASINS, GEOGRAPHY AND GEOLOGY OF THE OCEANS

... Continental crust or lithosphere – 100km thick Heat driven motion at the core creates convection currents and causes flowing and movement. HISTORY 200 million years ago – supercontinent Pangaea –Sea was Panthalassa – ancestor of Pacific –Tethy's sea separated Eurasia and Africa 180mya – Pangaea spli ...
Life in the Ocean - Faculty Bennington
Life in the Ocean - Faculty Bennington

... arth is misnamed. Even though the planet is largely made up of rock, 71 percent of its surface is covered with ocean. Like the wet film coating a newly washed plum, this water makes up a thin layer compared with the globe as a whole. Yet that watery veneer comprises more than 90 percent of the biosp ...
Get Up and Go
Get Up and Go

... was very calm. But at the bottom of the sea, a big piece of the sea floor suddenly moved. The movement caused a big earthquake. The earthquake registered, or was measured, at 9.0 on the Richter scale. The Richter scale is the measurement scientists use to tell others how strong an earthquake is. As ...
Ocean Bottom Relief
Ocean Bottom Relief

... temperature and density. These currents aid in the transport of excess energy from the tropics to the higher latitudes and have a profound influence on global climates. The most important ocean currents are those at and near the surface because they interact with the atmosphere and coast and affect ...
Midterm Exam 1 Study Guide
Midterm Exam 1 Study Guide

... What is the principle of constant proportions? Why does it save oceanographers time? What are the various ways salinity can be measured? How should it not be measured? What is the easiest and most popular method today? When a region of ocean has high salinity, what does that suggest? What is suggest ...
ocean zones - Somerset Academy
ocean zones - Somerset Academy

... Usually sub-divided by depth or amount of sunlight. The upper pelagic receives sunlight, so there are many phytoplankton for photosynthesis. Zooplankton, jellyfish, squid, and fishes of all sizes make up the food chain. The lower reaches receive less or no sunlight, so there are no plants and animal ...
Oceanographer publishes atlas of seafloor volcanoes
Oceanographer publishes atlas of seafloor volcanoes

... environments in the ocean depths. "This book lets people see parts of the Earth that most of them have never seen or thought about before, and the processes that form fundamental parts of our planet—and it does it in a very illustrative way," said co-lead author Deborah Kelley, a professor in the UW ...
Plate Tectonics
Plate Tectonics

... from the same earthquake arrive at 1:26:20. What is the distance from the epicenter to the seismic station? 2800 km ...
< 1 ... 41 42 43 44 45 46 47 48 49 ... 68 >

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.
  • studyres.com © 2025
  • DMCA
  • Privacy
  • Terms
  • Report