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Evidence for both crustal and mantle earthquakes in the subducting
Evidence for both crustal and mantle earthquakes in the subducting

... with our observation, that the upper and lower seismic layer represent the brittle upper oceanic crust and the brittle uppermost mantle, respectively, with the two seismic layers being separated by a ductile lower oceanic crust. [14] Kirby et al. [1996] showed that large volume changes related to th ...
FIO_AISO_PROPOSAL - USF College of Marine Science
FIO_AISO_PROPOSAL - USF College of Marine Science

... capabilities throughout the State. This AISO will promote increased scientific collaboration and economy of human resources. This new AISO will transform the way we conduct coastal ocean research and education in Florida and bring the State of Florida/SUS and other members to national prominence in ...
The Effect of Milankovitch Variations in Insolation on Equatorial
The Effect of Milankovitch Variations in Insolation on Equatorial

... top of the atmosphere (TOA) is depicted. Minimum OLR values indicate the location of the ITCZ as high clouds there associated with the ITCZ emit low longwave radiation because of their cold cloud-top temperature. There are also indications that the phase locking of ENSO to the seasonal cycle may be ...
How large is the subducted water flux? New constraints on mantle
How large is the subducted water flux? New constraints on mantle

... seawater infiltration along transform faults or deep faults (15–20 km) into the oceanic plate at the outer rise (Nedimovic et al., 2009; Ranero et al., 2003, 2005), the degree and spatial extent of serpentinization around the faults remain poorly constrained. Reasonable physical considerations can be ...
Parai and Mukhopadhyay 2012
Parai and Mukhopadhyay 2012

... seawater infiltration along transform faults or deep faults (15–20 km) into the oceanic plate at the outer rise (Nedimovic et al., 2009; Ranero et al., 2003, 2005), the degree and spatial extent of serpentinization around the faults remain poorly constrained. Reasonable physical considerations can be ...
seasonal variation of temperature and salinity at 10 meters in the
seasonal variation of temperature and salinity at 10 meters in the

... percent were “net-haul” stations, where work consisted of biological sampling and a 10-meter temperature and salinity measurement. The 10-meter level was chosen to represent the upper mixed layer in lieu of a surface sample to avoid such transient conditions as might be caused by rain or river runof ...
What are the FOUR (4) WAYS our Earth*s PLATES MOVE?
What are the FOUR (4) WAYS our Earth*s PLATES MOVE?

... Is it ocean crust from ocean crust diverging? ...
Mass balance related to UHP metamorphism in subduction zones
Mass balance related to UHP metamorphism in subduction zones

... - largely immobile (done) - global deep mass balance ...
Variability of currents in front of the Venice Lagoon, Northern Adriatic
Variability of currents in front of the Venice Lagoon, Northern Adriatic

... consideration the effects of highly-variable wind regimes. The purpose of the present work is to extend the analysis of the response of near-surface currents to highly-variable winds, study its structure along the water column and assess the response time-scales, based on subsurface current records ...
Guide to satellite remote sensing of the marine environment
Guide to satellite remote sensing of the marine environment

... it is true to say that for a considerable time the concept of 'oceanography from space' remained more of a promise than a reality. It is not difficult to find reasons. In the earlier years it was hardly surprising that a satellite sensor orbiting the earth at a height of about 1,OOO km, and travelli ...
Introduction To Marine Biology
Introduction To Marine Biology

... • The water is never so deep as to take it out of the photic zone. • This results in high primary production and makes the subtidal zone the location of the majority of sea life. ...
Role of the low-latitude ocean
Role of the low-latitude ocean

... why OGCMs are more low-latitude sensitive than box models. We compare the low-latitude sensitivities of the 3-box model of Toggweiler et al. [2003], the 5-box model with an explicit thermocline box of Follows et al. [2002], and a 3-dimensional abiotic carbon cycling model based on the OGCM of Primea ...
Plate Tectonics - El Camino College
Plate Tectonics - El Camino College

... the side or bottom of another plate, and the friction between them keeps them from moving. In addition, the rock in front of a moving plate (another plate or the semi-solid asthenosphere) can block it, possibly forcing it to bend. ...
Review of Soundings: The Story of the Remarkable Woman Who Mapped the Ocean Floor by Hali Felt
Review of Soundings: The Story of the Remarkable Woman Who Mapped the Ocean Floor by Hali Felt

... used fossil and glacial deposits to postulate the prior existence of a large supercontinent (Pangea), which then proceeded to split into pieces over geological time. His theory of continental drift was extremely controversial and rejected by most geologists, primarily because he was not able to prov ...
The strange ecosystem of hydrothermal vents Nation Taiwan Ocean
The strange ecosystem of hydrothermal vents Nation Taiwan Ocean

... detergent industries. They act as catalysts to break down fats, wood etc, as well as DNA and operate in organic solvents. The most commonly used DNA polymerase in PCR (Polymerase Chain Reaction – a technique used to amplify and clone DNA) is Taq DNA polymerase, isolated from Thermus aquatics, a bact ...
Overview of the SACLANTCEN family of trawl
Overview of the SACLANTCEN family of trawl

... water activity. This has accelerated the technological evolution of Acoustic Doppler Current Profilers (ADCP) and has broadened the market. Long term (several months) deployments of ADCPs in heavily fished coastal waters are now relatively common. This paper describes the work conducted at SACLANT U ...
W H O I
W H O I

... typically live under the sea ice central in the food chain that links in winter, researchers must don dive suits and single-celled phytoplankton to the top predators. use small plankton nets to collect specimens for Marguerite Bay, off the Antarctic Peninsula can laboratory studies (right). contain ...
Zooplankton abundance and secondary production in the seas
Zooplankton abundance and secondary production in the seas

... characterised by low temperature and salinity. Occurrence of eggs and larvae of finfishes, pelagic tunicates, euphausiids, copepods, amphipods, foraminifers and lucifers in profusion accounted for the NE monsoon maximum. SW monsoon (June-September) was the least productive season. Monthly variations ...
Chapter 11 -2 Study Guide
Chapter 11 -2 Study Guide

...  This boundary is known as the Moho. Vocabulary - Moho = the boundary between the crust and the mantle.  The boundary is named for the scientist, Andrija Mohorovicic, who ...
6.19 The Oceanic CaCO3 Cycle - Earth and Environmental Sciences
6.19 The Oceanic CaCO3 Cycle - Earth and Environmental Sciences

... supersaturated with respect to calcite. Because of the pressure dependence of solubility, the extent of supersaturation decreases with depth until the saturation horizon is reached. Below this depth, the waters are undersaturated with respect to calcite. While it is tempting to conclude that the sat ...
Relating paleoclimate data and past temperature gradients: Some
Relating paleoclimate data and past temperature gradients: Some

... what has happened in the past, and is likely to happen in the future? Obviously the best approach would be to improve our techniques for determining what happened in the past, and, with the aid of such observations, improve our ability to model the past and future climates. As this general problem h ...
The Impact of Submesoscale Physics on Primary Productivity of
The Impact of Submesoscale Physics on Primary Productivity of

... through the remineralization of sinking organic matter or by advection from regions where they are more abundant, such as the continental margins. Regions of the oceans that receive plenty of sunlight exhibit nutrient-depleted or oligotrophic surface conditions. The subtropical gyres are examples of ...
Marine snow latitudinal distribution in the equatorial Pacific along 180°
Marine snow latitudinal distribution in the equatorial Pacific along 180°

... snow like particles (MS). Direct in situ measurements of the standing stocks of MS particles are difficult because of their fragile nature, but Alldredge [1998] has shown that particle mass is a function of size and that elemental compositions are similar regardless of origin, composition or season ...
The World`s Largest Marine Reserve, Chagos Archipelago
The World`s Largest Marine Reserve, Chagos Archipelago

... Dr Ronan Roche, Bangor University, UK Dr Elizabeth Widman, Warwick University, UK Anne Sheppard, University of Warwick Peter Carr, Zoological Society of London,UK David Curnick, University College of London Catherine Head, Oxford University, UK Gary Murphy University of Exeter, UK ...
3 Types of Metamorphism
3 Types of Metamorphism

... Plate tectonics • Continents collide (smash into each other) • Ocean crust subducts ...
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Ocean



An ocean (from Ancient Greek Ὠκεανός, transc. Okeanós, the sea of classical antiquity) is a body of saline water that composes much of a planet's hydrosphere. On Earth, an ocean is one of the major conventional divisions of the World Ocean, which covers almost 71% of its surface. These are, in descending order by area, the Pacific, Atlantic, Indian, Southern, and Arctic Oceans. The word sea is often used interchangeably with ""ocean"" in American English but, strictly speaking, a sea is a body of saline water (generally a division of the world ocean) partly or fully enclosed by land.Saline water covers approximately 72% of the planet's surface (~3.6×108 km2) and is customarily divided into several principal oceans and smaller seas, with the ocean covering approximately 71% of Earth's surface. The ocean contains 97% of Earth's water, and oceanographers have stated that only 5% of the World Ocean has been explored. The total volume is approximately 1.35 billion cubic kilometers (320 million cu mi) with an average depth of nearly 3,700 meters (12,100 ft).As it is the principal component of Earth's hydrosphere, the world ocean is integral to all known life, forms part of the carbon cycle, and influences climate and weather patterns. It is the habitat of 230,000 known species, although much of the oceans depths remain unexplored, and over two million marine species are estimated to exist. The origin of Earth's oceans remains unknown; oceans are thought to have formed in the Hadean period and may have been the impetus for the emergence of life.Extraterrestrial oceans may be composed of water or other elements and compounds. The only confirmed large stable bodies of extraterrestrial surface liquids are the lakes of Titan, although there is evidence for the existence of oceans elsewhere in the Solar System. Early in their geologic histories, Mars and Venus are theorized to have had large water oceans. The Mars ocean hypothesis suggests that nearly a third of the surface of Mars was once covered by water, and a runaway greenhouse effect may have boiled away the global ocean of Venus. Compounds such as salts and ammonia dissolved in water lower its freezing point, so that water might exist in large quantities in extraterrestrial environments as brine or convecting ice. Unconfirmed oceans are speculated beneath the surface of many dwarf planets and natural satellites; notably, the ocean of Europa is estimated to have over twice the water volume of Earth. The Solar System's giant planets are also thought to have liquid atmospheric layers of yet to be confirmed compositions. Oceans may also exist on exoplanets and exomoons, including surface oceans of liquid water within a circumstellar habitable zone. Ocean planets are a hypothetical type of planet with a surface completely covered with liquid.
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