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583 RADIOCARBON IN THE WATER COLUMN OF THE
583 RADIOCARBON IN THE WATER COLUMN OF THE

... On the other hand, at Stations 1 and 2, the ∆14C values are lower (by up to 50‰) in the layer above 1500 m. At these stations, the differences between our and GEOSECS observations are found in vertical salinity profiles as well, and this may be caused by the influence of the saline Kuroshio Extensio ...
Appendix D: Plankton
Appendix D: Plankton

... INTRODUCTION...........................................................................................................................1 ...
1 ` ENSO Jigsaw [Key Science Knowledge Module] 1 Activity
1 ` ENSO Jigsaw [Key Science Knowledge Module] 1 Activity

... Pacific Ocean. Air rises over this warm pool. Rising air leaves the lower atmosphere and airflows in to fill the gap. The air filling the gap causes the winds to blow towards the warm water. The winds blowing in to fill the gap are the trade winds. The warm pool of water releases large amounts of he ...
Vailulu’u Seamount, Samoa: Life and death on an active submarine volcano
Vailulu’u Seamount, Samoa: Life and death on an active submarine volcano

... depth (CTD) profiles in the crater yielded relatively constant gradients in potential density and temperature (Fig. 2; ref. 12) with significant density and temperature inversions only in the immediate vicinity of the NMHC (Fig. 1). This result shows overall that a stable density structure in the cr ...
Ocean and Coastal Acidification off New England and Nova Scotia
Ocean and Coastal Acidification off New England and Nova Scotia

... the Northeast Coastal Acidification Network (NECAN) study area where ocean acidification will be more readily discernible than could be the case for the complex nearshore environments. The rate of ocean acidification of these waters is similar to the rate of atmospheric CO2 increase further modified ...
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... The aim of this conference is to bring together early career scientists to present and discuss their research in an engaged, multidisciplinary environment and offer opportunities to discover potential synergies between wide-ranging topics, thereby fostering interdisciplinary research. Sessions are t ...
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Seamounts Project
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... Revised: 12 February 2014 – Accepted: 13 February 2014 – Published: 29 April 2014 ...
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Synchronicity of Kuroshio Current and climate system variability

... The Kuroshio Current (KC) is the northward branch of the North Pacific subtropical gyre (NPG) and exerts influence on the exchange of physical, chemical, and biological properties of downstream regions in the Pacific Ocean. Resolving long-term changes in the flow of the KC water masses is, therefore, cr ...
Regional anomalies of sediment thickness, basement depth and
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... of water depths from Smith and Sandwell[2] to determine adjusted basement depth. We next corrected for expected variations in unloaded basement depth predicted by a model of conductive cooling of the underlying lithosphere as a function of its age, again assuming local isostasy. We first produced a ...
SOL 5.3(AE) - Staunton City Schools
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... travel only where there is matter to transmit them. ...
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... • For its scientific users, MERCATOR is an operational ocean observatory: by systematically combining, over several years, all the information yielded from observations (measurements reflecting reality) with that provided by the model (a threedimensional view and a memory of past states), it can pro ...
magnitude - Ministry of Earth Sciences
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... services for neighbouring countries, Seychelles and Sri Lanka was inaugurated on 10th July 2015 by the Union Minister for Earth Sciences, Dr. Harsh Vardhan in New Delhi. The potential fishing zone (PFZ) advisories and specific advisories (Tuna) to fishermen were also continued. An atlas of the PFZ ...
F-FOFM Report
F-FOFM Report

... from the 2,500 m isobaths. The implementation of the above rules or other rules implies knowledge of marine geomorphology and geology of the margin.  Outer boundary - 200 m depth because tides are not obligatory applied beyond this depth. ...
3. Anatomy of recently active convergent plate - diss.fu
3. Anatomy of recently active convergent plate - diss.fu

... Compaction and phase transitions within both sediments and the subducting slab lead to dewatering and dehydration, providing fluids to the plate interface system. This water release increases the pore pressure, and therefore reduces effective stress and effective friction. This in turn increases the ...
INFORMATION DOCUMENT
INFORMATION DOCUMENT

... projections for many areas of the world with an initial focus on Africa. A team of regional scientists evaluate the strengths and limitations of the regional climate model results that will be used for a range of climate adaptation and risk management practices. WCRP regional activities also cover t ...
Survival and settling of larval Macoma balthica in
Survival and settling of larval Macoma balthica in

... (OA), which includes changes in the inorganic carbon balance of the seawater coupled with a decrease in pH, is occurring at a rate faster than experienced in the geological past (Hönisch et al., 2012), and is expected to pose a major threat to marine ecosystems worldwide (Orr et al., 2005; Fabry et ...
link to answer key. - Warren County Schools
link to answer key. - Warren County Schools

... These are the 5 main layers in order from the surface to the center of the Earth. [4 pts.] inner core, outer core, mesosphere, asthenosphere, lithosphere mesosphere, asthenosphere, lithosphere, inner core, outer core lithosphere, asthenosphere, mesosphere, outer core, inner core asthenosphere, litho ...
Constraints on shallow mantle viscosity from morphology and
Constraints on shallow mantle viscosity from morphology and

... Ribe, 1988], then an axial high could not form at a fast‐ spreading center. Braun et al. [2000] also concluded that the sub‐ridge viscosity must be low based on thermo‐mechanical models for mid‐ocean ridges with melting effects considered. They suggested that a viscosity as low as 1018 Pa·s is requi ...
Thermal models of the Mexico subduction zone
Thermal models of the Mexico subduction zone

... affect sediment properties, including pore fluid pressure and physical and chemical changes in the sediments [e.g., Moore and Saffer, 2001]. One change that may be important is the dehydration of smectite clays to illite and chlorite at temperatures between 100 and 150C [Wang, 1980]. Whether this c ...
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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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