Sentences with phrase «of deep ocean water»

The many benefits of ocean thermal energy conversion (OTEC) include: small seasonal and daily variations in availability, benign environmental performance and by - products in a family of deep ocean water applications, for example food (aquaculture and agriculture) and potable water, and improving economics as a result of higher oil prices.
The federal government is about to open up to wind energy development vast swaths of deep ocean waters, and states and wind park developers are vying to be the first to seize the new frontier.
There is a long «tail» of the response (> 1000 years) due to the slow mixing of deep ocean waters which makes it dificult to give just one number.
Remote vehicles can measure the temperature of deep ocean waters, and periodically surface to transfer the information to satellites.
It may have its origin with the 800 year overturning of deep ocean waters from the polar sink places to the equatortial upwelling places.

Not exact matches

Blessed with warm sunny weather all year round (roughly 300 days of sunshine a year), ringed by the Atlantic Ocean on one side and protected on the other by the calm, deep - blue waters of the Tagus River (the longest river in the Iberian Peninsula), this traditionally sophisticated city seems to have it all.
«Son of man, bathe yourself in the ocean of matter; plunge into it where it is deepest and most violent; struggle in its currents and drink of its waters.
Our fish meal is from deep ocean water small fish, and our crab meal comes from the cold waters of the Pacific Northwest or Nova Scotia.
Kona Deep Water Purified Ocean Water from the waters of Hawaii, containing naturally occurring deep ocean electrolDeep Water Purified Ocean Water from the waters of Hawaii, containing naturally occurring deep ocean electroOcean Water from the waters of Hawaii, containing naturally occurring deep ocean electroldeep ocean electroocean electrolytes
The hotel's arrival will launch the transformation of the former shrimp boatyard and fishing village into a chic and contemporary destination, offering the largest deep water marina in the Florida Keys, direct ocean access, and an emerging retail and restaurant district.
A new map of the surrounding seafloor helps explain why: Many of the fastest - melting glaciers sit atop deep fjords that allow Atlantic Ocean water to melt them from below.
Depth may not be as much of an issue for you if you tend to fish in shallow waters, but if you fish in the ocean or deep lakes and rivers, having a maximum depth of 100 meters or more can be crucial to finding your next big catch.
A new study in Marine Biology Research tackles this issue by comparing the physical characteristics of two similar octopus species that live on the ocean floor, as deep as 9,500 feet (almost 2,900 m) below the water's surface.
The shrimp represent centimeter - sized swimmers, including krill and shrimplike copepods, found throughout the world's oceans that may together be capable of mixing ocean layers — and delivering nutrient - rich deep waters to phytoplankton, or microscopic marine plants, near the surface, the researchers suggest.
They found glacial fjords hundreds of meters deeper than previously estimated; the full extent of the marine - based portions of the glaciers; deep troughs enabling Atlantic Ocean water to reach the glacier fronts and melt them from below; and few shallow sills that limit contact with this warmer water.
This heating ought to be weak, but some unknown process seems to be amplifying it, possibly enough to melt a deep ocean of liquid water on Enceladus, or maybe only enough to form smaller pools of water within the moon's icy shell.
They identified wind patterns that mixed the warmer surface and colder deep waters to cool the ocean's surface and reduce the intensity of the storm.
«The undersides of glaciers in deeper valleys are exposed to warm, salty Atlantic water, while the others are perched on sills, protected from direct exposure to warmer ocean water,» said Romain Millan, lead author of the study, available online in the American Geophysical Union journal Geophysical Research Letters.
Researchers can measure annual changes in how the melt rate occurs, for example, or the effects of a single pulse of warm deep - ocean water.
Ryskin proposes that huge deposits of methane and other gases, which are naturally produced in deep - sea waters, became trapped under the pressure of a then - stagnant global ocean.
The fourth - largest moon of Jupiter may have a global ocean roughly 50 miles deep, but all that water lies below an intimidating ice shell up to 12 miles thick.
This water is warming an average of 0.03 degrees Celsius per year, with temperatures at the deepest ocean sensors sometimes exceeding 0.3 degrees Celsius or 33 degrees Fahrenheit, Muenchow said.
Driven by stronger winds resulting from climate change, ocean waters in the Southern Ocean are mixing more powerfully, so that relatively warm deep water rises to the surface and eats away at the underside of theocean waters in the Southern Ocean are mixing more powerfully, so that relatively warm deep water rises to the surface and eats away at the underside of theOcean are mixing more powerfully, so that relatively warm deep water rises to the surface and eats away at the underside of the ice.
The rising temperatures cause layers of ocean water to stratify so the more oxygen - rich surface waters are less able to mix with oxygen - poor waters from the deeper ocean.
A mass of water called the North Atlantic Deep Water enters the Southern Ocean off the southeast coast of South America (star in map below lwater called the North Atlantic Deep Water enters the Southern Ocean off the southeast coast of South America (star in map below lWater enters the Southern Ocean off the southeast coast of South America (star in map below left).
In a recent paper published in Nature Geoscience, his team identified two deep underwater cavities beneath the glacier that they note could be pathways for relatively warm ocean water to reach the underside of the glacier, enhancing its melting.
The fog is a gift of the Pacific Ocean's California Current where winds create upwellings that bring cold, deep, nutrient - rich waters to the surface.
A plague of oxygen - deprived waters from the deep ocean is creeping up over the continental shelves off the Pacific Northwest and forcing marine species there to relocate or die.
At high velocities deep in the ocean, that dual pressure heaves water with forces powerful enough to generate a tsunami, as a similarly massive chunk of seafloor did in the 2011 event in Japan.
Unexplored deep waters in the Atlantic Ocean could offer a preview of life — if it exists — on other moons and planets.
Once a year, they migrate from the deep ocean to shallow water along the Pacific Coast of North America.
And C. finmarchicus is far from being the only animal in the ocean which spends part of its life cycle in deep water.
Today, cold water sinks near the Arctic and flows deep below the surface of the Atlantic toward the southern oceans, where it rises up.
But the balance between DVMs and the limited deep - water oxygen supply could be easily upset, Bianchi said — particularly by climate change, which is predicted to further decrease levels of oxygen in the ocean.
Research begun at Princeton University found that the numerous small sea animals that migrate from the surface to deeper water every day consume vast amounts of what little oxygen is available in the ocean's aptly named «oxygen minimum zone» daily.
Beatty believes that when 570 degree Fahrenheit water from thermal vents hits cold, deep ocean currents, several light - producing processes may occur: sonoluminescence from imploding gas bubbles; chemiluminescence from chemical reactions (analogous to fireflies lighting up); crystalloluminescence from the formation of crystal bonds; and triboluminescence from the breaking of those bonds.
«Nobody had done rapid - response drilling in the ocean, nobody had drilled anything substantial under 7 kilometers of water, nobody had placed an observatory in a fault that deep, and nobody had retrieved a string of instruments from that deep,» she said.
The oxygen content of the ocean may be subject to frequent ups and downs in a very literal sense — that is, in the form of the numerous sea creatures that dine near the surface at night then submerge into the safety of deeper, darker waters at daybreak.
«We need to do more studies to be able to determine if this new species, which we are yet to name, only lives in the shallow waters of the western Mediterranean or if it is also found in other deep water basins in the eastern Mediterranean or Atlantic Ocean, for example,» highlights Conxita Àvila.
«These results show that the effect of ocean acidification on deep - water corals may not be as severe as predicted,» said David Garrison, a program director in the National Science Foundation's Division of Ocean Sciences, which funded the reseocean acidification on deep - water corals may not be as severe as predicted,» said David Garrison, a program director in the National Science Foundation's Division of Ocean Sciences, which funded the reseOcean Sciences, which funded the research.
A fleet of robotic submarines, based at the National Oceanography Centre (NOC), head - quartered in in Southampton, have been used to map vulnerable cold - water coral reefs in the deep ocean off southwest England.
Real - world data back the claim: Accumulations of calcium carbonate in deep - sea Pacific sediments show that the Pliocene ocean experienced huge shifts at the time, with waters churning all the way from the surface down to about three kilometers deep, as would be expected from a conveyor belt — type circulation.
This enabled the research team to reconstruct, for the first time, a detailed picture of the environmental conditions at the ocean's surface, as well as in deeper water layers, over the last 30,000 years.
The region is getting stormier, which threatens settlements, aids ocean mixing that funnels nutrients to deeper waters, and could speed the breakup of sea ice.
They compared isotope measurements on the silica skeletons of diatoms, which store environmental signals from the ocean's surface, with isotope signals from radiolarians, which live in deeper water layers.
At the edge of the Pacific continental shelf, deeper, nutrient - rich waters rise to the ocean's surface.
El Nino's mass of warm water puts a lid on the normal currents of cold, deep water that typically rise to the surface along the equator and off the coast of Chile and Peru, said Stephanie Uz, ocean scientist at Goddard Space Flight Center in Greenbelt, Maryland.
When that edge moves off the continental shelf into deep open ocean waters, the productivity drops off and the marine organisms that feed larger wildlife are out of reach, scientists say.
Even as the surface warms, the deeps remain cool, and this cold water will continue to periodically push the ocean out of the El Niño state.
The researchers found that during glacial periods when the atmosphere was colder and sea ice was far more extensive, deep ocean waters came to the surface much further north of the Antarctic continent than they do today.
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