Sentences with phrase «deep cold ocean waters»

There is also an increased upwelling of deep cold ocean waters and more intense uprising of surface air near South America, resulting in increasing numbers of drought occurrences, although fishermen reap benefits from the more nutrient - filled eastern Pacific waters.

Not exact matches

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.

Deep water is cold, dense water that sinks to the ocean depths.

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 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.

Today, cold water sinks near the Arctic and flows deep below the surface of the Atlantic toward the southern oceans, where it rises up.

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.

Just two decades ago, scientists discovered that colorful tropical reefs have ghostly counterparts in deep, cold waters throughout the world's oceans.

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.

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.

The resultant steam runs a turbine, and cold water drawn up from deep in the ocean condenses the steam to start the cycle again.

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.

Ocean Thermal Energy Conversion A technology using the temperature difference between cold, deep ocean waters and warmer surface waters to generate electriOcean Thermal Energy Conversion A technology using the temperature difference between cold, deep ocean waters and warmer surface waters to generate electriocean waters and warmer surface waters to generate electricity.

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.

Whether they are living in cold waters near the North Pole or around Antarctica or are visiting the deep ocean, these animals» blubber is vital to their survival.

One morning last August, the Monterey Bay Aquarium Research Institute's deep - sea robot, named Doc Ricketts, was snooping around the ocean floor in 1,812 meters of very cold water off the coast of northern California.

«Cold, deep water from this little area of the Nordic seas, less than 1 % of the global ocean, travels the entire planet and returns as warm surface water.

So the air was getting colder, but the deep ocean water was getting warmer, during the coldest periods of the Ice Age.

About 19 months after the wind churned the ocean, cycling warm deep waters upward and sending the cold surface waters down, the Totten ice shelf was noticeably thinner and had sped up.

Known as the Antarctic Bottom Waters (AABW), these deep, cold waters play a critical role in regulating circulation, temperature, and availability of oxygen and nutrients throughout the world's oceans.

Arrays monitor circulating currents in the Atlantic Ocean, in which warm shallow waters move north (red), while cold deep waters move south (blue).

The resulting EMUs include the deep, very cold, low - oxygen waters that encompass roughly one - quarter of the world's oceans.

The method consists of supplying bubbles of compressed air from a perforated pipe lowered in the water, which then rise, taking with them colder water from deeper in the ocean.

With the removal of the warm surface waters, an upwelling current is created in the east Pacific Ocean, bringing cold water up from deeper levels.

There is also a contribution of excess atmospheric CO2 absorption introduced to deep - water masses from dense, cold CO2 - rich surface waters at downwelling sites (e.g., North Atlantic), which then move through the oceans via meridional overturning circulation.

During normal conditions, trade winds blow to the west across the tropical Pacific Ocean, piling up warm surface water in the western Pacific, and cold, deeper water rises up, or upwells, off the west coast of South America.

Those winds allow an upwelling of deep, cold water off the northwest coast of South America to move west, piling up on the other side of the ocean.

CO2 is more soluble in colder than in warmer waters; therefore, changes in surface and deep ocean temperature have the potential to alter atmospheric CO2.

As we continue to learn more about the tenacious lifeforms found in deep, cold waters here on Earth, excitement grows over the possibility of Europa's oceans harboring extraterrestrial life.

Colder water can hold more carbon dioxide, however, the deep ocean is already an average of 4C and will freeze (salty or not) at around -1.8 C.

The phrase «deep, cold ocean - water fish» is a huge warning sign as we now know many of the deep water fish are slow to mature and very sensitive to over-fishing.

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Ray Ladbury wrote at 27 «However, there is also a huge reservoir of cold water in the deep oceans.

However, the ocean is very strongly stratified, and the interaction with the bulk of the deep cold water is very slow — it is generally the upper ocean that determines the time scale for the transient warming we might expect.

However, there is also a huge reservoir of cold water in the deep oceans.

Think of what would happen if you could pump cold deep water up to the surface, increasing the air / sea temperature gradient and warming the water; that would give you an anomalously large ocean heat uptake.

IF cool deep sea water were mixed relentlessly with surface water by some engineering method --(e.g. lots of wave operated pumps and 800m pipes) could that enouromous cool reservoir of water a) mitigate the thermal expansion of the oceans because of the differential in thermal expansion of cold and warm water, and b) cool the atmosphere enough to reduce the other wise expected effects of global warming?

I have to raise an objection to the phrase «the only region of the world that has defied global warming» — that might be neglecting a certain area in the Pacific where England 2014 has identified a very obvious point where the «Pacific conveyor» was bringing in the last decade up a lot of cold water from the deep ocean and has possibly played a major role in the specific trends for that period.

Even assuming that the dataset is comprehensive: Considering that the upper - ocean cooling is seen mainly at 30N and 30S, another explanation for this cooling is increased ocean — to — atmosphere heat transfer in these regions (possibly aided by hurricane - mixing of the upper ocean layer, and advection of deeper cold water as a result).

It's always worth remembering that the other end of the AMOC involves two main factors: (1) vorticity - mixing of heat from surface waters into the deep abyssal ocean (which decreases density causing the Atlantic Deep Water to start rising above the colder Antarctic Bottom Water) and (2) the wind - driven upwelling around the Antarctic Circumpolar Currdeep abyssal ocean (which decreases density causing the Atlantic Deep Water to start rising above the colder Antarctic Bottom Water) and (2) the wind - driven upwelling around the Antarctic Circumpolar CurrDeep Water to start rising above the colder Antarctic Bottom Water) and (2) the wind - driven upwelling around the Antarctic Circumpolar Current.

Consenquently, the associated SST pattern is slightly cooler in the deep convection upwelling regions of the Equitorial Pacific and the Indian Ocean, strongly cooler in the nearest deep convection source region of the South Atlantic near Africa and the Equator, warm over the bulk of the North Atlantic, strongly warmer where the gulf stream loses the largest portion of its heat near 50N 25W, and strongly cooler near 45N 45W, which turns out to be a back - eddy of the Gulf Stream with increased transport of cold water from the north whenever the Gulf Stream is running quickly.

Marine biological activity then transfers a bit more C to the deep ocean than cold, upwelling waters bring back up, such that the net sink to the deep ocean is about 1.6 GtC / yr, and much slower permanent removal in sediments.

They then looked at the challenges that warmer oceans delivered for crustaceans, molluscs, sponges, deep sea invertebrates, the warm and cold water corals that provide habitat for one - fourth of the ocean's variety, the pelagic or surface - swimming fish, and the demersal or deep - sea denizens that live longer, reproduce more slowly and are thus less likely to evolve and adapt to changing conditions.

The Atlantic overturning is driven by the differences in the density of the ocean water: when the warm, lighter water flows from south to north it becomes colder, denser and heavier, making it sink deeper and flow back southwards.

Ocean temperature change, however, reached a lower limit, probably because the freezing point of sea water put a restriction on how cold the deep ocean couldOcean temperature change, however, reached a lower limit, probably because the freezing point of sea water put a restriction on how cold the deep ocean couldocean could get.

While such a «missing heat» explanation for a lack of recent warming [i.e., Trenberth's argument that just can not find it yet] is theoretically possible, I find it rather unsatisfying basing an unwavering belief in eventual catastrophic global warming on a deep - ocean mechanism so weak we can't even measure it [i.e., the coldest deep ocean waters are actually warmer than they should be by thousandths of a degree]...

Now the researchers noticed that all of these flu pandemics started in the boreal spring or summer and were preceded by La Niñas — the phases in the El Niño Southern Oscillation (ENSO) that see large upwelling of cold deep ocean water in the East Pacific, which is then spread out across much of the ocean.

The resulting formation of Antarctic sea ice expelled colder, salty waters that filled the abyss and began cooling the deep oceans.

Between 2 and 3 million years ago the cooling of the deep oceans reached a tipping point, and modern upwelling regions ogf cold deep water off the coast of Peru, California and the west coast of Africa were established.

The aragonite, a crystal form of calcium carbonate, formed by tiny organisms then become too corroded to survive in high - pressure or cold waters including some parts of the shallow North Pacific, the southern ocean and the deepest waters of the ocean.