This means that they can have heat circulate
into deep ocean water, which has been observed to be the case.
Not exact matches
«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.
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.
It was the Antarctic ice, they argue, that cut off heat exchange at the
ocean's surface and forced it
into deep water.
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.
Geysers and
deep - sea vents are hydrothermal phenomena in which
water, heated and pressurized by molten rock, is released through vents at the land surface or
into the
oceans.
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.
Warm and saline
water transported poleward cools at the surface when it reaches high latitudes and becomes denser and subsequently sinks
into the
deep ocean.
When petroleum leaks from a ship or a
deep -
water drilling operation, «it tends to break up
into tiny droplets that don't all end up on the surface of the
ocean,» says Thomas Azwell, an environmental scientist at the University of California (UC), Berkeley, who was not involved in the work.
That means it sinks
into the
deeper layers of the
ocean, and the contrast between this warm
water and the undersea ice canyons contributes an unknown but substantial amount of sea level rise, said Josh Willis, an oceanographer at JPL in Pasadena, California.
The
deep waters of the modern Arctic flow into the North Atlantic via the Nordic seas, contributing up to 40 percent of the water that becomes North Atlantic Deep Water — known as the «ocean's lungs» for delivering oxygen and salt to the rest of world's oce
deep waters of the modern Arctic flow
into the North Atlantic via the Nordic seas, contributing up to 40 percent of the
water that becomes North Atlantic Deep Water — known as the «ocean's lungs» for delivering oxygen and salt to the rest of world's oc
water that becomes North Atlantic
Deep Water — known as the «ocean's lungs» for delivering oxygen and salt to the rest of world's oce
Deep Water — known as the «ocean's lungs» for delivering oxygen and salt to the rest of world's oc
Water — known as the «
ocean's lungs» for delivering oxygen and salt to the rest of world's
oceans.
Expanding sea ice would have melted
into the North Atlantic
Ocean, interfering with the normal mixing between surface and
deeper waters.
Once we reach
deep water, we stop driving and drop the submarine
into the
ocean.
Mysterious under - snow lakes pockmarking its edges and
deep layers of ice at higher elevations both point to changes that could hasten melt and send
water cascading
into the
ocean, pushing global sea levels ever higher.
In addition, seamounts rising
into the
ocean create obstacles that shape
ocean currents and direct
deep, nutrient - rich
waters up the sloping sides of seamounts to the surface.
And while you can jump
into the
deep end of the
ocean and start swimming, it's my goal to empower you to spend minimal time just treading
water.
Unexpectedly, Norman ran
into the
ocean and started swimming straight
into deep water.
Travis explained to us how each time he first goes
into the
water for a surfing session, as he gets out
into the white wash he lies face down floating in the
water between waves and gives
deep thanks to Mother
Ocean.
Monterey Bay's five beautiful sandy beaches are sheltered by rugged, tree studded cliffs that drop
into the
deep azure
waters of the Pacific
Ocean.
A 12 ′ depth allows students to practice
deep water entries and equalization before moving out
into the
ocean.
Waves at low tide are said to be quick, steep or dumpy, this is because there is very little
water sitting over the sand bank or reef allowing the
ocean swells to travel from very
deep water straight
into very shallow
water.
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Furthermore, changes in runoff routing through the Arctic
Ocean can regulate the extent to which Arctic tDOM is incorporated into North Atlantic Deep Water (NADW) and distributed in the global o
Ocean can regulate the extent to which Arctic tDOM is incorporated
into North Atlantic
Deep Water (NADW) and distributed in the global
oceanocean.
That altered
ocean currents, strengthening the subtropical sea
water circulation thus providing a mechanism to transport heat
into the
deeper ocean.
The standard assumption has been that, while heat is transferred rapidly
into a relatively thin, well - mixed surface layer of the
ocean (averaging about 70 m in depth), the transfer
into the
deeper waters is so slow that the atmospheric temperature reaches effective equilibrium with the mixed layer in a decade or so.
They suggested that the transient changes in El Nino (before the
deeper water tapped by upwelling has warmed) may be different from the state of El Nino after the
ocean has come
into equilibrium.
«As a result,
ocean waters deeper than 500 meters (about 1,600 feet) have a large but still unrealized absorption capacity... As emissions slow in the future, the
oceans will continue to absorb excess CO2...
into ever -
deeper layers... eventually, 50 to 80 percent of CO2 cumulative emissions will likely reside in the
oceans»
Presumably, it does take a lot of energy to move that much
water faster, with the heat potentially being redistributed
into deeper ocean layers associated with perhaps poorly understood fluctuations of the Antarctic convergence at depth?
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 Curr
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 Curr
Deep Water to start rising above the colder Antarctic Bottom
Water) and (2) the wind - driven upwelling around the Antarctic Circumpolar Current.
The
deep waters formed by this process then flow
into the world
ocean, purging the North Atlantic of part of its excess salt.
eadler2 January 10, 2015 at 5:54 pm ... When
ocean surface temperatures cool, due to a La Nina, the warmer surface
water is mixed
deeper into the
ocean and cooler
ocean water flows along the surface of the Pacific.
When
ocean surface temperatures cool, due to a La Nina, the warmer surface
water is mixed
deeper into the
ocean and cooler
ocean water flows along the surface of the Pacific.
Due to the predominance of La Nina's in the last 15 years, the warmer surface
water has been mixed
into the
deeper ocean.
This discourages surface
water from sinking downwards
into the
deep ocean.
But mapping with ice - penetrating radar has revealed a low - lying region cut by glacially carved channels that drop as far as 8,500 feet below sea level — perfect for guiding warm
ocean water deep into the heart of the ice sheet.
Without cooled
water plunging
into the
deep ocean near Greenland, and turning back south, the entire conveyor belt will stop.
In contrast to La Nina induced shallow - aquifer effects,
deep aquifers have been filled with meltwater from the last Ice Age, and that
water is slowly and steadily seeping back
into the
oceans today.
The main mechanism for wind - driven mixing
into the
deep ocean (down to around 2000 metres) is via convergence of warm tropical surface
water in the subtropical
ocean gyres.
With the Earth known as the «
water planet» because of over 70 % of the globe covered by
deep oceans, warmer temps directly result in more evaporation of the
ocean water into the air - clouds.
Most of the
deep ocean warming is occurring in the subtropical
ocean gyres - vast rotating masses of
water in each
ocean basin where near - surface currents converge and are forced downward
into the
ocean interior.
The Revelle Effect (RE) to me appears to be based on the unproven assumption that the surface
ocean waters (SOW) can be regarded separately from the
deep oceans when taking
into consideration the partitioning ratio for PCO2atm and pCO2aqueous because of the apparently long - time it takes for free CO2 to diffuse to the bottom of the
oceans.
In addition, there are a completely unknown number of thermal vents directly warming the bottoms of the
oceans, and some lakes, emitting a completely unknown amount of heat
into the
deep water.
Joe Postma is also wrong in assuming solar radiation can heat the Earth's surface to that extent, especially when 70 % of the surface is a thin (say 1 centimetre
deep) surface layer of
water which transmits most of the radiation down
into the
ocean thermoclines.
Icelandic scientists say they have discovered a new overturning site, where cold, dense,
deep water is formed and transported through a separate route towards the Denmark Strait and further south
into the Atlantic
Ocean.
Winds and storms pushing
into lower latitudes spin up the gyres pushing cold polar
water into the Californian and Peruvian currents facilitating
deep ocean upwelling.
The «strong trade winds,» says study co-author Gerald Meehl of the U.S. National Center for Atmospheric Research, «are bringing cooler
water to the surface in the equatorial Pacific and mixing more heat
into the
deeper ocean.»
Another factor is convection currents in
water allow heat to move
into the depths and
oceans are very
deep.
The warming reached a depth of about 10,000 feet (4,000 meters), interfering with the normal circulation process in which colder surface
water descends, taking oxygen and nutrients
deep into the
ocean.
Climate change can influence the distribution of dead zones by increasing
water temperature and hence microbial activity, as well as reducing mixing of the
ocean (i.e., increasing layering or stratification) of the Ocean — which have different temperatures, densities, salinities — and reducing mixing of oxygen - rich surface layers into the deeper parts of the O
ocean (i.e., increasing layering or stratification) of the
Ocean — which have different temperatures, densities, salinities — and reducing mixing of oxygen - rich surface layers into the deeper parts of the O
Ocean — which have different temperatures, densities, salinities — and reducing mixing of oxygen - rich surface layers
into the
deeper parts of the
OceanOcean.
The
deep waters, being warmer than such surface
waters, rise to the surface, as the upper layers sink slowly
into the dark
ocean depths.