Injecting the same meltwater further down is believed to have the opposite effect, favoring
sinking of surface waters and the retreat of Antarctic sea ice.
This is thought to slow down
the sinking of surface water, and to favor the expansion of Antarctic sea ice.
Not exact matches
I took the dough out
of the bowl and flattened it on a floured
surface, kneading it lightly to get the air out, and repeated the rising process; placed the dough in the bowl, covered, filled
sink with warm
water, and placed the bowl in
sink.
Once they are dispersed, the tiny droplets
of oil are more likely to
sink or remain suspended in deep
water rather than floating to the
surface and collecting in a continuous slick.
Ocean
water sops up the red so effectively that 100 feet below the sea
surface only the bluish components
of sunlight penetrate; a
sunken ship's crimson lower keel appears black to divers since nothing can look red in the absence
of red light.
Today, cold
water sinks near the Arctic and flows deep below the
surface of the Atlantic toward the southern oceans, where it rises up.
«The primary producers, the phytoplankton, take carbon dioxide out
of the
surface waters and «fix» it into a form
of carbon that can
sink down to the deep where it is stored,» Gibson says.
When sea ice forms, it expels salt into the surrounding
water, increasing the density
of the
water and causing it to
sink, carrying oxygenated
surface water into the depths.
After they die, their detritus slowly
sinks from the
surface to the sea floor, and there is a layer in the
water column, the OMZ, where microbes consume much
of the detritus, a process that depletes oxygen through bacterial respiration.
Their main source
of food is «marine snow» — a slow drift
of mucus, fecal pellets, and body parts — that
sinks down from the
surface waters.
When they
sink to the seafloor at the end
of their life cycles, they take the carbon from the
surface waters with them, provide it as food to organisms at the bottom or store it in deep
water layers after decomposition.
I've been experimenting with T10 dextran coated iron oxide nanoparticles, obviously not the same as fullerenes, but still a very interesting tool, I've been testing if the coating is giving the particle antioxidant abilities because
of it's the (basically) indigestable sugar chains (glucose) creating a high
surface area which are largely made from hydroxyl groups, I hypothesised this act's as a «
sink» for reactive oxygen species converting them to
water.
In addition, reductions in calcification from lowered pH in
surface waters could reduce phytoplankton
sinking rates through loss
of ballast (Hofmann and Schellnhuber, 2009), though this effect will depend on the ratio
of the fraction
of ballasted vs. un-ballasted fractions
of the
sinking POC.
The combination
of the
water's temperature and salinity determines whether it rises to the
surface,
sinks to the bottom, or stays at some intermediate depth.
Imagine this place being like a pool
of warm
water, and allow your attention to flow back from the
surface of your forehead, toward the center
of your skull — as though
sinking from the
surface of a pool
of water to its depths.
When you have everything in its place bring the entire container over to the
sink and give it a good drink
of water — consider whether your vessel has drainage holes and if you need to protect the table
surface as well as how much
water the bulbs will rest in.
Also if you're in deep
water, you really want to get out before you
sink to the bottom, or getting out
of the car won't help, as you won't be able to make it to the
surface in time.
For a scene in the movie, based on the popular book
of the same name, a frightened German shepherd was forced into a churning pool
of water and, at one point,
sunk beneath the
surface.
Fleas
sink and drown instead
of remaining on the
water's
surface.
There is a basilisk lizard, Basiliscus vittatus, locally called «cock malalla» or» tul - luk» in Maya, that has the ability to run across the
surface of the
water without
sinking.
Coral reefs can grow anywhere there is a hard foundation like limestone sea floors or
sunken ships that are close enough to the
surface of the
water to allow access to sunlight.
While on your tour you will experience beautiful coral formations, old
sunken ship hulls where schools
of Local Hawaiian typical fish live amongst the wreckage.On the
surface during your tour you may get to see whales breaching and playing with their young during our winter months in the beautiful blue Hawaiian
waters, while Dolphins can be seen at times surfing next to the Queen as She motors along Oahu's coastline.
Use your feet to
sink the tail
of the board, you and your board should be underneath the
surface of the
water now so don't forget to take a deep breath!
Speaking
of which, there's a really informative tutorial mode for new comers to
sink there teeth into, heading in to the DiRT Academy menu you can head in to a free roam session with lessons being accessible from the pause menu, here you can learn everything from basic and advanced techniques, to learning how to drive over different
surface conditions and how to handle track features like jumps and
water splashes, with plenty in between.
In many cases, his acrylic artworks will rise out
of water on the
surface of hard - to - reach rusting
sunken ships or forgotten concrete posts
of bridges.
For Vauxhall 2003 Hiorns
sunk a gully into the
surface of the Sculpture Court at Tate Britain but, instead
of water running down through the grating, a flame rises up from it.
The large works that have occupied him since 1969 are, in brief: Hubris, commissioned for the University
of Hawaii at Manoa, one
of Smith's most open and regular pieces to date, which consists
of a two - section, 9 - by - 9 grid in black concrete, one half thin slabs at ground level, the other half the same grid raised to 3 feet 3 inches by a four - sided pyramidal module; Batcave, a complex environmental interior designed to «mold space and light» rather than material form, at the Osaka World's Fair, a new version
of which will be shown soon at the Los Angeles County Museum; a gigantic triangular sculpture inserted into a Californian mountainside; a labyrinthine
water garden for a delta; Smog, a huge new horizontal piece made from the dismantled components
of Smoke (which was made for the Corcoran's «Scale as Content» show, 1967); Haole Center, a
sunken square «pavement» within a square stone sculpture, with a metal ladder leading down below the earth's
surface; two related monumental sculptures on platforms (Arch and Dial); and a flat 81 - block grid proposed for downtown Minneapolis.
In general, the regions
of expanding warming upwelling
water in the Indian Ocean, North Pacific, or wherever they are, must create slight bulges in the
surface, and the regions
of shrinking, cooling,
sinking water in the Arctic must create slight depressions in the sea
surface (again, I mean in a very low pass sense — obviously storms, tides, etc, create all kinds
of short - terms signals obscuring this).
The significant difference between the observed decrease
of the CO2
sink estimated by the inversion (0.03 PgC / y per decade) and the expected increase due solely to rising atmospheric CO2 -LRB--0.05 PgC / y per decade) indicates that there has been a relative weakening
of the Southern Ocean CO2
sink (0.08 PgC / y per decade) due to changes in other atmospheric forcing (winds,
surface air temperature, and
water fluxes).
Ground source heat pumps, which were mentioned by Senator Inhofe, essentially use
water circulated through pipes
sunk into the ground to use the relatively stable temperature
of the earth just below the
surface to provide warmth in the winter and cooling in the summer.
Theory and modelling suggest that if the
sinking of the salty
surface waters in the North Atlantic slowed down or stopped, there would be a reduction in the heat transport by the ocean, which would have implications for the climate
of northern Europe.
The idea
of the void being a
sink - hole faces the problems
of its formation through permafrost, and
of the lack
of any
surface water penetration
of the solid gas - tight cap — which rather knock this hypothesis.
We use some
of the power to spread the cold
water over the
surface so that it does not
sink below the layer where phytoplankton convert dissolved CO2 into organic matter that increases the mass
of their bodies to feed other ocean creatures.
I suspect the amount
of additional 33psu
surface waters entrained by the
sinking brine is indicated by the nearly 35psu salinity
of Arctic ocean
water below about 300 meters depth; if the salt from each cubic meter
of ice formed were added to approximately 15 cubic meters
of water at 33psu, it would raise the salinity to near 35psu.
Many
of the
surface currents
of the world oceans (i.e., the ocean «gyres» which appear as rotating horizontal current systems in the upper ocean) are driven by the wind, however, the
sinking in the Arctic is related to the buoyancy forcing (effects that change either the temperature or salinity
of the
water, and hence its buoyancy).
The
sinking is mainly driven by the saltiness
of the
water, which is affected by evaporation
of fresh
water from the
surface or, particularly in the Arctic, freezing seawater which leaves salt behind in the
water beneath the ice.
It's possible that terrestrial
sinks could continue to sop up and sequester some anthropogenic carbon, but there's an owful lot
of near -
surface carbon and if that get's oxidized at some point in the future, then we could be in even hotter
water.
Only in certain regions, notably in the Antarctic and northwest Atlantic Oceans, does a combination
of evaporation (which increases the
water's salt content) and wintertime cooling make
surface water dense enough to
sink all the way down.
Based on evidence from Earth's history, we suggest here that the relevant form
of climate sensitivity in the Anthropocene (e.g. from which to base future greenhouse gas (GHG) stabilization targets) is the Earth system sensitivity including fast feedbacks from changes in
water vapour, natural aerosols, clouds and sea ice, slower
surface albedo feedbacks from changes in continental ice sheets and vegetation, and climate — GHG feedbacks from changes in natural (land and ocean) carbon
sinks.
Cold
water in clouds is the nearest
sink that absorbs the CO2 that is outgassed from the
surface of the ocean.
If it does
sink through the mass
of water, then that CO2 in the air should just drop like a stone to the
surface of the Planet.
4) By interpreting the analyss
of Bob Tisdale, the global sea
surface temperatures used by Endersbee in his calculations have been controlled by warming
of the sea
surface waters outside the tropical sea
surface i.e. mainly by the warming
of the sea
surface waters of higher latitudes where the sea
surface CO2
sinks are.
The Atlantic Meridional Overturning Circulation (AMOC)- the transport
of warm tropical
surface water northward - is indeed propelled by dense
water sinking in the North Atlantic and travelling equatorward in the deeper layers, but it also has a wind - driven component to it.
5) As a consequence, the partial pressure
of CO2 has been rising in these as
sinks acting
surface waters, which has been making CO2 absorption from the atmosphere to the sea
surface sinks become slower.
New Dutch research has shown for instance the overturning has been relatively weak in recent years [which means cold
water has accumulated close to the
surface instead
of sinking to deeper
waters, one
of two reasons why there has been a lull in upper ocean warming].
AGW climate scientists seem to ignore that while the earth's
surface may be warming, our atmosphere above 10,000 ft. above MSL is a refrigerator that can take
water vapor scavenged from the vast oceans on earth (which are also a formidable heat
sink), lift it to cold zones in the atmosphere by convective physical processes, chill it (removing vast amounts
of heat from the atmosphere) or freeze it, (removing even more vast amounts
of heat from the atmosphere) drop it on land and oceans as rain, sleet or snow, moisturizing and cooling the soil, cooling the oceans and building polar ice caps and even more importantly, increasing the albedo
of the earth, with a critical negative feedback determining how much
of the sun's energy is reflected back into space, changing the moment
of inertia
of the earth by removing
water mass from equatorial latitudes and transporting this
water vapor mass to the poles, reducing the earth's spin axis moment
of inertia and speeding up its spin rate, etc..
Concerning decadal changing trends
of CO2 content in atmosphere I have expressed that they are caused by changing temperatures
of sea
surface water on the seasurface areas where seasurface CO2
sinks are.
For more than a decade, researchers have struggled and failed to balance global carbon budgets, which must balance carbon emissions to the atmosphere from fossil fuels (6.3 Pg per year; numbers here from Skee Houghton at Woods Hole Research Center) and land use change (2.2 Pg; deforestation, agriculture etc.) with carbon dioxide accumulation in the atmosphere (3.2 Pg) and the carbon
sinks taking carbon out
of the atmosphere, especially carbon dioxide dissolving in Ocean
surface waters (2.4 Pg).
Because only very cold
surface water is able to
sink, it is simple to understand that the deep ocean can never warm up, regardless
of how warm the
surface ocean around the world may become.
So, the saltier and more dense Atlantic
water sinks below the
surface and a colder fresher layer
of water above it acts as a insolation blanket that limits the amount
of ocean heat in contact with the ice above.