I didn't keep the links but there is at least one d18O study from the Pacific Warm Pool which clearly indicates that first the deep ocean warmed there, followed later by the CO2 increase and then
the shallow ocean warmed, leading to the LGM to Holocene transition.
The rate of
shallow ocean warming can decrease at the same time the rate of deep ocean warming increases.
Not exact matches
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.
The report found some deep mesophotic coral ecosystems may be less vulnerable to the most extreme
ocean warming, but others may be just as vulnerable as their
shallow counterparts and can not be relied on to act as «life boats.»
In North America, a
warm,
shallow sea called the Western Interior Seaway extended from the Arctic
Ocean to the Gulf of Mexico, subdividing the continent into eastern and western landmasses, known as Appalachia and Laramidia, respectively.
The long - term geological record reveals an early Cenozoic
warm climate that supported smaller polar ecosystems, few coral - algal reefs, expanded
shallow - water platforms, longer food chains with less energy for top predators, and a less oxygenated
ocean than today.
Faster flow is more turbulent, and in this turbulence more heat is mixed into AABW from
shallower,
warmer ocean layers — thus
warming the abyssal waters on their way to the Equator, affecting global climate change.
In some parts of the Arctic
Ocean, the
shallow regions near continents may be one of the settings where methane hydrates are breaking down now due to
warming processes over the past 15,000 years.
These European reptiles inhabited
warm,
shallow seas of the continent, but «they were not as agile in this environment as today's sea turtles, who are able to cover very large distances and cross seas and even
oceans,» the expert explains.
Arrays monitor circulating currents in the Atlantic
Ocean, in which
warm shallow waters move north (red), while cold deep waters move south (blue).
Corals are found in all of Earth's
oceans, from tropical to freezing temperatures, however they only build coral reefs in
warm,
shallow seas in the tropics.
Ocean warming, which is caused by climate change, is a serious threat to coral reefs, especially for coral reefs in
shallower waters.
They created a model to determine how temperatures of
ocean waters could change
shallow reef systems when sea levels rise and climate
warms in the future.
These great winged creatures glide majestically in the
warm shallows of the surrounding
ocean, much to the delight of the divers and snorkelers that frequently explore the coral reefs that line the coast.
Turtles swim in the
shallow water, and in the winter season humpback whales frolic in the
warm ocean close to shore.
This can happen if something increases the amount of mixing between the (
warm)
shallow ocean and the (cold) deep
ocean.
But seen the environmental global CRISIS of GLOBAL
WARMING and its devastating climatological impact, I would recommend as an environmental policy - expert that Both NATURAL plankton will be bred in
shallow waters as carbondioxide inhibitors in a large volume on the one hand and let nature goes its course in the seas and
oceans so that sea - organisms / life - forms / mamals will not become extinct due to (for them) food poisoning.
Ocean waters around Antarctica have
warmed steadily for the past 50 years, but in addition to that, the region's
shallow seas are also heating up, more quickly than others.
Under the new slab -
ocean approach, the LHF increase is weaker under
warming, the Cu layer
shallows (if the large - scale subsidence rate is kept fixed), and the inversion strengthens.
Due to the Antarctic Refrigerator Effect, the deep
oceans continued to cool, and the thermocline that separates
warm surface water from cooler deep waters became increasingly more
shallow.
MA Rodger # 16 Yes, it's the fallacious argument that a mass can not
warm a
warmer mass, used in both atmosphere (radiation) and
ocean comments (the fallacy that heat can not increase at depth with also increasing
shallower, and this «heat gone forever» one).
Their scientific cruises on the
shallow continental shelf occurred as sea ice in the Arctic
Ocean was rapidly melting and as northern Siberia was earning the distinction — along with the North American Arctic and the western Antarctic Peninsula — of
warming faster than any place on Earth.
I don't know about heat sloshed under the poles but I need a slosh of scotch heat after this; since you know Bob well you will know he has discussed a reemergence mechanism to explain how the
ocean can put heat into the atmosphere in an El Nino year yet keep
warming itself; and despite the fact that the
oceans are a complex eddying mess the fact remains that AGW is a top down heater; if the
oceans were going to be heated by AGW a
shallow ocean would be heating; but it ain't:
26 Sun Stepped Art Aerosols Greenhouse gases
Warming from decrease Cooling from increase CO 2 removal by plants and soil organisms CO 2 emissions from land cleaning, fires, and decay Heat and CO 2 removal Heat and CO 2 emissions Ice and snow cover Natural and human emissions Land and soil biotoa Long - term storage Deep
ocean Shallow ocean Troposphere Fig. 20 - 6, p. 469
25 Fig. 20 - 6, p. 469 Troposphere Cooling from increase Aerosols
Warming from decrease Green - house gases CO2 removal by plants and soil organisms CO2 emissions from land clearing, fires, and decay Heat and CO2 emissions Heat and CO2 removal Deep
ocean Long - term storage Land and soil biotoa Natural and human emissions
Shallow ocean Sun Ice and snow cover
When many modern families of animals developed in a hot greenhouse world in which a
warm ocean and land filled most of earths surface with fertile
shallow seas and vast tropical jungles.
O.T. but here's another paper for Kenneth to add to the ever growing pile of real research called «Enhanced CO2 uptake at a
shallow Arctic
Ocean seep field overwhelms the positive
warming potential of emitted methane» and is available here http://www.pnas.org/content/114/21/5355.abstract.
If some of the
ocean heat uptake during the last 20 years has shifted from the
shallow and
warm parts to the deeper and colder parts this would reduce the total thermal expansion even if the total heat flux into the
oceans remained the same.
The first is salinity driven and carries mostly hot saline water down into the depths from
shallow equatorial atolls
warming the deep
ocean.
47
Warm, shallow current Cold, salty, deep current Fig. 20 - 12, p. 476 Figure 20.12 Natural capital: a connected loop of shallow and deep ocean currents stores CO2 in the deep sea and transports warm and cool water to various parts of the ea
Warm,
shallow current Cold, salty, deep current Fig. 20 - 12, p. 476 Figure 20.12 Natural capital: a connected loop of
shallow and deep
ocean currents stores CO2 in the deep sea and transports
warm and cool water to various parts of the ea
warm and cool water to various parts of the earth.
Nuccitelli et al. (2012) considered the
warming of the
oceans (both
shallow and deep), land, atmosphere, and ice, and showed that global
warming has not slowed in recent years (Figure 3).
That the slowdown in surface
warming has been concentrated in the
ocean - surface (and
shallow -
ocean) temperatures has led a number of scientists (including the Met Office) to posit that the pause in
ocean surface
warming may be driven in part by increased heat uptake in the deep
ocean.
However, it must be borne in mind that the MOC can also include
shallower, wind - driven overturning cells such as occur in the upper
ocean in the tropics and subtropics, in which
warm (light) waters moving poleward are transformed to slightly denser waters and subducted equatorward at deeper levels.
It looks like the sub-sea permafrost is failing due to
warmer ocean temperatures and allowing methane to escape; because the Siberian Sea is very
shallow the methane isn't oxidized as it travels to the surface.
What are telling observations against the hypothesis of a largely internally driven imbalance are, on the one hand, the fact the sea level variations are relentlessly positive, irrespective the phase of the PDO, and, on the second hand, the fact that the rate of
warming over land is larger than it is over sea (and also that the
shallow (0 - 700m)
ocean layer never actually cools).
However, there has been plenty of
warming of the
shallow oceans that could have been transferred to the deeper
oceans.
In our case, the water is flowing into the tub faster than it's draining out - the
shallow oceans are
warming fast, as the figure above illustrates.
The Arctic
Ocean may be a special case, because of the
shallower stability zone due to the colder water column, and because
warming is expected to be more intense in high latitudes.
I've often wondered at the fact that the deep
ocean has been
warming while the
shallow ocean is cooling.
It's not clear boreal feedbacks are even necessary to lighting off tropical biomass (fire once again), but they'll certainly speed the process way up; if that does happen in turn we're on our way to a hyperthermal (with some lag since the
oceans have to
warm enough to trigger a self - sustaining loss of
shallow methane hydrates).
They explain the lesser
warming in the East Pacific
Ocean, near South America, as being due to the fact this region is kept cool by upwelling, rising of deeper colder water to
shallower depths.