Recent observational studies have focused on ascertaining two questions of relevance to the AMOC response to climate change: What is the impact of variable North Atlantic
Deep Water production on the ocean's meridional overturning?
To ascertain with confidence the extent to which
deep water production impacts the ocean's meridional circulation and hence the ocean's contributions to the global poleward heat flux, continuous measures of trans - basin mass and heat transports are needed.
Therefore, a transoceanic line in the subpolar North Atlantic, currently being planned by the international community, that measures the net contributions of the overflow waters from the Nordic Seas as well as those from the Labrador Sea, to the AMOC, would directly test the legitimacy of the decades - long supposition that variability in North Atlantic
Deep Water production translates into meridional overturning variability (Figure 2.4).
Rind, D., G.L. Russell, G.A. Schmidt, S. Sheth, D. Collins, P. Demenocal, and J. Teller, 2001: Effects of glacial meltwater in the GISS Coupled Atmosphere - Ocean Model: Part II: A bi-polar seesaw in Atlantic
Deep Water production.
This result raised questions about the responsiveness of the AMOC to changes in
deep water production; however, the linkage could not be conclusively ruled out because of increasing indications that the DWBC was not the sole conduit for the passage of deep waters to the lower latitudes (Schott et al., 2006).
Weyl (1968), speculating that the «temporary stagnation» of the bottom water would end because of warming by the interior heat of the Earth; the role of glacial meltwater suppressing North Atlantic
Deep Water production was also pioneered by Worthington (1968); a neat explanation of the entire circulation in terms of water evaporating from the North Atlantic more than from the cooler North Pacific was indicated by Warren (1983).
The closure of the circumtropical seaways is assumed to have triggered and / or strengthened the North Atlantic
Deep Water production, initiated the Caribbean Current, strengthened the Gulf Stream, and, therefore, changed the global distribution of deep - water masses, heat and salinity (Haug & Tiedemann1998).
But
deep water production by convection may be less, depending on how much NADW is Arctic in origin and how much is simply recirculated Antarctic bottom water (extremely dense water, formed as brine under the sea ice around polynas offshore of Antarctica and sliding down the continental shelf into the depths without much mixing, creates a giant pool of dense water extending all the way up the bottom of the Atlantic to about 60 ° N).
The relationships between the NAO and
deep water production are discussed by R. Dickson, «Observations of DecCen climate variability in convection and water mass formation in the northern hemisphere,» in the CLIVAR Villefranche workshop summary at http://www.dkrz.de/clivar/villesum.html. More generally, see the Climate Research Committee, National Research Council, Natural Climate Variability on Decade - to - Century Time Scales (National Academy Press 1995).
They haven't reached the point of development when we are sure that they are doing everything right for the right reasons, and so my instinct is to be very cautious in interpreting ocean model results that rely on shifts in the location of
deep water production etc..
A bipolar seesaw in
deep water production.
Not exact matches
For
deep water, the time frame from initial exploration discovery to
production of oil ranges from 5 to 10 years.
Furthermore, oxytocin
production often increases when women are immersed in
deep warm
water, which can speed up labor without any increase in sensation / pain.
With the discovery of larger commercial quantities of oil and gas in
deep water offshore Ghana, It became necessary for the bill to passed as the new phase of oil exploration has comes with new challenges with actual development,
production and utilisation of its oil and gas resources.
This innovation, he said, marked a turning point in SNEPCo's efforts to develop the capabilities of Nigerian companies in the provision of goods and services in
deep -
water oil and gas
production.
If not enough
water is present in the mantle about 100 to 200 km
deep to keep things flowing, continental
production decreases.
In 2000, the US Department of the Interior's Minerals Management Service (MMS) published a report warning that there were several difficulties connected with
deep -
water well control, that experience in this area was «limited» and with many rigs having very high oil
production rates, a blowout could be «a potential show - stopper» for
deep -
water drilling in general.
Phytoplankton
production is enhanced by strong winds (because they cause upwelling of nutrients from
deeper waters) and diminished by weaker winds, and the scientists found evidence that trade winds were weaker then.
All that, combined with benchmark braking and world - class ride and handling characteristics, make the Dodge Charger SRT8 civilized enough for a grocery run but fully capable in more challenging situations • The 2009 Dodge Charger SRT8 is part of a broad lineup of Street and Racing Technology vehicles developed under the credo «Race inspired, street legal» SAFETY AND SECURITY Please refer to the Safety and Security Glossary for descriptions of the following features: • Advanced Multi-stage Air Bag System • All - speed Traction Control System • Anti-lock Brake System (ABS) • Auto - reverse Sun Roof • BeltAlert • Brake Assist • Brake / Park Interlock • Child - protection Rear Door Locks • Constant Force Retractors • Crumple Zones • Electronic Stability Program • Energy - absorbing Steering Column • Enhanced Accident Response System • Height - adjustable Seat Belts • HomeLink Universal Home Security System Transceiver • Inside Emergency Trunk Release • Interior Head - impact Protection • Knee bolsters • LATCH (Lower Anchors and Tethers for CHildren) • Low - risk Deployment Air Bag • Power Adjustable Pedals • Remote Keyless Entry • Seat Belt Pretensioners • Sentry Key ® Engine Immobilizer • Side - impact Door Beams • Tire Pressure Monitoring Display COLOR AVAILABILITY •
Deep Water Blue Clear Coat • Bright Silver Metallic • Brilliant Black Crystal Pearl Coat • TorRed • Hemi Orange (with Super Bee Special Edition Package) MANUFACTURING INFORMATION • 2009 model year
production start: July 2008 • Production location: Brampton Assembly Plant in Brampton, Ontario, Canada • 6.1 - liter HEMI V - 8 engine: Saltillo Engine Plant in Saltillo, Mexico • Five - speed automatic transmission: Indiana Transmission 1 in Indianapolis MARKET POSITION Dodge Charger SRT8 is the latest incarnation of a storied Dodge performance nameplate, combining SRT performance attributes with Dodge
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Production location: Brampton Assembly Plant in Brampton, Ontario, Canada • 6.1 - liter HEMI V - 8 engine: Saltillo Engine Plant in Saltillo, Mexico • Five - speed automatic transmission: Indiana Transmission 1 in Indianapolis MARKET POSITION Dodge Charger SRT8 is the latest incarnation of a storied Dodge performance nameplate, combining SRT performance attributes with Dodge
Production location: Brampton Assembly Plant in Brampton, Ontario, Canada • 6.1 - liter HEMI V - 8 engine: Saltillo Engine Plant in Saltillo, Mexico • Five - speed automatic transmission: Indiana Transmission 1 in Indianapolis MARKET POSITION Dodge Charger SRT8 is the latest incarnation of a storied Dodge performance nameplate, combining SRT performance attributes with Dodge attitude.
As most of the earth is covered by ocean the next questions could be of the UV / VIS - spectrum of
water:» How
deep under
water floating algae can photosynthesize and what is the effect of ozone hole to the primary
production on the southern ocean?»
The government hopes to revive domestic natural gas
production with the technology that has transformed the energy picture in the United States — horizontal drilling into
deep underground shale, and high - pressure injection of
water, sand, and chemicals to create fissures in the rock to release the gas.
«The goal of Sapphire is to produce a crude product that can be introduced into the existing crude stream for
production costs that are similar to other new opportunities like oil shales, oil sands, and even
deep,
deep water drilling,» Jason Pyle, Sapphire's chief executive said in an interview.
Changes in the
production rate of
deep water in this sector of the ocean may push the climate system from one quasi-stable mode of operation to another.
Primary
production will change in the surface layers according to sun exposure,
water temperature, major stratification of
water masses, for example, and this will affect the food chain down to the
deep seafloor, which will be subject to differences in quantity, quality, and timing of organic matter input.
[6] The main methods of disposing of produced
water involve pumping it back into oil - or gas - producing wells to bolster
production, or injecting it
deep into other formations below usable groundwater resources.
Wind power
production in the
deep waters of the open ocean is in its infancy of commercialization.
Though many modeling studies have demonstrated the impact of
deep water formation changes on the overturning circulation, the observational evidence for such a linkage has been hard to come by for two reasons: (1) Deep water formation is difficult to quantify because the time and locale of production are highly variable from winter to winter, and (2) overturning circulation measures require observations that span the basin, which have been limited in space and t
deep water formation changes on the overturning circulation, the observational evidence for such a linkage has been hard to come by for two reasons: (1)
Deep water formation is difficult to quantify because the time and locale of production are highly variable from winter to winter, and (2) overturning circulation measures require observations that span the basin, which have been limited in space and t
Deep water formation is difficult to quantify because the time and locale of
production are highly variable from winter to winter, and (2) overturning circulation measures require observations that span the basin, which have been limited in space and time.
Rather, it is likely that surface warming gradually stabilizes ocean stratification, thus reducing
deep -
water production at high latitudes, which acts to weaken advective heat uptake by meridional overturning circulation [cf. Meehl et al., 2011; 2013].»
Currently available proxy data are equivocal concerning a possible increase in the intensity of the meridional overturning cell for either transient or equilibrium climate states during the Pliocene, although an increase would contrast with the North Atlantic transient
deep -
water production decreases that are found in most coupled model simulations for the 21st century (see Chapter 10).