Sentences with phrase «water circulation more»

-LSB-... * Salinity in the sea fell sharply during the Permian for the first time, changing oceanic physics to make deep water circulation more difficult.

Not exact matches

Right after birth you will quickly drop a few pounds from excess water and more weight loss will happen when your blood circulation goes back to normal and so does your uterus size.

Bleeding might be more severe in a tub as the warmth might cause more circulation, and with a pre-term baby, the lungs may not be developed enough to handle the water should the baby breathe any water in.

For more than two decades, scientists studying hydrothermal circulation in the water under the seafloor have assumed that the flow is relatively stable.

See also the saturated GCM calculation in my more recent water vapor article, from the Caltech general circulation book.

Are you saying that ocean circulation patterns in the Northern Hemisphere do not reach Antarctic regions where ice is more in the water?

It's more common to take warm showers and finish with a jolt of cold water to tone and firm the skin by enhancing circulation.

Less is known about its usefulness in mixtures against water retention and cellulite, where it can advantageously replace lemon essence, and its more general circulation revitalizing action.

Water is essential for replenishing skin tissues, moisturizing, and enhancing * elasticity, ridding of toxins, improving * blood circulation, and producing energy to give you a more youthful, radiant, glowing complexion.

The constant circulation of water keeps it oxygenated and as a result, it has more taste appeal.

Our Class IV therapeutic laser delivers specific wavelengths of laser light to increase circulation and deliver more oxygen, water and nutrients to tissues.

This seems like it's going to keep tropical waters hotter and thus promote more hurricanes (in agreement with what Gray says (if one interprets his statements as referring to the portion of the atlantic circulation — the subtropical gyre — that delivers more warm water to the tropics).

In particular, I won't be surprised if continued decade - to - decade variability in atmospheric circulation results in more, and less, intrusion of circumpolar deep water onto the continental shelf, and to more, and less, rapid thinning of ice shelves in West Antarctica *.

As far as this historic period is concerned, the reconstruction of past temperatures based on deep boreholes in deep permafrost is one of the best past temperature proxies we have (for the global regions with permafrost — polar regions and mountainous regions)-- as a signal of average temperatures it's even more accurate than historic direct measurements of the air temperature, since the earth's upper crust acts as a near perfect conservator of past temperatures — given that no water circulation takes place, which is precisely the case in permafrost where by definition the water is frozen.

Partly this has to do with changes in ocean circulation taking warmer water deeper and partly as the result of the southern hemisphere having less land mass and more ocean — where the ocean has a higher thermal inertia, meaning that it takes longer for those waters to warm.

Another possibility might be a slowing of deep circulation (not sure how much there is, mind), in which case the opposite occurs, and the surface waters heat up even faster, leading to yet more rapid surface melt, smaller winter ice volumes and so on.

The undetected «threshold» scenario that I posed in # 11 could be more generally characterized as a shift in the thermo - haline circulation (THC) caused by an emergent new source region for deep water formation.

It is known that there is a pronounced difference in Hadley cell circulation between winter and summer, heat spreading more evenly would mean greater water vapor density, exacerbating AGW effects a great deal more.

Ultimately if the freshwater melt was a dominant (which seems hard to believe given the scale of the wind - driven gyre transport) factor, it would be entrained into the gyres at the surface and you'd see an overall freshening of North Atlantic surface waters to make the whole system more like the Pacific, which has a much weaker meridional overturning circulation.

The Guardian says: «the Atlantic Meridional Overturning Circulation (Amoc), has weakened by 15 % since 1950, thanks to melting Greenland ice and ocean warming making sea water less dense and more buoyant.

So while the monsoon winds might weaken the precipitation nonetheless increases (more bang for the buck) as a weaker circulation carries more water vapor (and latent energy).

Higher modelled temperature in the troposphere enables the general circulation model to assume there is more water vapour in the troposphere which amplifies the CO2 forcing by increasing the amount of water vapor in troposphere.

The vertically integrated inventory of human emitted CO2 in the oceans is (not surprisingly) much greater in areas of cold deep convection, especially in the northern Atlantic (the falling leg of the thermohaline circulation), and much less in the tropics where the ocean is strongly stratified; absorption in the tropics really is more in the near - surface waters.

When the tropical easterly trade winds strengthen, as they have from the year 2000 onwards, this whole wind - driven ocean circulation becomes more vigorous, the South Pacific subtropical gyre spins up, and the western arm of the gyre exports more tropical water through the Indonesian archipelago into the Indian Ocean.

Some of the warm water would be subducted by Atlantic Meridional Overturning Circulation / Thermohaline Circulation, some would be carried by ocean currents into the Arctic Ocean where it would melt sea ice, and the remainder would be spun southward by the North Atlantic gyre toward the tropics so it could be warmed more by the effects of the slower - than - normal trade winds.

It releases more than it absorbs because of ocean conveyor belt circulation pulling in tropically warmed water.

Through horizontal averaging, variations of water vapor and temperature that are related to the horizontal transport by the large - scale circulation will be largely removed, and thus the water vapor and temperature relationship obtained is more indicative of the property of moist convection, and is thus more relevant to the issue of water vapor feedback in global warming.

The tropical cyclones that bend northwards, move across this warm water, that adds more vertical convection power and moisture to the weather system — that can then turn into a closed circulation hurricane.

It would explain a lot more if there were variations in the water temperatures coming from the oceanic circulations BEFORE they became involved in the ENSO process.

This is due to several ACD - linked factors, including warming water (which expands as it warms), more severe storms and a stronger Atlantic meridional overturning circulation, on which Truthout previously reported in detail.

and «It would explain a lot more if there were variations in the water temperatures coming from the oceanic circulations BEFORE they became involved in the ENSO process.

The water cycle assists stabilisation of top of atmosphere energy balance and reduces the need for a more vigorous circulation.

Scientists have recently observed major changes in these glaciers: several have broken up at the ocean end (the terminus), and many have doubled the speed at which they are retreating.2, 5 This has meant a major increase in the amount of ice and water they discharge into the ocean, contributing to sea - level rise, which threatens low - lying populations.2, 3,5 Accelerated melting also adds freshwater to the oceans, altering ecosystems and changing ocean circulation and regional weather patterns.7 (See Greenland ice sheet hotspot for more information.)

In the Atlantic Ocean, the Gulf Stream is part of what's called the Atlantic Meridional Overturning Circulation, a conveyor belt of ocean water that carries warm water from Florida to Greenland where it cools and sinks to 1000 meters or more before traveling back down the coast to the tropics.

«Relatively cool waters in the eastern Pacific often result in stubborn summer high - pressure systems over the eastern states that block storms, reducing the frequency of precipitation below normal,» noted study co-author Richard Healy of the Woods Hole Oceanographic Institution, Woods Hole, Mass. «Less frequent storms result in higher surface and atmospheric temperatures that then feedback on the atmospheric circulation to further reduce storm frequency and raise surface temperatures even more.»

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 (1water 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 (1Water 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 (1water evaporating from the North Atlantic more than from the cooler North Pacific was indicated by Warren (1983).

In addition to the main threshold for a complete breakdown of the circulation, other thresholds may exist that involve more - limited changes, such as a cessation or diminishment of Labrador Sea deep water formation (Wood et al., 1999).

While a surge in heavy, salty water can invigorate deep water circulation, a dilution of the waters prompts a more lethargic flow.

«Salt plays a far more important role that we first thought,» says Rainer Zahn, a palaeoclimatologist at the Autonomous University of Barcelona in Spain.Zahn and his colleagues found that a build up of salty water off the coast of South Africa could jump start ocean circulation in the North Atlantic (this despite the two regions being thousands of kilometers apart) while a reduction in the South African waters» saltiness could cause the opposite effect.

Adding more Co2 will either increase this process slightly (the Walker circulation) or limit water vapor's presence in the upper troposphere by radiational cooling.

More recently, there was a proposal to dam the Straits of Gibraltar in order to prevent more saline Mediterranean Sea water (because of the Aswan Dam) from affecting the North Atlantic conveyor circulation (no, it didn't make sense to us eithMore recently, there was a proposal to dam the Straits of Gibraltar in order to prevent more saline Mediterranean Sea water (because of the Aswan Dam) from affecting the North Atlantic conveyor circulation (no, it didn't make sense to us eithmore saline Mediterranean Sea water (because of the Aswan Dam) from affecting the North Atlantic conveyor circulation (no, it didn't make sense to us either).