Sentences with phrase «transport of heat into»

However, the transport of heat into the air might go through four channels, which are radiation, convection of the air in the air layer, heat conduction and evaporation.

It has to do with intermittent transport of heat into the deep ocean.

Mauritsen said the warming of the upper ocean and the atmosphere during the summer through reduced cooling around Europe results in the stronger transport of heat into the Arctic, which is actually «pristine» in general.

Not exact matches

It would provide important insight into how much SRM would reduce radiative heating, the concentration of water vapor in the stratosphere, and the processes that determine water vapor transport — which affects the concentration of ozone.

In 1982, German researchers discovered that the edge of the plasma can spontaneously bifurcate into a high pedestal with a steep gradient, or transport barrier, that produces the H - mode confinement and maintains the heat of the plasma core.

They looked at how different planetary rotation rates would impact heat transport with the presence of oceans taken into account.

A combination of computer simulations and observational data reveal that air pockets from the eye can transport heat and moisture into the surrounding storm, increasing the hurricane's intensity.

When the jet stream does that, it transports more heat and moisture up into the Arctic, which heats the Arctic more, which make the jet stream even wavier — another vicious cycle related to disappearance of sea ice.

Transport by these deep - reaching eddies provides a mechanism for spreading the hydrothermal chemical and heat flux into the deep - ocean interior and for dispersing propagules hundreds of kilometers between isolated and ephemeral communities.

After flowing to the cooler face in a wind, it will then tend to recombine into neutral atoms, and thus will enhance the transport of heat.

Water vapor can transport a lot of heat, so when Ceres formed 4.6 billion years ago, sublimation of water ice might have dissipated much of its heat into space, Campins and Comfort wrote.

Going against our previous inclination to not use any other road transport, we escaped the heat of Oaxaca and crossed the border into Chiapas, arriving in the state capital of Tuxtla Gutiérrez nearly 2,000 feet above sea level.

Interior rooms were no longer containers but portals to transport the viewer; the tiny, yet implicitly vast sunset breaking down the distinction between in and out, close and distant, small and large, whilst introducing intense summer heat into a scene of winter mists and cold.

This process is part of what is called the «thermohaline» or «overturning» circulation and is associated with a significant amount of heat transport into the North Atlantic, which indeed keeps Britain and the rest of the North Atlantic region 3 to 6 degrees C warmer than they otherwise would be.

For instance, there is no evidence that, with the current configuration, atmospheric heat transports have vastly different modes of behaviour — and so they are unlikely to suddenly flip into a new state.

One of the reasons that more heat is being transported into the Barents Sea is because of the general rise in temperatures within the Atlantic waters.

It then turns into the North Atlantic Drift which is really the flow of water responsible for the anomalous northward heat transport in the Atlantic.

A good way to estimate the effect of the thermohaline part of the heat transport is to shut it down by dumping a lot of freshwater into the north Atlantic in a climate model, which stops deep water formation there.

This storm is helping to transport large amounts of heat out of the subtropics and mid-latitudes into the Arctic and that is resulting in a pattern change that is reversing the record strong polar vortex into a weaker, more disturbed polar vortex that should support a colder weather pattern across the hemisphere....

How would this change in currents affect the amount of heat in the surface layer that is transported into the Arctic and contributes to melting the Arctic Sea Ice?

re14 Ike Solem >... the rapid changes at the poles seem to involve a lot of heat transport into that region via both the atmosphere and the oceans.

Another course participant, Matt Briggs, who is a wild mushroom seller and Near - Net - Zero Retrofit house owner and the writer, director, and producer of the documentary Deep Green - Solutions to Stop Global Warming Now «was waiting for the affordable Model 3 to plug into my 10kw solar roof so I can finally almost eliminate my carbon footprint for coal electricity, natural gas heat, and now oil transport.»

Rob Painting: The transport of heat down into the surface to deep ocean occurs via the subtropical ocean gyres.

Scientists are still trying to decide how the poleward heat transport will be affected by global warming — but the rapid changes at the poles seem to involve a lot of heat transport into that region via both the atmosphere and the oceans.

IBM thinks one of its 10 MW data centers could heat about 700 homes, and they're looking into using a water - cooled system to transport the heat.

This reminds me of a reference I read some years ago to a country in Africa that has put a well - designed «better donkey cart» into use in rural areas, where heat, sand, and lack of roads make automotive transport unsuitable.

«The bikes will be transported between locations by increasing the heat pumped into the balloon so that it may float into the sky with the rack of bikes connected.

Unfortunately, there is no detailed instrument record of subsurface changes in Gulf Stream heat transport into the region over the past decades, so it's hard to say — and the atmospheric component?

Sea ice is lost due to increasing ocean heat transport into the arctic and the resulting loss of ice causes the atmosphere to warm.

This has nothing to do with heat transport into the ocean, although that phenomenon, in my view, also supports fairly high sensitivities once the evidence for significant rates of deep ocean transport are factored in (but that's a different topic).

A near 80 degree Fahrenheit reading that would be warm in summertime — but one that cropped up in early April as a result of powerful and hot south to north air flows transporting heat across Asia and into the Arctic.

«It is found that the heat transport into the western Barents Sea sets the boundary of the ice - free Atlantic domain and, hence, the sea ice extent.»

Storms help replenish warm water next to the ice, and help carry addtional heat into the melting region via atmospheric transport of warmer moist air.

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..

There is also a planetary boundary layer module that evaluates the turbulent transport of heat and water vapor from the ground surface into the atmosphere.

Based on various paleoclimate proxies and model results, it has been suggested that the input of freshwater into the North Atlantic following these events led to slowdowns of the Atlantic meridional overturning circulation (AMOC) and reductions of its considerable northward cross-equatorial heat transport.

There is no energetic or entropic advantage to be gained from an isoentropic circulation — the only place you actually increase entropy and irreversibly lose heat (the factor that drives all of those heat transport mechanisms) is where something warms and where it cools, where I mean really cools by irreversibly rejecting heat into a cold reservoir, not just adiabatically moving it around, conserved.

Here, we have shown that this warming was associated and presumably initiated by a major increase in the westerly to south - westerly wind north of Norway leading to enhanced atmospheric and ocean heat transport from the comparatively warm North Atlantic Current through the passage between northern Norway and Spitsbergen into the Barents Sea.»

This, in turn, results in increased heat transport into the Arctic (i.e., the «Arctic Amplification»), a prominent feature of earth's recent warming [7 - 9]..

I would assume that all that happens is that the transport of heat is changed in the model: if surface air temps in the model are too high compared to observations, more heat is made to go down into the ocean, and vice versa.

According to a new study, this cold pool may be an indicator of a dramatic slowdown in the Gulf Stream, which transports vast amounts of heat north from the equator to the pole, passing off the East Coast of the U.S. and into the North Atlantic.

Convective patterns driven by heat transport in the interior of the Earth push one crustal plate under another (subduction) and the friction heats up the magma necessary for volcanic action — which in turn releases CO2 into the atmosphere.

My point is that reduction in Arctic / Antarctic ice uses almost no «global» heat, while raising sea - levels orders of magnitude (~ 120 times) more than thermal expansion due to heat transported into the deep ocean.

It's long been known that the Gulf Stream has a significant role in maintaining a mild climate in Northern Europe by the transport of heat far into the North Atlantic.

Since the equatorial westerlies / easterlies are indications of the state of the Quasi-Biennial Oscillation, which is linked to Sudden Stratospheric warming, your head starts getting cooked once you get into the gravity waves that transport all that energy to the polar heat sinks:)

Given that they make the bulk of vertical heat transport in the atmosphere, not sure the models are worth more than the expertise of the different groups into building complex subgrid paramterisations, and this is very far from «models implemetning first principles»... I think that at this stage, climatology have more to win from progress in filling experimental database than from progress from modelling.

That's because solar energy drives evaporation which is an express elevator transporting energy (insensibly; without surface heating) thousands of feet up into the atmosphere where it condenses and radiates to space much easier than it can radiate from lower altitudes.

[3] The Greenhouse House Gas Protocol categorizes direct and indirect emissions into three broad scopes: Scope 1: All direct GHG emissions; Scope 2: Indirect GHG emissions from consumption of purchased electricity, heat or steam; and Scope 3: Other indirect emissions, such as the extraction and production of purchased materials and fuels, transport - related activities in vehicles not owned or controlled by the reporting entity, electricity - related activities (e.g. T&D losses) not covered in Scope 2, outsourced activities, waste disposal, etc..

Simpson began with a gray - body calculation, Simpson (1928a); very soon after he reported that this paper was worthless, for the spectral variation must be taken into account, Simpson (1928b); 2 - dimensional model (mapping ten degree squares of latitude and longitude): Simpson (1929a); a pioneer in pointing to latitudinal transport of heat by atmospheric eddies was Defant (1921); for other early energy budget climate models taking latitude into account, not covered here, see Kutzbach (1996), pp. 354 - 59.

This occurred in part because of large amounts of ocean heat being transported into the area through the Bering Strait.