Sentences with phrase «little heat transport»

Not exact matches

We have to clean the plastic in a closed looped system to remove all of the chemical residues and contaminants, then we apply the NANO technology to the plastic and when we heat it up to make the green little nurdles, the heat exchange eliminates any toxins, poisons, leaching, the list goes on and on... The plastic is so safe, that the Department of Conservation has asked us to make the same box for agricultural applications for loading and transporting fresh veggies from farm to market instead of using a waxed based cardboard box.

The stress on shelter staff is significant: no room to put ever more dogs; having to euthanize dogs to make room for new dogs; performing triage on sick animals when space is limited; having to make hard choices about evening and weekend heating and lighting with a small budget; no veterinarian or vet tech on the staff; no evening or weekend staff; no time to network adoptable animals; no available homes in the surrounding communities; inadequate transport vehicles; little or no support from local government; an Animal Control Officer often doing double duty, responsible also for managing the shelter; counties lacking even a shelter or inside kenneling.

They change the heat transport between hemispheres and cause a kind of «see - saw»: the south cools as the north heats up and vice versa, with little effect on the global mean.

... not intended to suggest that the heat capacity exchange / transfer / transport rates used are a realistic representation of actual ocean circulation, although from what little I know, it could be a step in that general direction from using one upper and one deep ocean reservoir.

I hadn't heard about the heat transport via the atmosphere, but it didn't surprise me — that is what the jet streams are all about — a wind caused by an atmospheric temperature differential, given a little bit of a spin.

Conceptually, it's hard to see how the Gulf Stream western boundary current could be weakened by conditions around Greenland; this is a fluid dynamics system, not a mechanical «belt»; a backup due to less deep water formation should have little effect on the physics of the gyre and the formation of the western boundary current, and it also seems the tropical warming and the resulting equator - to - pole heat transport are the drivers — but perhaps modulation by jet stream meandering is playing some role in the cooling?

Re 40 simon abingdon — there is very little mass loss to space (can be significant for evolution of conditions over geologic time or in more extreme conditions, but not for Earth like conditions over the timescales over which climatic equilibrium is determined), and latent and sensible heat are transported by conduction and convection and mass diffusion, which can't significantly extend outside the atmosphere.

That one was little - noticed by the world's media, but now its findings may receive more attention, as an independent study by NCAR, published yesterday in Nature Climate Change, has investigated the same subject and reaches a confirming conclusion: in recent years atmospheric warming has been delayed due to increased heat transport to the deeper ocean.

When it gets a little warmer in the NH tropics a little more heat is transported to the Arctic for disposal.

For example, the Hadley cell, the large - scale pattern of atmospheric circulation that transports heat from the tropics to the subtropics, has marched south during recent decades, moving the subtropical dry zone (a band that receives little rainfall) along with it.

Conversely, during low solar activity during the Little Ice Age, transport of warm water was reduced by 10 % and Arctic sea ice increased.17 Although it is not a situation I would ever hope for, if history repeats itself, then natural climate dynamics of the past suggest, the current drop in the sun's output will produce a similar cooler climate, and it will likely be detected first as a slow down in the poleward transport of ocean heat.22 Should we prepare for this possibility?

Little research exists to determine how large an area must remain unchanged, but one suspects it is quite large to be beyond the heat transported by wind.

We find that an increase in poleward heat transport by the tropical ocean results in a warming of the extra-tropics, relatively little change in the tropical temperatures, moistening of the subtropical dry zones, and partial but incomplete compensation of the planetary - scale energy transport by the atmosphere.