Sentences with phrase «radiate heated water»

Near the vessel's keel, divers can find thermal vents that radiate heated water from deep underground.

Not exact matches

The so - called greenhouse gases — mainly water vapor and carbon dioxide — make the planet warm and habitable by trapping solar heat as it radiates back off the Earth.

The next most abundant gases — water vapor and carbon dioxide — do absorb a portion of the infrared heat radiated by the earth's surface, thereby preventing it from reaching space.

Clouds of water vapor around Ceres absorbed the heat that radiates from the dwarf planet, which Herschel's instrument detected.

Animals are kept warm with circulating warm water blankets, a heat radiating recovery bay, and blankets until they can thermo regulate on their own.

Although their body temperatures are no higher than that of any other dog, the Peruvian Inca Orchid's hairless skin radiates more heat than that of a regular dog and acts almost like a hot water bottle.

The effervescent waters of the Seaside Kingdom's Bubblaine fizz and pop, while the sticky hot candy caramel lava of the Luncheon Kingdom's Mount Volbono oozes and bubbles like you can almost feel the heat radiating off of it.

The works on show, sand cast sculptures hanging to the wall, are connected with a circuit of pipe to the building's water system; warmed by hot water, they radiate heat.

There's also a number of interesting applications in the evolution of Earth's atmosphere that branch off from the runaway greenhouse physics, for example how fast a magma - ocean covered early Earth ends up cooling — you can't lose heat to space of more than about 310 W / m2 or so for an Earth - sized planet with an efficient water vapor feedback, so it takes much longer for an atmosphere - cloaked Earth to cool off from impact events than a body just radiating at sigmaT ^ 4.

Resonant absorption will convert heat energy to kinetic energy in the molecule (water vapour, CO2 et al) and be transferred by collision to the general atmosphere, from where it will be radiated into space.

Away from the dense network of heat absorbing (daytime) then heat radiating (nighttime) structures which is the Urban Heat Island and above the air with high water vapor content trapped by the valley along the river, not to mention the pall of coal dust over the city, morning low temps were much more like what the natural countryside would experieheat absorbing (daytime) then heat radiating (nighttime) structures which is the Urban Heat Island and above the air with high water vapor content trapped by the valley along the river, not to mention the pall of coal dust over the city, morning low temps were much more like what the natural countryside would experieheat radiating (nighttime) structures which is the Urban Heat Island and above the air with high water vapor content trapped by the valley along the river, not to mention the pall of coal dust over the city, morning low temps were much more like what the natural countryside would experieHeat Island and above the air with high water vapor content trapped by the valley along the river, not to mention the pall of coal dust over the city, morning low temps were much more like what the natural countryside would experience.

The 540 cal / gram of evaporated water removed is released in the upper troposphere, where some of the heat released can be radiated into space = net cooling effect.

I would think that 3 degrees would be more than enough, especially after a few years of that heat radiating through any sediment that is between the water and the hydrate or permafrost.

Of course, maybe this is kind of what you were saying all along:), but it worried me when you said that the air could gain heat from the water and still cool, which is only possible if the air is radiating heat to space faster than it is receiving it from the ocean.

but it worried me when you said that the air could gain heat from the water and still cool, which is only possible if the air is radiating heat to space faster than it is receiving it from the ocean.

If you stand next to the pool and hold your hands over it you can actually feel the heat radiating from the water.

Some heat radiates back to space or trapped in biosphere Balance determines Earth's average temperature Gases that control in atmosphere are carbon dioxide, methane, water vapor.

Basically, as fast as heat loiters about on our planet's surface, it either radiates off to space or Water will pick it up and carry it to the upper layers of our atmosphere, where it will change form from gas to liquid or solid giving off heat to space while being super cooled at the same time.

This heat is radiated to space with the physical form change from gas to liquid or solid and this super or sub cooled water returns to Earth for further cooling.

Part way there, but no quantitation yet: of the 3.77 W / m ^ 2 radiated back dowwnard, most goes to increased rate of evaporation of the water at the surface, and much less goes to increased mean temp increase at the surface; hence increased rate of non-radiative transfer of heat from surface to upper atmosphere, slight increase in rainfall as hydrological cycle is faster, and slight increase in cloud cover.

Heat is being radiated into space from GH gases (including water vapour) in the upper atmosphere.

The new system has only a tiny fraction of the heat energy and that 1 gram of hot water will quickly radiate its energy away.

As water has the property of reaching maximum density above its freezing point, the heat is transported towards the surface, eventually to be radiated away to outer space.

A hot frying pan can cooled much quicker by pouring water on it - probably around 100 times faster - than compared simply letting it radiate the heat.

But perish the thought that you should heat the water to above 100 deg C whereupon it becomes a gas, and immediately stops radiating thermal radiation; because everybody knows; or seems to think that gases do not emit black body like thermal radiation.

LIA wasn't GLOBAL cooling; but colder in Europe, north America — because Arctic ocean had less ice cover - > was releasing more heat / was accumulating - > radiating + spreading more coldness — currents were taking that extra coldness to Mexican gulf — then to the Mediterranean — because Sahara was increasing creation of dry heat and evaporating extra water in the Mediterranean — to top up the deficit — gulf stream was faster / that was melting more ice on arctic also as chain reaction — Because Mediterranean doesn't have enough tributaries, to compensate for the evaporation deficit.

We humans feel the heat radiated by the Sun and other systems with a higher temperature because our bodies contain 55 - 75 % of water.

These stem from a diversity of site - specific conditions, including, but not limited to: local vegetation; presence of building structures and contributions made by such structures involving energy use, heating and air conditioning, etc; exposure to winds, the wind velocities determined by climatic factors and also whether certain wind directions are more favored than others by terrain or the presence or absence thereof to bodies of water; proximity to grass, asphalt, concrete or other material surfaces; the physical conditions of the CRS itself which include: the exact location of the temperature sensors within it, the degree of unimpeded flow of external air through the CRS, the character of the paint used; the exact height of the instrument above the external surface (noting that when the ground is covered by 3 feet of snow, the temperature instrument is about 60 % closer to, or less than 2 feet, above an excellent radiating surface, much closer than it would be under snow - free conditions).

One idea was that increased IR radiated from water vapour in these air masses could off - set expansion due to release of latent heat, and ad drive horizontal circulation This had to be attacked as it showed a role for radiative gases in atmospheric circulation.

As obvious on figures 6 - A and 6 - B, Ttop and Ptop are determined by the water vapour that radiates over some 1900 cm - 1 much more than the 40 cm - 1 of the tropospheric CO2 near 614 cm - 1 and 718 cm - 1.; stratospheric radiation to the cosmos is not very important because the cooling of each layer is exactly equal to its heating mostly by UV absorbed by Ozone.

In fact the sensible heat or a portion of it gets radiated to space so the heated air parcel never becomes as light as it was when it contained water vapour so it becomes denser and heavier and must fall.

Since the water vapor emission level (WVEL) has not increased in altitude, extra latent heat is mostly radiated to space.

When water vapor (97 % of Earth's Greenhouse gas) condenses into clouds, vast amounts of heat are released and radiated into Space.

Also forgotten is the 50W radiated by each human's basal metabolic rate, plus the heat of condensation of the water in each breath when cold enough.

The warm surface waters radiate more heat to the atmosphere and even directly to space, so there's more net cooling going on than in ENSO - neutral or La Nina conditions.

The CO2 (and water vapour etc.) gains heat and but can't store it (except by transfer to O2 & N2 which are poor radiators) so must radiate.

K) However, radiation heat loss does depend on the fourth power of radiating (sea surface or ice surface) temperature — which will be right at 273 K — 275 K for open water; but what might be as low as -12 to -20 at the equinox for ice - covered water exposed directly to the rapidly freezing Arctic air.

Earth has a natural «greenhouse effect» that results from gases like water vapor, carbon dioxide (CO2), and methane absorbing heat radiated from the Earth's surface and lower atmosphere and radiating that heat back towards the surface.

So water can explained as same as atmosphere - sunlight is transparent to water, sunlight passes thru the water and heats the water under the surface, and heat generated is blocked from radiating IR.

«what does happen is that the water surface radiates away at about 400W / m ^ 2, in fact the top few microns will be cooler than the water a mm deeper because the transfer of heat from lower down (conduction, convection, diffusion etc.) is slower than the loss from the surface.»

Obviously that doesn't happen, what does happen is that the water surface radiates away at about 400W / m ^ 2, in fact the top few microns will be cooler than the water a mm deeper because the transfer of heat from lower down (conduction, convection, diffusion etc.) is slower than the loss from the surface.

Water vapor, which is a greenhouse gas, albeit short lived, and a component of and response to weather conditions — but not, being so ephemeral, a driver of much longer term weather patterns (or climate)-- and due to it's heavy prevalence the greenhouse gas that is on average responsible for more re ra - radiated heat than any other, in fact is not warming, but cooling.

But the additional water vapor will radiate heat away more quickly, having the opposite effect; however, when the temperature drops to where the water begins condensing, the latent heat released will decrease the lapse rate to the moist adiabatic lapse rate.

At night, «low grade» heat is transferred to the ball from the water by convection / conduction and is radiated out to «space.»

They constantly radiate heat into its ovens and hob plates, so it's always ready to use and in some cases can provide heating and hot water for the household, therefore the mighty appliance was popular in an era when central heating was a luxury in your home.