Sentences with phrase «outgoing heat from»

The influence of atmospheric CO2 on the balance between incoming energy from the Sun and outgoing heat from the Earth (also called the planet's energy balance) is well established.

The influence of atmospheric CO2 on the balance between incoming energy from the Sun and outgoing heat from Earth (also called the planet's energy balance) is well established.

Not exact matches

Education may have been mostly left out of this year's heated presidential election, but that hasn't stopped the current, outgoing president from shining a spotlight on his education record.

The increase in insolation of 2 W / m2 from the cloud cover decrease was accompanied by an extra outgoing 5 W / m2 heat flow...

Surface temperature is an imperfect gauge of whether the earth has been warmed by an imbalance between incoming radiation from the sun, and outgoing radiation, because of the role of ocean currents in the distribution of heat between deeper and surface waters.

Is the majority of the initial (before feedback) atmosphere heating resulting from increased CO-2 reduced by the fact that the majority (W - Sq - M at low latitude) of outgoing radiation is in the latitudes most saturated by water vapor?

A heat recovery ventilator reduces energy use by transferring the heat or cold from the outgoing stale air and using it to condition the incoming fresh air.

All ventilation through a Heat Recover Ventilator which conserves 95 % of heat and cold from outgoing Heat Recover Ventilator which conserves 95 % of heat and cold from outgoing heat and cold from outgoing air.

The house features: Earth sheltering on three sides with a carefully designed PAHS style insulation umbrella that uses the surrounding earth for thermal storage.Passive solar gain through the south triple glazed windows.Active solar through several Trombe walls integrated into the south wall.An extensive earth tube system that pre-heats incoming fresh air and recovers heat from outgoing stale air.A carefully designed back up wood heating system.Solar water heatingProvisions for solar electricity.The house is located at 45 degrees north latitude and has a serious winter — the total heating bill for the past two winters has been $ 70 worth of wood — about 0.6 cords.

An atmosphere that is perfectly transparent to incoming and outgoing radiation can not radiate and all its heat content comes from conduction from the surface and is transported through the atmosphere solely by convection with no loss of energy to space except for the tiny fraction of atoms at the top of the atmosphere that exceed escape velocity.

The only thing that is relevant to the GHE is the outgoing radiation budget, which is the only way the Earth loses the heat it picks up from the Sun (with an extremely modest addition from all other sources).

The cooling or heating effects from incoming or outgoing radiation occurs on these surfaces and not to any appreciable effect within the airmass itself.

As long as the outgoing longwave radiation is n`t decreasing over the Top Of Atmosphere, all the heat uptake comes from the change of short wave radiation.

On the 2000 meter depth graph over 2006 - 2014 of Poitou & Bréon, the yearly minima increased from 10 units to 16 units of 1022 J that is 0.41 W / m ²; but there is every year some oceanic heat storage during six months and a release of this heat the following six months: the maximum of the global outgoing longwave radiation is in July, shifted by 6 months w.r.t. the solar flux hat is maximum in January (1412 W / m ²) and minimum in July (1321 W / m ²).

To be energy or more properly, heat transferred, the one - way upwelling radiation from the surface absorbed by the air should be reduced by subtraction of the down - welling radiation of the air absorbed by the surface Note that by subtraction of the (about 20 W / m ² in global average) flow surface to cosmos of both terms of GH, GH expression becomes GH = (radiation from the surface absorbed by the air) minus (outgoing longwave radiation from the air) which has absolutely no physical sense!

northern Scandinavia) cloudy days in November and December are typically warmer than cloud - free days because the Earth's surface has a net radiation loss at the time (i.e. outgoing heat loss exceeds radiation received from the sun).

If so, then we can put numbers behind the qualitative discussion on the influence of CO2 on the climate of the Earth since we can now relate the additional heat available due to the absorption of the outgoing radiation by CO2 to the total heat available due to the irradiation from the Sun and the back radiation previously to the enriching of the atmosphere by CO2.

On top of the ocean heating, we can look at the outgoing radiation from the atmosphere, by satellite, to see that frequencies associated with water vapor and CO2 have reduced upward emissions.

In other words, * we can observe the increase of CO2 in atmosphere above the ocean, * CO2 absorbs some part of the outgoing radiation from the surface of the ocean which increases somewhat the temperature of the air * The increasing of temperature causes the (slight) increase of the (already existing) back radiation * This (now increased) back radiation is absorbed by the surface skin layer of the ocean which means that the energy delivered by the back radiation to the surface skin layer is now slightly higher * This additional energy will now be distributed over the channels that are participating in the heat transfer from the absorbing surface skin layer to both the air above the skin layer and the bulk of the ocean.

It includes results from a variety of different empirical approaches, including (1) time series analyses of the published temperature record; (2) examination of the response of the earth's outgoing radiation response to transient climate events; (3) calorimetric studies of the ocean - atmosphere system; (4) mechanisms for secular climate change arising from ocean circulation systems and astronomical influences; and (4) radiative and convective heat transfer in the oceans and atmosphere.

With no greenhouse gases, the earth will either heat up or cool down until the outgoing flux from the earth is equal to the incoming flux from the sun.

It is also not because of the initial outgoing from the surface, after absorption of and heating from that solar flux.

One might say that the heat that consumes time migrating from the incoming surface to the outgoing surface represents the heat of greenhouse warming.

[38] Greenhouse gases absorb and emit some of the outgoing energy radiated from Earth's surface, causing that heat to be retained in the lower atmosphere.