Sentences with phrase «larger heat capacity of»

The «note» you refer to goes: «Note: LOTI provides a more realistic representation of the global mean trends than dTs below; it slightly underestimates warming or cooling trends, since the much larger heat capacity of water compared to air causes a slower and diminished reaction to changes; dTs on the other hand overestimates trends, since it disregards most of the dampening effects of the oceans that cover about two thirds of the earth's surface.»

Note: LOTI provides a more realistic representation of the global mean trends than dTs below; it slightly underestimates warming or cooling trends, since the much larger heat capacity of water compared to air causes a slower and diminished reaction to changes; dTs on the other hand overestimates trends, since it disregards most of the dampening effects of the oceans that cover about two thirds of the Earth's surface.

«Note: LOTI provides a more realistic representation of the global mean trends than dTs below; it slightly underestimates warming or cooling trends, since the much larger heat capacity of water compared to air causes a slower and diminished reaction to changes.»

The observed fact that temperatures increases slower over the oceans than over land demonstrates that the large heat capacity of the ocean tries to hold back the warming of the air over the ocean and produces a delay at the surface but nevertheless the atmosphere responds quit rapidly to increasing greenhouse gases.

The first issue is that because of the large heat capacity of the southern oceans, warming trends are in general going to be smaller than in the northern hemisphere.

(It is to be noted that the same models predict a significant delay until equilibrium is reached, due to the large heat capacity of the Southern ocean.

Because of the large heat capacity of the ocean, nothing disastrous regarding the Earth's climate is likely to happen in your lifetime.

In contrast, the oceans lose heat less rapidly, because of the large heat capacity of water, their ability to overturn as the surfaces cool and become negatively buoyant, and the movement of ocean currents such as the Gulf Stream and the Kuroshio current.

The large heat capacity of the oceans mean they soak up a lot of energy and slow down the heating of the atmosphere.

The basic results of this climate model analysis are that: (1) it is increase in atmospheric CO2 (and the other minor non-condensing greenhouse gases) that control the greenhouse warming of the climate system; (2) water vapor and clouds are feedback effects that magnify the strength of the greenhouse effect due to the non-condensing greenhouse gases by about a factor of three; (3) the large heat capacity of the ocean and the rate of heat transport into the ocean sets the time scale for the climate system to approach energy balance equilibrium.

Not exact matches

Of course the oceans and the earth itself have a large heat capacity and will therefore respond slowly and with a delay.

The problem you'll have in extracting heat from your exhaust gases to heat your engine is twofold: Gases don't generally have a high specific heat capacity so though it's hot, it's not a lot of heat energy, and it'll take some time to heat up a large mass.

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Yes, one of the «non-linearities» we need to consider is the capacity of large mammals to lose heat at sufficient rates.

Especially in light of Prof. Zeebe comment that such a large temperature swing in such a short time would require decoupling ocean heat capacity from surface temperature, which would have required strong magic.

Heat accumulation as in (4) can take decades, because the heat capacity of the oceans is far larger than that of the atmosphHeat accumulation as in (4) can take decades, because the heat capacity of the oceans is far larger than that of the atmosphheat capacity of the oceans is far larger than that of the atmosphere.

That and its large heat capacity explains why the ocean holds much of the earth's transient climate sensitivity.

This makes sense since warming the surfaces of the world's oceans would tend to decrease their CO2 - carrying - capacity, and this would be a slow process due to the buffering effects of the specific heat capacity of these large bodies of water.

The heat capacity of the OSBL is about 10 ^ 6 as large as that in the diffusive boundary layer, as shown with this definition:

Also, keep in mind that the heat capacity of the climate system is very large.

lgl says: April 14, 2011 at 11:15 am Good, then you realize TSI is not a measure of T «C * dT / dt = dH / dt = Q - E» and «Time constant τ varies linearly with heat capacity» The longer cycles will mix more of the ocean, thus larger heat capacity and larger time constant.

Of course, this is not true of mean ocean heat capacity nor the world's mean temperature, however it may be substantial true over a 5 x 5 degree section of ocean or even a region as large as a single ocean basiOf course, this is not true of mean ocean heat capacity nor the world's mean temperature, however it may be substantial true over a 5 x 5 degree section of ocean or even a region as large as a single ocean basiof mean ocean heat capacity nor the world's mean temperature, however it may be substantial true over a 5 x 5 degree section of ocean or even a region as large as a single ocean basiof ocean or even a region as large as a single ocean basin.

Schwartz has a nice analysis of the energy balance Good, then you realize TSI is not a measure of T «C * dT / dt = dH / dt = Q - E» and «Time constant τ varies linearly with heat capacity» The longer cycles will mix more of the ocean, thus larger heat capacity and larger time constant.

Given the high thermal inertia of the ocean and it's large heat capacity, the climate can be controlled to the extent the ocean heat content can be controlled.

``... whereas the thermal lag of water by contrast is great and whilst energy is being absorbed due to its large heat capacity the response is slow...»

The deep sea has a large enough heat capacity to absorb all that heat, but just assuming that all the heat can be fed to deep ocean without changes in the rest of circulation is not realistic.

A thin sheet of metal quickly absorbs the solar energy, and having good conductivity, quickly converting it into an increase in heat whereas the thermal lag of water by contrast is great and whilst energy is being absorbed due to its large heat capacity the response is slow.

* In addition to maturity issue for the dataset, what about the fact that large (compared to the rest of the system's heat capacity) changes can result from tiny changes in temperature measurements arguably within instrumental detection limits?

«To better monitor Earth's energy budget and its consequences, the ocean is most important to consider because the amount of heat it can store is extremely large when compared to the land or atmospheric capacity,» said Yan.

A heavy ceramic cup, doesn't work as good as thermos but works slightly better than less heavy cup [more a bit more heat capacity and more insulation] But if you don't screw on the lid, a thermos works about a good as ceramic cup - preventing evaporation of the hot coffee is large factor.

But seems quite different matter to add hundreds of C as compared to tens of C. And with Earth oceans one talking much larger heat capacity.

Thanks to their large heat capacity, the oceans absorb warming caused by human activities, and more than 90 % of the Earth's extra heat from global warming is absorbed by them.

If you go down, say, to a depth of a mere 1000 meters, the diffusion of this transferred heat, over a volume of water with a heat capacity that now is some 400 times larger than the entire atmosphere, would make it 400 times more undetectable, we suppose.

In order to accomplish the high solar fraction, the system must include several days worth of heat storage for extended cloudy periods — a large storage capacity.

Given its large mass and high heat capacity, the ability of the Ocean to absorb heat is 1000 times larger than that of the atmosphere.

Realistically, the range of sensitivity should be listed as 4.5 to 0.8, because there would be a larger impact when the heat capacity is lower and there is more ice to feedback.

of the ocean with its much larger heat capacity.

A suitable large capacity heat bank could be a water tank beneath the floor of the house.

The variations are stronger because of the northern hemisphere's larger fraction of land, which has a lower heat capacity than the ocean and thus responds more quickly to variations.

It raises the question why a reputable researcher would make simplified assumptions such a single heat capacity and a single time scale for all of Earth's sphere's when there are such large differences for land surface, atmosphere and ocean, and expect it to fly.

Due to its large heat capacity, the ocean is the likely source of natural long - term climate variability on interdecadal time scales.

As happens the heat capacity of water is very large, 4.2 kJ / kg.

The ocean dominates the change in energy because of its large mass and high heat capacity compared to the atmosphere.