Among them, he said, are natural variations in the climate and rising trade winds that have helped funnel
atmospheric heat into the ocean.»
These models predicted that the Northern Hemisphere Polar region would warm fastest and first, that the Southern Ocean would draw a greater portion of
atmospheric heat into the ocean system, and that land ice melt near Greenland and West Antarctica would generate cold, fresh water flows into the nearby ocean zones and set off localized cooling.
Not exact matches
A mighty
atmospheric river, fueled by water vapor from the Amazon and
heat from the sun, flows across South America until it reaches the Andes and condenses
into rain.
Together, they describe variations in
atmospheric heat and moisture, and how those translate
into weather patterns.
That
heated surface air then rose
into the
atmospheric boundary layer — the lowest level of the troposphere — doubling its height to more than 4 kilometers, and creating a thick blanket of
heat.
Instead of dissipating
into space, the infrared radiation that is absorbed by
atmospheric water vapor or carbon dioxide produces
heating, which in turn makes the earths surface warmer.
The takeaway is that if humanity stopped cranking out greenhouse gases immediately, sea levels would still rise for centuries before the
heat dissipates through Earth's atmosphere and
into space, says study co-author Susan Solomon, an
atmospheric scientist at MIT.
But it is a complicated picture: the effect that extra
atmospheric CO2 has in these kind of experimental setups might not reflect its effects in the real world, where other factors — such as elevated
heat, or changes in precipitation — come
into play.
That could allow
heat from the ocean to be released
into the atmosphere — causing a jump in
atmospheric global warming, Trenberth says: «This could be a very important year.»
The effect of
atmospheric cooling due to an AMOC collapse is associated with
heat flow from the atmosphere
into the ocean, which has been witnessed during the climate hiatus of the last 15 years.
Under extreme pressure, black phosphorus is transformed
into a simple cubic form, so the team wondered if the same could be done to GeSe and
heated the abundant alpha - GeSe form of the compound to 1200 °C under 6 GPa of pressure or 60,000 times
atmospheric pressure.
More than 90 % of global warming
heat goes
into warming the oceans, while less than 3 % goes
into increasing the
atmospheric and surface air temperature.
For as much as
atmospheric temperatures are rising, the amount of energy being absorbed by the planet is even more striking when one looks
into the deep oceans and the change in the global
heat content (Figure 4).
By trapping
heat, rising concentrations of
atmospheric pollution are causing glaciers and ice sheets to melt
into seas, lifting high tides ever higher.
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.
The standard assumption has been that, while
heat is transferred rapidly
into a relatively thin, well - mixed surface layer of the ocean (averaging about 70 m in depth), the transfer
into the deeper waters is so slow that the
atmospheric temperature reaches effective equilibrium with the mixed layer in a decade or so.
Hypothesis A — Because the
atmospheric radiation is completely absorbed in the first few microns it will cause evaporation of the surface layer, which takes away the energy from the back radiation as latent
heat into the atmosphere.
The 2 Gton / yr net CO2 invasion
into the ocean is driven by the rising
atmospheric concentration, not by water flow or
heat fluxes or anything like that.
The vast majority of research in recent decades on the carbon dioxide buildup has been focused on the
atmospheric impacts of the accumulating greenhouse - gas blanket even though the vast majority of the
heated trapped by these gases has gone first
into the seas — and the drop in seawater pH driven by CO2 has been a clear signal of substantial environmental change.
As
atmospheric temperatures increase, therefore,
heat transfer
into the oceans increases as the system tends towards a new equilibrium temperature.
Thus, if the absorption of the infrared emission from
atmospheric greenhouse gases reduces the gradient through the skin layer, the flow of
heat from the ocean beneath will be reduced, leaving more of the
heat introduced
into the bulk of the upper oceanic layer by the absorption of sunlight to remain there to increase water temperature.
Reflectiveity versus the insolative mid-tropospheric
heating that can result versus the tendency to reduce terrestrial IR re-emission
into space seem to be the three primary characteristics of clouds in relation to surface and
atmospheric temperatures.
So if there were, say, a decadal - scale 1 % -2 % reduction in cloud cover that allowed more SW radiation to penetrate
into the ocean (as has been observed since the 1980s), do you think this would have an impact of greater magnitude on the
heat in the oceans than a change of, say, +10 ppm (0.00001) in the
atmospheric CO2 concentration?
It rises till it emits energy to lower energy dense regimes above — they strap a big cooling fin to the top in the computer of course, the
heat is washed / radiated off
into the room and beyond; and in the storm system the
heat is given off toward higher
atmospheric regions and ultimately space
More than 90 % of global warming
heat goes
into warming the oceans, while less than 3 % goes
into increasing the
atmospheric and surface air temperature.
where latent
heat release and net radiation
into the
atmospheric column, R, balance
heat divergence, and the relatively weak contribution from sensible
heat transport from the land surface to the
atmospheric column has been neglected.
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?
2)-- We can't detect the rise because the additional
atmospheric heat energy is somehow being transmitted
into the oceans.
What I have written is that the climastrologist's claim that the so - called «missing»
atmospheric heat has somehow found its way DIRECTLY
into the oceans, and that such a transfer is impossible.
For as much as
atmospheric temperatures are rising, the amount of energy being absorbed by the planet is even more striking when one looks
into the deep oceans and the change in the global
heat content (Figure 4).
Pacific trade winds, for instance, which have been unusually strong for the past two decades thanks to a 20 - to 30 - year cycle called the Interdecadal Pacific Oscillation, have been pumping
atmospheric heat down
into the western Pacific.
If we continue emitting large amounts of CO2 while we work towards converting to 3/4 solar power and survive the
heating that we inadvertently speed up by reflecting more
heat into an atmosphere already overburdened with reflective -
heat - capturing CO2, some day in the future when the
atmospheric CO2 returns to its natural percentage of 0.0300 % instead of today's extremely high 0.03811 % the world will cool down to the levels that nature intended.
His reference to the oceans» role as a sink for CO2 and
heat is significant in the present debate about the apparent slight slow - down in the pace of
atmospheric warming and the likelihood that the
heat is going
into the oceans instead.
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.
The surface temperature response, T, to a given change in
atmospheric CO2 is calculated from an energy balance equation for the surface, with
heat removed either by a radiative damping term or by diffusion
into the deep ocean.
Not all at once of course, but as mentioned above, when the PDO goes positive, we can likely expect a significant change in the
atmospheric heat content as
heat energy is transferred from the deep oceans back
into the atmosphere.
By trapping
heat, rising concentrations of
atmospheric pollution are causing glaciers and ice sheets to melt
into seas, lifting high tides ever higher.
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.»
The 490 ppm CO2e number — due to added
atmospheric heating contributions from human - emitted gasses like methane, chlorofluorocarbons, NOx compounds, and others — is enough to catapult our current climate context
into the upper Middle Miocene range.
El Nino events tend to cause
atmospheric warming because they are transporting
heat from the ocean back
into the atmosphere.
What is ACTUALLY happening now is that the
atmospheric greenhouse effect is getting stronger; and at the same time the circulations of water and air and
heat and cloud and so on around the globe are going on their merry chaotic way, meaning that we are going to have unpredictable short term variations while there is a continual flow of
heat into the ocean from the energy imbalance between what is being emitted and what is being absorbed.
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.
Because the
atmospheric radiation is completely absorbed in the first few microns it will cause evaporation of the surface layer, which takes away the energy from the back radiation as latent
heat into the atmosphere.
Process - based studies have focused on understanding the role of the land surface on climate, with research looking
into the regional impact of historical or hypothetical (future scenario) land - use change on climate, as well as understanding diurnal - scale relationships between surface fluxes of
heat and moisture and subsequent
atmospheric processes such as convection and the generation of precipitation.
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.
Alan, Have you ever looked
into the role massive deployment of wind turbines might play in affecting
atmospheric circulation and thus
heat transfer to and from outer space.
As
atmospheric concentrations of greenhouse gases increase, the Earth system is warming, and over 90 percent of that increase in
heat goes
into the ocean.
For the real earth, with a significant
heat capacity and significant
atmospheric and ocean transport, the one summary number that has meaning is the average of T ^ 4 over the surface of the earth... That is what is going to go
into determination of the global surface radiative balance.
A bit of digression, but can
atmospheric warming have «stalled» because of the enormous emission of reflective aerosols from coal burning in China and India in the last decade or so?p class =» response» > [Response: In principle yes, but the evidence that more
heat has gone
into the ocean is very strong.
I think it is really important to make that distinction - that there are a number of factors that influence the extent of Arctic sea ice, some of them of course associated with changes in the radiative forcing from the atmosphere, as a result of anthropogenic greenhouse gases and aerosols, but also changes in the
atmospheric circulation and also the advection of
heat into or out of the Arctic by the ocean circulation.