It is the physical basis for calculating and analyzing
the radiation energy balance of Earth.
During the second study period, the team also measured emissions of methane in order to calculate its influence on the wetlands»
radiation energy balance.
Not exact matches
When the team looked at the overall
balance between the
radiation upward from the surface of the ice sheet and the
radiation both upward and downward from the upper levels of the atmosphere across all infrared wavelengths over the course of a year, they found that in central Antarctica the surface and lower atmosphere, against expectation, actually lose more
energy to space if the air contains greenhouse gases, the researchers report online and in a forthcoming Geophysical Research Letters.
The findings should explain how the multicomponent aerosols affect clouds, solar
radiation and ultimately the earth's global climate and
energy balance.
Clouds alter the amount of sunlight, or
radiation, that can reach Earth, affecting Earth's
energy balance, and in some areas can lead to precipitation.
The clouds affect the «global radiative
balance» by reflecting solar
energy or trapping terrestrial
radiation.
Surface radiative
energy budget plays an important role in the Arctic, which is covered by snow and ice: when the
balance is positive, more solar
radiation from the Sun and the Earth's atmosphere arrives on the Earth's surface than is emitted from it.
[Response: The way the
radiation is written in the Uvic model — which is typical for
energy balance models of this sort — you can dial in whatever sensitivity parameter you want.
But what's important to note is that orgonite doesn't change the EMF
radiation per se, but changes the underlying negative Orgone (Chi, Prana, Life Force)
energy into
balanced and positive
energy.
This page outlines a map of assessment through the unit, including skill based questions, short writing responses and extended writing responses including essays.The atmospheric system, including the natural greenhouse effect and
energy balance (incoming shortwave
radiation and outgoing long wave
radiation) Changes in the global
energy balance, and the role of feedback loops, resulting from: Glossary - Student should make...
An
energy surplus there gives rise to warming which causes a rise in infra - red
radiation leading to more
energy loss at the top of the atmosphere and hence a trend back into
energy balance (negative feedback).
However, the other terms in the
energy balance directly or indirectly affect the amount of absorbed solar
radiation which is available for ablation.
Detailed studies of the
energy balance and ablation of the Zongo and Chacaltaya glaciers support the importance of air temperature increase, and identify the increase in downward infrared
radiation as the main way that the effect of the warmer air is communicated to the glacier surface [Wagnon et al. 1999; Francou et al, 2003].
They don't have to be scientists to understand that the higher
energy waves of visible light from the Sun can penetrate through CO2, H2O, CH4, NOZ etal in the atmosphere, but the lower
energy radiation of infra - red waves, from Earth's surface, have problems getting back out through these molecules, and a new
energy balance has to be established in the form of rising temperature.
Perhaps there is room for more indicators inspired by the «big picture physics», such as the planetary
energy balance and the outgoing long - wave
radiation (OLR).
What happens at the «top of atmosphere» — the level where outgoing
radiation leaves for space, not itself a very easy concept — is the restoration of equilibrium, the increase in temperature that, through Helmholtz - Boltzmann at the Earth's brightness temperature 255K, restores the
balance between incoming and outgoing
energies.
Earth's
energy balance In response to a positive radiative forcing F (see Appendix A), such as characterizes the present - day anthropogenic perturbation (Forsteret al., 2007), the planet must increase its net
energy loss to space in order to re-establish
energy balance (with net
energy loss being the difference between the outgoing long - wave (LW)
radiation and net incoming shortwave (SW)
radiation at the top - of - atmosphere (TOA)-RRB-.
This is because part of the outgoing
radiation signal (albeit small) is emerging from relatively warm layers aloft, and thus slightly less emission is demanded from the troposphere in order to satisfy planetary
energy balance.
In equilibrium to maintain the
energy balance of the earth you must have just as much long wave
radiation passing through (and warming) the top layer as before.
To bring more
energy into the system, that surface warming would have to cause the top - of - the - atmosphere
radiation balance to change positively, but that would add to warming, amplifying the initial perturbation and leading to a runaway instability.
So to maintain
energy balance the stratosphere must be losing
energy via long wavelength
radiation which means long wavelength emitters like CO2 must be radiating more than they are absorbing.
Covers earth - sun relationships,
radiation and
energy balances, microclimatology, and includes some math.
I ask because my limited understanding is that temperature is related to kinetic
energy, but would not register an overall increase in potential
energy, in which case
energy from the sun could be partitioned in heat
energy emitted from the planet and work used to increase potential
energy, possibly allowing an
energy balance that does not require a
radiation balance, and also does not require a warming effect.
The general argument however is being discussed by rasmus in the context of planetary
energy balance: the impact of additional CO2 is to reduce the outgoing longwave
radiation term and force the system to accumulate excess
energy; the imbalance is currently on the order of 1.45 * (10 ^ 22) Joules / year over the globe, and the temperature must rise allowing the outgoing
radiation term to increase until it once again matches the absorbed incoming stellar flux.
The Stephens et al paper is a very incremental change from previous estimates of the global
energy balances — chiefly an improvement in latent heat fluxes because of undercounts in the satellite precipitation products and an increase in downward longwave
radiation.
Pekka Pirilä: Where the effect of increase in CO2 is important for the
energy balance is in the upper troposphere, because a significant part of the
radiation emitted upwards by CO2 of the upper troposphere goes trough the tropopause to stratosphere or through it to open space.
I support his findings on the basis that convective changes will always adjust the
balance between
radiation and conduction within the Earth system so as to match
energy out to space with
energy in from space.
Dynamical upward transport by convection removes excess heat from the surface more efficiently than longwave
radiation is able to accomplish in the presence of a humid, optically thick boundary layer, and deposits it in the upper troposphere where it is more easily radiated to space, thereby affecting the planetary
energy balance.
Physics says the
energy into a system must equal the
energy out once in
balance, The heat in the oceans is what must be there to produce enough heat
radiation out to space through the air / GHG blanket.
The
energy balance is more sensitive to the troposphere temperature than the tropopause which is a boundary that doesn't move much because the
radiation is coming from the troposphere as a whole.
Where the effect of increase in CO2 is important for the
energy balance is in the upper troposphere, because a significant part of the
radiation emitted upwards by CO2 of the upper troposphere goes trough the tropopause to stratosphere or through it to open space.
In particular, the authors find fault with IPCC's conclusions relating to human activities being the primary cause of recent global warming, claiming, contrary to significant evidence that they tend to ignore, that the comparatively small influences of natural changes in solar
radiation are dominating the influences of the much larger effects of changes in the atmospheric greenhouse gas concentrations on the global
energy balance.
Lacis points out that only outgoing
radiation can
balance the global
energy budget of the Earth; as clearly the convection and conduction ends at the boundary of the atmosphere.
The evolving
radiation balance of the earth as seen in the satellite data shows that the
energy added by the CO2 and feedbacks is more than sufficient to explain the observed warming surface temperatures.
«the tendency to a radiative equilibrium means that the emitter with the higher surface temperature will loose
energy due to a negative net
radiation balance until this net
radiation balance becomes zero.»
It clearly states that (a) emission of
energy by
radiation is accompanied with cooling of the surface (if no compensating changes prevent it), and (b) the tendency to a radiative equilibrium means that the emitter with the higher surface temperature will loose
energy due to a negative net
radiation balance until this net
radiation balance becomes zero.
That claim is too simple to be useful, ignoring a) the complex interaction of Boltzmann
radiation with the surface, the clouds, the GHGs, and the like, and b) the various regimes in the tropics, each of which modifies and changes the overall
energy balance by things like convection and latent heat transfer.
There more CO2 leads to a change in the altitude of the level whose
energy balance is controlled by
radiation without a significant convective component.
This is an
energy balance constraint due to the effectiveness of
radiation in removing excess surface
energy above the
balanced state, seen for example just after El Ninos as the surface temperature anomaly cools within a year.
Over land, you have a surface
energy balance that includes downwelling IR, upwelling IR (Stefan Boltzmann), downwelling solar
radiation minus what is reflected back from the surface, latent heat flux and sensible heat flux (these are turbulent fluxes associated with exchange with the atmosphere), and conductive flux from the ground (below the surface).
Because the climate system derives virtually all its
energy from the Sun, zero
balance implies that, globally, the amount of incoming solar
radiation on average must be equal to the sum of the outgoing reflected solar
radiation and the outgoing thermal infrared
radiation emitted by the climate system.
Until the surface warms to a level that emits
radiation at a rate that is
balanced with the higher level of
energy capture there will continue to be «net
energy capture».
In the heat -
energy balance, which describes the gain or loss of heat in the system, sketched in figure 5, the solar and atmospheric
radiation terms dominate.
He was right that surface temperature is determined by the
balance between incoming solar
energy and outgoing infrared
radiation, and that the
balance that matters is the
radiation budget at the top of the atmosphere.
The final temperature the earth attains represents a
balance between the amount of
radiation reflected back and the temperature increase due to that reflection of
energy.»
However there is no law that says radiative transfers have to
balance, in fact we know from the law of conservation of
energy that this isn't the case: a solar panel has no radiative equilibrium because the incoming
radiation is converted into heat.
And that to use it as an example or reason why we are thus NOT affecting the earth through a multi million year change in long lived atmospheric greenhouse gases — which absorb and re radiate thermal
radiation, slowly increasing the
energy balance of the earth — is irrational.
«Because the solar - thermal
energy balance of Earth [at the top of the atmosphere (TOA)-RSB- is maintained by radiative processes only, and because all the global net advective
energy transports must equal zero, it follows that the global average surface temperature must be determined in full by the radiative fluxes arising from the patterns of temperature and absorption of
radiation.»
Was it taking the 390 W / m2 of back
radiation in common
energy balance charts and calculating from that the upward pressure and therefore the volume expansion?
The job of the
radiation module is to calculate the solar heating rate profiles and the thermal cooling rate profiles, including the
energy deposition at the ground surface, as well as the
energy balance at the top of the atmosphere for the specified climate variable distribution at each grid box.