It seems to me that the two papers use at least a similar approach — and one that seems very sensible to me — correlating surface temperature
with radiation fluxes at the top of the atmosphere.
Not exact matches
Our best guess is that the lower
flux of ultraviolet
radiation during the winter, along
with the sun - blocking effect of the ring shadows on the winter hemisphere, reduces the production of the overlying haze.
The correlation we observed is compatible
with the hypothesis that the highest - energy particles originate from nearby extragalactic sources whose
flux has not been substantially reduced by interaction
with the cosmic background
radiation.
With this relatively slow movement, the megnetic
flux lines were of a more congruent, harmonious pattern offering the best protection against the solar
radiation.
ocean system is associated
with an amplified increase in arctic surface air temperature, downward longwave
radiation, and net heat
flux.
-- The aforementioned empirical determinations of climate sensitivity are much more consistent
with each other if the contribution of the cosmic ray
flux / cloud cover effect is included in the
radiation budget.
In that survey, it was almost universal that groups tuned for
radiation balance at the top of the atmosphere (usually by adjusting uncertain cloud parameters), but there is a split on pratices like using
flux corrections (2 / 3rds of groups disagreed
with that).
Physically, the extra GHG is causing a reduction in the total outgoing
radiation at a certain T, and so the planet must warm to re-satisfy radiative equilibrium
with the absorbed incoming stellar
flux.
The warming of the world ocean is associated
with an increase in global surface air temperature, downward longwave
radiation, and therefore net heat
flux.
Refraction, specifically the real component of refraction n (describes bending of rays, wavelength changes relative to a vacuum, affects blackbody
fluxes and intensities — as opposed to the imaginary component, which is related to absorption and emission) is relatively unimportant to shaping radiant
fluxes through the atmosphere on Earth (except on the small scale processes where it (along
with difraction, reflection) gives rise to scattering, particularly of solar
radiation — in that case, the effect on the larger scale can be described by scattering properties, the emergent behavior).
Finally, going back to Bryan's remark, he is certainly correct that the physical heat flow generated at ridges etc is tiny
with respect to the
flux of SW
radiation.
ocean system is associated
with an amplified increase in arctic surface air temperature, downward longwave
radiation, and net heat
flux.
So actually the local
radiation field is much simpler that what you're trying to describe: in the transparent windows, it's just the emitted intensity from the source (sun + ground), and in the opaque lines, it is nearly isotropic
with the excitation temperature of the molecules close to the local kinetic temperature if collisions are numerous enough,
with a small anisotropy linked to the net
radiation flux.
If it is in an isothermal layer, it will radiate upward as much as downward; it will decrease the baseline TRPP net
flux and increase the baseline TOA
flux by the same amount, but it will decrease the baseline TOA
flux by a greater amount if it is absorbing
radiation with a higher brightness temperature from below (the baseline upward
flux at TRPP), so it will increase the amount by which the baseline net
flux at TRPP is greater than that at TOA.
The calculations estimate the reduction in the energy
flux density
with distance away from the sun (Gauss» theorem) and the black body
radiation describing the rate of planetary heat loss.
Recent accurate laboratory measurements of the absorption in the CO2 band by CLOUD (1952) were used to calculate the
radiation flux in the atmosphere
with the aid of the MIDAC high speed digital computor.»
Within a convecting layer, convective
fluxes can also be part of the response, but where convection is bounded within a layer, the layer as a whole must respond
with radiation to radiative forcings and feedbacks.)
Our observational studies (Gray and Schwartz, 2010 and 2011) of the variations of outward
radiation (IR + albedo) energy
flux to space (ISCCP data) vs. tropical and global precipitation increase (from NCEP reanalysis data) indicates that there is not a reduction of global net
radiation (IR + Albedo) to space which is associated
with increased global or tropical - regional rainfall.
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).
A SOM is much cheaper and simpler to run compared to a full ocean model, but still reacts to things happening in the atmosphere, like changes in downwelling
radiation or
fluxes associated
with surface wind.
Sea ice
with its strong seasonal and interannual variability (Fig. 1) is a very critical component of the Arctic system that responds sensitively to changes in atmospheric circulation, incoming
radiation, atmospheric and oceanic heat
fluxes, as well as the hydrological cycle1, 2.
Temperature at 100hPa changes at 20 ° -30 ° latitude in both hemispheres
with the change in solar
radiation as represented by 10.7
Flux.
Bill Gray has a favorite diagram, taken from a 1985 climate model, showing little nodules in the center
with such labels as «thermal inertia» and «net energy balance» and «latent heat
flux» and «subsurface heat storage» and «absorbed heat
radiation» and so on, and they are emitting arrows that curve and loop in all directions, bumping into yet more jargon, like «soil moisture» and «surface roughness» and «vertical wind» and «meltwater» and «volcanoes.»
We checked this assumption by comparing TEC obtained at three selected sites in Europe (cf. http://swaciweb.dlr.de)
with the solar activity dynamics represented by the radio
flux index F10.7 which is also a proxy for EUV
radiation changes (see Fig. 6).
In Chapter 5 there are steady state measurements of Ar / N2, CO2 / N2 and O2 / N2; along
with photosynthetic
radiation flux.
In all of these simple models, we assume the atmosphere to have a volume as fixed as a bathtub, we assume that the atmosphere / ocean system is a closed system, we assume that the incoming
radiation from the Sun is constant, we assume no turbulence, we assume no viscosity, we assume radiative equilibrium
with no feedback lag, we take no account of water vapor
flux assuming it to be constant, no change in albedo from changes in land use, glacier lengthening and shortening, no volcanic eruptions, no feedbacks from vegetation.
The
flux of heat from the ground, however, can not keep up
with radiation cooling if the sky is clear.
Certain things come out of it easily, such as the concept of black body
radiation and balance of energy
flux with energy density in a cavity (for example).
In contrast to this, the calculated TOA outgoing
radiation fluxes from 11 atmospheric models forced by the observed SST are less than the zero feedback response, consistent
with the positive feedbacks that characterize these models.
The climate models create ~ 66 % more than real lower atmosphere warming by the fake «back
radiation» idea, taught in US Atmospheric Science for ~ 50 years, coupled
with the fake single -18 deg C OLR emitter idea, which provides an imaginary negative Down
flux in the bowdlerised two - stream approximation (blame Sagan for this).
A significant
flux of solar
radiation was found to penetrate the entire thickness of the atmosphere,
with the amount at the ground 1.5 % of that incident on the top of the atmosphere.
Maps of the long - term monthly and annual means of the net surface energy
flux together
with the four components of the total
flux (latent heat
flux, sensible heat
flux, incoming
radiation, and outgoing
radiation) for the global oceans are presented.
It might help you if you had a few concepds in mind too when considering this subject, like «space» is the big energy «sink»
with old sol (and the internal heat generating processes (including nuclear) of the earth) as sources... any mechanism that results in a delay of energy leaving earth, such as a «bounce - back» or a re-rad of energy (like back
radiation) certainly is going to increase the «energy
flux» in the system, and this in any way you want to frame the argument translates to a «higher» energy state, and a higher so - called temperature» (movement in matter, velocity of air molecules or oscillations in certain «resonant molecules) as well.
This is an appalling failure of basic teaching because it leads directly to the «back
radiation» myth, confusing Emittance
with a real energy
flux.
In other words, a bigger share of the 240 W / m 2 of the vertical energy transport will be transported by convective / advective means
with a stronger GHE, and a smaller share by radiative means because the sum of convective vertical energy transport plus the diminished radiative
flux must add up to about 240 W / m 2 in order to balance the incoming shortwave
radiation.
Since the intensity of infrared
radiation increases
with increasing temperature, one can think of the Earth's temperature as being determined by the infrared
flux needed to balance the absorbed solar
flux.
The 2008 K&T cartoon gives a NET upward
radiation flux from the surface of 33w / m2
with a downward adjustment to water vapour to 76w / m2 and conduction to 16w / m2 but the point holds; that point is more net heat is leaving the surface through methods other than
radiation, particularly water; that to me means 2 things; water is a dominant mover of heat compared to CO2 and the sun's 168/166 w / m2 is a far more dominant heater than CO2 backradiation.
Part Three — Kinetic Energy — why kinetic energy can not be equated
with flux (
radiation in W / m ²), and how equation 7 is invented out of thin air (
with interesting author comment)
With this relatively slow movement, the megnetic
flux lines were of a more congruent, harmonious pattern offering the best protection against the solar
radiation.
The study includes an estimate of the effect of the observed stratospheric water decadal decrease by calculating the
radiation flux with and without the change, and comparing this to the increase in CO2 forcing over the same period.
The team examined data on carbon - dioxide
flux, evapotranspiration, sensible heat, air temperature, net
radiation and photosynthetic active
radiation from five FLUXNET grassland sites in Canada, the US and Hungary, along
with leaf - area index information derived from satellite data.