A comparison of the radiative equilibrium temperatures with the observed temperatures has indicated the extent to which
the other atmospheric processes, such as convection, large - scale circulation, and condensation processes, influence the thermal energy balance of the system.
Of course, this doesn't mean that much, since the «closed» system will not be open to the vacuum of space, and is not subject to
other atmospheric processes like convection and to cloud and precipitation feedbacks, all of which render the experiment fairly meaningless.
The factors that determine this asymmetry are various, involving ice albedo feedbacks, cloud feedbacks and
other atmospheric processes, e.g., water vapor content increases approximately exponentially with temperature (Clausius - Clapeyron equation) so that the water vapor feedback gets stronger the warmer it is.
Not exact matches
In advancing these theories they disregard factors universally admitted by all scientists — that in the initial period of the «birth» of the universe, conditions of temperature,
atmospheric pressure, radioactivity, and a host of
other catalytic factors were totally different than those existing presently, including the fact that we don't know how single atoms or their components would bind and consolidate, which involved totally unknown
processes and variables, as single atoms behave far differently than conglomerations of atoms.
The main objectives of this mission are to search for evidence of methane and
other trace
atmospheric gases that could be signatures of active biological or geological
processes and to test key technologies in preparation for ESA's contribution to subsequent missions to Mars.
The setting gave scientists the rare opportunity to look at the impact of pollution on
atmospheric processes in a largely pre-industrial environment and pinpoint the effects of the particles apart from
other factors such as temperature and humidity.
He wants to know whether the tendency of emitted compounds to end up as long - lived
atmospheric components is generally applicable to
other compounds and how this
process might coexist or compete with
other processes occurring in the atmosphere.
So in
other words, you know, P is going to be about 1.2, S is going to be about 2, and E, say we do super-well in efficiency, it's a 0.5, because there's a mix of things like lighting that you can do super-well, and things like making fertilizer, where you're literally, unless there's something we're not seeing, we're close to the, you know, taking
atmospheric N2 and making fertilizer's got an energy cost that — actually, those
processes are so amazing, they're within like 20 percent of what we think that minimum looks like.
There are many
other atmospheric observations and models we need to look at to see how this entire
process works.»
Her photograms are a direct record of
atmospheric conditions during the
process of their production: light, humidity, and the outside temperature, among
other factors, determine the surface of the final works.
The Humboldt Current Large Marine Ecosystem (off Chile and Peru), the Benguelan Current LME (Namibia and South Africa), the Canary Current LME (Morocco), are the
other main upwelling ecosystems, all driven by similar oceanographic and
atmospheric processes, all on the eastern sides of ocean basins (western sides of continents).
Relevant to
other discussions in this thread, rising
atmospheric CO2 tends to stimulate forest growth and CO2 uptake, thus mitigating
atmospheric CO2 increases, although this
process is impeded in areas subject to drought.
Depending on what they are used for, models can also include interactive
atmospheric chemistry, ocean biology, and
other processes.
Putting those two, theoretical,
processes together with some shaky assumptions about aerosols, clouds and
other atmospheric phenomena, and arriving at an assumption that the theoretical minor warming of CO2 is tripled is what concerns a true skeptic.
temperature,
other climatic variables, and concentrations of aerosols and trace gases; and (2) making raw and
processed atmospheric measurements accessible in a form that enables a number of different groups to replicate and experiment with the
processing of the more widely disseminated data sets such as the MSU tropospheric temperature record.
To produce a weather forecast we need to model the dynamics of the atmosphere and the physical
processes that occur, such as the formation of clouds, and the
other processes in the Earth system that influence the weather such as
atmospheric composition, the marine environment and land
processes.
3 Further complicating the response of the different
atmospheric levels to increases in greenhouse gases are
other processes such as those associated with changes in the concentration and distribution of
atmospheric water vapor and clouds.
How do theories for the Hadley circulation and for
atmospheric macroturbulence based on dry dynamics need to be modified in the presence of moist
processes, which alter, among
other things, the effective static stability of the atmosphere?
«Understanding what drives the meteorology on Saturn, and in general on gaseous planets, has been one of our cardinal goals since the inception of the Cassini mission,» said Carolyn Porco, imaging team lead, based at the Space Science Institute, Boulder, Colo. «It is very gratifying to see that we're finally coming to understand those
atmospheric processes that make Earth similar to, and also different from,
other planets.»
JW comment — What is in debate is the
process (my words above) has a net effect on
atmospheric temperatures when all
other atmospheric conditions and
processes are involved.
Thus, at least for the spring season, it seems unnecessary to invoke
processes other than the
atmospheric circulation to explain trends in Antarctic sea ice.
States that
other feedbacks likely to emerge are those in which key
processes include surface fluxes of trace gases, changes in the distribution of vegetation, changes in surface soil moisture, changes in
atmospheric water vapor arising from higher temperatures and greater areas of open ocean, impacts of Arctic freshwater fluxes on the meridional overturning circulation of the ocean, and changes in Arctic clouds resulting from changes in water vapor content
-- the
atmospheric concentration of CO2 and
other GHG's; — the reflective & absorptive characteristics, as a function of wavelength, for the GHG's; — the specific heat and mass of the earth's intermediate - term heat - storage media — the oceans (primarily) and the atmosphere; — the quantity of heat absorbed by phase - changes = ice - melt; and by chemical / biological
processes.
Other applications of past geomagnetic field reconstructions include investigations of
atmospheric ionisation by galactic cosmic rays (e.g., Usoskin et al. 2008, 2010) or in - situ cosmogenic nuclide production rates to study Earth surface
processes (e.g., Pigati & Lifton 2004; Lifton et al. 2008).
Catalytic hydrotreating: A refining
process for treating petroleum fractions from
atmospheric or vacuum distillation units (e.g., naphthas, middle distillates, reformer feeds, residual fuel oil, and heavy gas oil) and
other petroleum (e.g., cat cracked naphtha, coker naphtha, gas oil, etc.) in the presence of catalysts and substantial quantities of hydrogen.
Terrestrial radiation absorbed by CO2 is immediately thermalized, i.e. the radiant energy absorbed by CO2 molecules is immediately (about 0.1 nanosecond) transferred (in a
process similar to thermal conduction) to
other atmospheric molecules which outnumber CO2 molecules 2500 to 1.
Authors conclude from this and
other evidence from
process models that warmer climates may enhance tropical forest release of CO2, thus accelerating
atmospheric CO2 accumulation through a positive feedback.
As we still don't know how nature put us in ice ages (yes we have the overall picture, but not the details for a model) or get us out again, and what
other effects there are from altered
atmospheric chemistry we really do not know how the mean of the chaotic
process might change in the future.
While this is true, the
atmospheric model used to generate the reanalysis must by - pass this shortcoming by letting
other resolved
processes provide a means for the unresolved flux of energy, mass, and momentum.
Collaboration in evaluation of the statistical results by VS (and
others) and the evaluation of the potential physical possibilities by physicists represent an opportunity to add to our understanding of our
atmospheric process.