Over time, CO2 and
other atmospheric components would remain stable until energy is switched over world - wide.
The exact amount of this temperature increase, however, remains uncertain because of unpredictable changes in
other atmospheric components, especially cloud cover.
And there is, of course, some CO2, which is dissipated out to space along with
other atmospheric components, although I have seen no good estimates of this.
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.
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.
Antarctic climate results from a complex mix of oceanic and
atmospheric circulation patterns, so there could also be
other components affecting the amount of snow accumulation in the region, Bromwich said.
Musk says it can be rapidly reused up to 10 times (basically just refilling the fuel tanks), and then it needs to be serviced properly (probably to check the heat shielding and
other components that are stressed during
atmospheric reentry).
A 2015 USDA report (Brown et al. 2015) on how climate affects agriculture delineates the sensitivities of specialty crops to many climate
components (e.g., temperatures,
atmospheric CO2 levels, water supply, cloud and light conditions, high winds and
other extreme conditions).
[Response: At the dawn of coupled modelling, errors that arose in separate developments of ocean and
atmospheric models lead to significant inconsistencies between the fluxes that each
component needed from the
other, and the ones they were getting.
[Equilibrium] climate sensitivity is defined as the increase in global mean surface temperature (GMST), once the ocean has reached equilibrium, resulting from a doubling of the equivalent
atmospheric CO2 concentration, being the concentration of CO2 that would cause the same radiative forcing as the given mixture of CO2 and
other forcing
components.
Radiative transfer codes that accurately calculate the radiative impact of greenhouse gases and
other atmospheric constituents are an essential
component of the global climate models used to simulate present and future climate.
The
other component needed to make the system complete is an equally micron sized and equally accurate factory acting as a fuel cell, consuming sugar &
atmospheric oxygen and producing electricity on demand while releasing carbon dioxide & water to the environment.
He deduced that the cooperation of these gases has to take the form of an optimal
atmospheric transmittance window for infrared radiation, such that if the concentration of one gas, say carbon dioxide, varies and changes
atmospheric transmittance, the
other components, such as water vapor, will have to compensate for it by changing their concentrations.
In one of our 1995 papers (see above for reference and description) we produced 6 models with 3 of them assuming the recent rise in
atmospheric CO2 concentration has a significant anthropogenic
component and the
other 3 assuming there was no significant anthropogenic
component.
There are no analogous greenhouse
components for the
other gases or
atmospheric factors.
I do need to check whether all of the 78 W / m ^ 2 is said to be absorbed in the absorption wavelengths of GHGs or whether some of this is
component is absorbed in the absorption wavelenghts of
other gases and / or by
atmospheric aerosols.
Called ModelE, it provides the ability to simulate many different configurations of Earth System Models — including interactive
atmospheric chemistry, aerosols, carbon cycle and
other tracers, as well as the standard atmosphere, ocean, sea ice and land surface
components.
The term Earth System Model is a little ambiguous with some people reserving that for models that include a carbon cycle, and
others (including me) using it more generally to denote models with more interactive
components than used in more standard (AR4 - style) GCMs (i.e.
atmospheric chemistry, aerosols, ice sheets, dynamic vegetation etc.).