Citaat:
Oorspronkelijk geplaatst door parcifal
Goed begonnen, maar verre van compleet.
Je moet ook nog het stralingsenergie budget opmaken, de relatieve kracht van co2, hoelang co2 actief blijft in de atmosfeer.
er zijn trouwens modellen om daarmee te spelen, nog nooit gedaan?
Modtran bvb. Moet je maar eens naar vragen bij patrickve, dat is de echte specialist ter zake. 
Aha teruggevonden, hier dus : http://modtran5.com/
Of hier gratis : http://climatemodels.uchicago.edu/modtran/ |
Generally speaking, water vapor is the single most important atmospheric absorber in the IR band..
No other atmospheric constituent is better known to the general public as a “greenhouse gas” than CO2. In actuality, water vapor has a larger overall impact on the radiative energy budget of the atmosphere..
A First Course in Atmospheric Radiation, Grant Petty, Sundog Publishing (2006)
Water vapor is the most important gas for the transfer of radiation in the atmosphere..
Global Physical Climatology, Hartmann, Academic Press (1994)
Table 6 shows the relative contributions of H2O, CO2 and O3 to reducing the outgoing longwave flux, from which it is seen that the longwave effect of H2O is significantly larger than the effects of CO2 and O3..
Climate Modeling through Radiative-Convective Models, Ramanathan & Coakley, Reviews of Geophysics and Space Physics (1978)
The importance of water vapor in regulating climate is undisputed. It is the dominant greenhouse gas, trapping more of Earth’s heat than any other gaseous constituent..
The Radiative Signature of Upper Tropospheric Moistening, Soden, Jackson, Ramaswamy, Schwarzkopf & Huang, Science (2005)
The authors find that for the clear sky case the contribution due to water vapor to the total longwave radiative forcing is 75 W/m², while for carbon dioxide it is 32 W/m²..
Earth’s Annual Global MeanEnergy Budget, Kiehl & Trenberth, Bulletin of the American Meteorological Society (1997)
Voila, ik moet die grafiekjes zelfs niet ontleden. Deze mensen hebben dit voor mij gedaan.