There is also
a cloud radiative component.
Not exact matches
Or does he perhaps mean that slow
components, like the ocean, modulate the
clouds, and the resulting
cloud radiative forcing amplifies or damps the resulting interannual or decadal variability?
If he succeeds in showing that there is negligible
radiative forcing present, then Dessler 2010 is defended, and he can move on and easily address and dismiss the secondary question — whether or not there was a
CLOUD forcing
component involved.
The second is that it rebutts Dessler 2010, who used a zero - lag regression of flux derivative for clear - sky and all - sky data, under a stated assumption of no significant
radiative forcing
component during the period 2000 to 2010, to conclude that
cloud feedback really is positive.
Motivated by findings that major
components of so - called
cloud «feedbacks» are best understood as rapid responses to CO2 forcing (Gregory and Webb in J Clim 21:58 — 71, 2008), the top of atmosphere (TOA)
radiative effects from forcing, and the subsequent responses to global surface temperature changes from all «atmospheric feedbacks» (water vapour, lapse rate, surface albedo, «surface temperature» and
cloud) are examined in detail in a General Circulation Model.
In all calculations of A, TA, t A, and of the
radiative flux
components, the presence or absence of
clouds was ignored; the calculations refer only to the greenhouse gas
components of the atmosphere registered in the radiosonde data; we call this the quasi-all-sky protocol.
In all calculations of A, TA,, and of the
radiative flux
components, the presence or absence of
clouds was ignored; the calculations refer only to the greenhouse gas
components of the atmosphere registered in the radiosonde data; we call this the quasi-all-sky protocol.
The direct and indirect
radiative effects of aerosols suspended in the atmosphere above
clouds (ACA) are a highly uncertain
component of both regional and global climate.
For a comprehensive GCM I can count oceans, land, atmosphere, ice, biological processes, organic and inorganic chemical processes, human - made sources and other effects,
radiative energy transport, conduction and convective heat transfer, phase change,
clouds and aerosols, as some of the important system
components, phenomena, and processes.