Your statement that «Thus it is natural to look at the real world and see whether there is evidence that it behaves in the same way (and it appears to, since model hindcasts of past changes match observations very well)» seems to indicate that you think there will be no changes in ocean circulation or land use trends, nor
any subsequent changes in cloud responses thereto or other atmospheric circulation.
Your statement that «Thus it is natural to look at the real world and see whether there is evidence that it behaves in the same way (and it appears to, since model hindcasts of past changes match observations very well)» seems to indicate that you think there will be no changes in ocean circulation or land use trends, nor
any subsequent changes in cloud responses thereto or other atmospheric circulation.
Not exact matches
«The overall slow decrease of upwelling SW flux from the mid-1980's until the end of the 1990's and
subsequent increase from 2000 onwards appear to caused, primarily, by
changes in global
cloud cover (although there is a small increase of
cloud optical thickness after 2000) and is confirmed by the ERBS measurements.»
In addition, the warming stopped and started to slide lower when the cloud coverage increased after the 1990s - apparently, small changes in cloud coverage are quite powerful in terms of subsequent temperature trend
In addition, the warming stopped and started to slide lower when the
cloud coverage increased after the 1990s - apparently, small
changes in cloud coverage are quite powerful in terms of subsequent temperature trend
in cloud coverage are quite powerful
in terms of subsequent temperature trend
in terms of
subsequent temperature trends.
«The overall slow decrease of upwelling SW flux from the mid-1980's until the end of the 1990's and
subsequent increase from 2000 onwards appear to caused, primarily, by
changes in global
cloud cover (although there is a small increase of
cloud optical thickness after 2000) and is confirmed by the ERBS measurements... The overall slight rise (relative heating) of global total net flux at TOA between the 1980's and 1990's is confirmed
in the tropics by the ERBS measurements and exceeds the estimated climate forcing
changes (greenhouse gases and aerosols) for this period.
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.