Further work is needed to quantify links of
regional nonradiative forcing to regional and global climate response
As is the case for regional radiative forcing, further work is needed to quantify links between
regional nonradiative forcing and climate response.
Not exact matches
Nonradiative forcings generally have significant
regional variation, making it important that any new metrics be able to characterize the
regional structure in forcing and climate response — whether the response occurs in the region, in a distant region through teleconnections, or globally.
It needs to be expanded to account for the vertical and
regional structure of radiative forcing and also for
nonradiative climate forcings.