The efficacy E is then used to define an effective forcing fe = f E. Table 4 - 2 summarizes the forcings, responses, efficacies, and effective forcings of
different forcing agents from several models.
Not exact matches
At the close of the twentieth century, with ecological deterioration accelerating and the nuclear threat ever with us, we need to feel not acceptance but the challenge to join
forces on the side of life, for while we, like all creatures, are ultimately part of a universe that is brutal and may well end, we have, while we live, a part to play
different from that of any other creature: we are responsible
agents who can join with our loving parent to help our own and other species to survive and flourish.
«In addition, 4,969 personnel of the Police Mobile
Force (PMF) drawn
from different squadrons across the country have been deployed to strategic places, to complement the 11,000 conventional Police manpower, and other security
agents already deployed for the election.
When it came to their state of mind, they were not so
different from US Special
Forces agents.
The other wrinkle is depending slightly on the spatial distribution of
forcing agents,
different feedbacks and processes might come into play and thus an equivalent
forcing from two
different sources might not give the same response.
Different climates have different vertical temperature profiles (aside from horizontal and temporal temperature variations), which affects the radiative forcing that an amount and arrangement of greenhouse agents (CO2, CH4, etc, also, water vapor and clouds) w
Different climates have
different vertical temperature profiles (aside from horizontal and temporal temperature variations), which affects the radiative forcing that an amount and arrangement of greenhouse agents (CO2, CH4, etc, also, water vapor and clouds) w
different vertical temperature profiles (aside
from horizontal and temporal temperature variations), which affects the radiative
forcing that an amount and arrangement of greenhouse
agents (CO2, CH4, etc, also, water vapor and clouds) will have.
On the contrary, I want to separate out the effects on climate sensitivity estimation of varying GMST responses to
different forcing agents, which is what MEA15 is about,
from the effects of time - varying climate sensitivity in GISS - E2 - R.
[ii] It is usual to assume that
forcings from different agents are linearly additive; results
from GCMs generally support this assumption.
As you note there are ERF data for 3
different decades for all the
forcing agents from a single model run.
Hansen 2005 concluded that, at least for climate
forcing agents over the historical period, Fs was a good measure of the effective
forcing (the product of a
forcing, however defined, and the efficacy taken relative thereto), notwithstanding that some
forcings had
different spatial distributions
from others.