The unforced temperature estimate is used as a proxy for what cumulative emissions should be given the current level of warming.
Not exact matches
We then used this new
estimate of
unforced variability to aid in our interpretation of observed global mean
temperature variability since 1900.
We compare global - scale changes in satellite
estimates of the
temperature of the lower troposphere (TLT) with model simulations of forced and
unforced TLT changes.
«Our reconstructions broadly agree with historical emissions
estimates, and can explain the differences between observed changes in Arctic
temperatures and expectations from non-aerosol forcings plus
unforced variability.»