The current NCEP forecast (Fig. 5) has a Nino3.4 peak at only about 1.5°C,
which would not be a super El Nino, but some other models predict a
strong El Nino, comparable to those in 1997 and 2016, which are
described as super El Ninos. The expectation that aerosols will decline
moderately during the next few decades is based on the assumption that
the world will trend toward clean energy sources that emit fewer
aerosols than fossil fuels. Aerosol sources are complex, however, and
include fires that may increase with global warming. It is unfortunate
that we are not monitoring the global aerosol climate forcing; that is
difficult because it requires precise global measurements of aerosol and
cloud microphysics; we knew how to do that in 1990,[10] but chose not
to initiate such a monitoring system.
Finally, we note that these topics are discussed in plain language in a
prior communication.[11] The distinction between equilibrium warming
(which is approximately 10°C for present atmospheric composition) and
committed warming (which is a more complex matter that depends on ocean
and ice sheet response times and on the rate of future greenhouse gas
emissions) is discussed in that communication, where we also explain
that we prefer to work on advancing the science, rather than engage in
Twitter wars about the difference between equilibrium warming and
committed warming. The difference between equilibrium and committed
warmings is also discussed in a recent communication.[12]
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