Start Date/Time: Friday, January 06, 2012, 3:30 PM
Location: JHN 075
Speaker: Robert J. Charlson, Professor of Atmospheric Sciences and Chemistry, UW
Abstract
Global climate forcing by aerosols (i.e., the change in Earth's energy balance
imposed by anthropogenic particles in the atmosphere) is estimated to range
from about -0.5 to -1.5 W/m2, which remains as the dominant factor in the
uncertainty in total climate forcing (the sum of greenhouse gas plus all other
forcings). By comparison, this forcing is opposite in sign and somewhat smaller in
magnitude than the current global mean forcing by anthropogenic greenhouse
gases of ca. +2.5 W/m2. The uncertainty in total forcing precludes accurate
quantification of climate sensitivity from the temperature record over the 20th
century; in fact, it has allowed various climate models to fit the T record despite
large differences in their climate sensitivity.
This lecture traces the early history of greenhouse gas and aerosol/climate
research, in particular the first estimates of aerosol forcing made in the early
1990's, which were largely based on observations of atmospheric aerosol
properties. Subsequent efforts have been dominated by models of increasing
complexity while attempts at improving the global observational basis via
instrumented satellites are underway. Predictably, the total forcing will become
less uncertain as the greenhouse gases continue to accumulate in the
atmosphere, such that the need for control of those gases will become
increasingly urgent, even if the present uncertainty in aerosol forcing is not
reduced. Meanwhile, reducing the uncertainty of the aerosol forcing is necessary
if we are to be able to understand the causes of the observed warming over the
20th century and to refine the projections of climate change in the future
Coordinator: Prof. Robert Houze (houze@atmos.washington.edu)