Greg McFarquhar (PI)
University of Illinois Urbana-Champaign
mcfarq@atmos.uiuc.edu
Quantifying Aerosol Indirect and Semi-Direct Effects on Trade Wind Cumuli
Using Cloud Process Models and High Resolution Satellite Observations
Increases in aerosol concentrations lead to smaller cloud droplets that
increase cloud albedo and suppress drizzle (first and second indirect
effects). Where significant absorption of solar radiation by carbonaceous
aerosols exists, a warming of the cloud layer may lead to a reduction
in cloud cover (semi-direct effect). Through these effects, anthropogenic
aerosols can modify the surface radiation budget, the vertical profile
of atmospheric heating and cooling, evaporation off Earth’s surface,
detrainment from clouds and fluxes of sensible and latent heat, that
in turn impact cloud cover, feedback on the energy budget and hydrological
cycle and induce cloud dynamical responses. We propose to use a cloud-resolving
model in coordination with satellite observations to quantify aerosol
impacts on trade cumuli microphysical, macrophysical and radiative properties
over the Indian Ocean and to better understand the processes through
which these impacts occur. We focus on trade cumuli because they are
nearly ubiquitous over tropical oceans, impact global water and energy
budgets, and their properties are highly susceptible to aerosol indirect
and semi-direct effects--yet our understanding of their properties and
their treatment in climate models is extremely poor. We will focus our
modeling and satellite studies on the Indian Ocean region where trade
cumuli in pristine and polluted air occur in close proximity to each
other during the winter monsoon, and where in-situ data (e.g., aerosol
properties, thermodynamic profiles) are available from the Indian Ocean
Experiment (INDOEX) to guide and initialize modeling studies. We
will use the 3-d version of the NCAR Eulerian/semi-Lagrangian (EULAG)
model, which will have bin-resolved microphysics, to quantify and better
understand processes by which aerosols impact cloud cover, microphysical
processes and properties, precipitation, vertical velocities (w), detrainment,
life cycles, profiles of radiative heating and surface fluxes of sensible
and latent heat. We will examine the impacts of aerosols on these quantities
over the diurnal cycle, in particular, investigating: 1. impacts of the
vertical distribution of aerosols on simulated trade cumuli properties
and their feedbacks on heating rates, surface fluxes, w and cloud properties;
2. how different mixing scenarios for black carbon (i.e., internally
or externally mixed, embedded as core within haze) influence the absorption
of radiation and nucleation of cloud droplets, and hence the resultant
feedbacks between simulated cloud properties, heating rates, surface
fluxes and w; 3. whether improved representations of drizzle development
with bin-resolved microphysics can help better understand the second
indirect effect in polluted trade cumuli and the associated feedbacks
to surface fluxes, w, heating rates and cloud properties; and 4. the
magnitude of indirect and semi-direct forcing on regional scales, which
can be compared to similar estimates from large-scale models to assess
their representations of aerosol forcing. A critical element of
our research is to evaluate whether model results are consistent with
satellite remote sensing observations of aerosol effects on cloud properties.
This will involve comparing statistics (e.g., means, spreads) of how
modeled and observed cloud properties change depending on aerosol optical
depth, single-scattering albedo, aerosol vertical distribution and meteorological
forcing. Hence, we will: 1. develop and compare climatologies of trade
wind cumuli (fractional coverage, size distribution, height distribution,
albedo, optical depth, effective particle size) from EOS-Terra and A-Train
satellite data moving away from a “pixel” summary approach
to a “cloud object” approach to provide properties of individual
clouds rather than of individual pixels; and 2. use these climatologies
to examine impacts of aerosols and meteorology on trade cumuli statistics,
focusing on the Indian Ocean, where we have large samples of cumuli in
both pristine and polluted air. We will assess whether cloud properties
change in a consistent manner with varying aerosol properties (e.g.,
optical depth) or meteorological forcing (e.g., humidity in mixed layer)
for models and observations, revisiting representations of model processes
when necessary. The ultimate goal is to gain a process-oriented
understanding of how aerosols impact trade cumuli microphysical and dynamical
properties, to isolate processes that have the largest impact on energy
and water budgets on a regional scale and to assess whether our regional
estimates of semi-direct and indirect effects are consistent with estimates
obtained from large-scale models.
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