Driven by precise new satellite measurements and sophisticated new computer
models, a team of NASA researchers is now routinely producing the first global
maps of fine aerosols that distinguish plumes of human-produced particulate
pollution from natural aerosols.
In the current issue of Nature, atmospheric scientists Yoram Kaufman, at
NASA’s Goddard Space Flight Center, Greenbelt, Md., Didier Tanré and
Olivier Boucher from CNRS (Centre National de la Recherche Scientifique) at the
University of Lille, reported in a review paper that these global maps are an
important breakthrough in the science of determining how much aerosol pollution
comes from human activities. Aerosols are tiny solid or liquid particles
suspended in the atmosphere. The authors stated that the next step is to
quantify more precisely the roles human aerosol pollution plays in Earth’s
weather and climate systems.


The top scene is a Moderate Resolution Imaging Spectroradiometer (MODIS) true-color image of a thick plume of
desert dust (brownish pixels) blowing from Northeast Africa eastward over the
Red Sea on July 11, 2002. The bottom scene is a true-color image of haze and
pollution (greyish pixels) blowing southeastward over Bangladesh and toward the
Bay of Bengal on January 14, 2002. The top image is an example of natural
aerosols, while the bottom image shows human pollution. (Images courtesy
Jacques Descloitres, MODIS Land Rapid Response Team at NASA GSFC)
For more information and high resolution images, see Dust Storm over the
Red Sea and Thick Haze Over
Northern India.
“Plumes of smoke and regional pollution are distinguished by their
large concentrations of small particles (less than 1 micrometer) downwind of
biomass burning sites and urban areas,” Kaufman said. “These
particles are important because, depending upon the type of particles produced,
human pollution can either have a warming or cooling influence on climate, and
they can either increase or decrease regional rainfall.”
Distinguishing small from large aerosol particles requires good understanding
of how aerosols reflect sunlight at key wavelengths of the solar spectrum. For
the first time ever, the Moderate Resolution Imaging Spectroradiometer (MODIS)
instrument flying aboard NASA’s Terra and Aqua satellites measures
precisely the sunlight reflected by aerosols back to space every day over almost
the entire planet at wavelengths spanning across the solar spectrum (from 0.41
to 2.2 micrometers).


high resolution images:
Aerosol Optical Depth (1.3 MB JPEG)
Aerosol Optical Depth for Print (5.9 MB TIFF)
Aerosol Radius (1.2 MB JPEG)
Aerosol Radius for Print (6.9 MB TIFF)
Aerosol plumes comprised of smaller particles (less than 1 micrometer)
reflect light at shorter wavelengths (blue light) much more strongly than plumes
comprised of larger particles (greater than 1 micrometer) which scatter and
reflect light roughly equally at short and long wavelengths (blue, green, red
and near-infrared light). It is this basic understanding that helps scientists
use MODIS data to distinguish human-produced aerosol.
However, there are exceptions to this rule. Kaufman noted that nature
produces small particles too, while humans can generate large particles by
changing land surface cover through agricultural practices and deforestation.
Therefore, scientists need additional information—such as land use and fire
activities, which are also observed by satellites, as well as information on
population and economic activities—that is fed into advanced new computer
aerosol models.
“Natural aerosols like salt particles from sea spray are typically
widespread over larger areas and not particularly concentrated downwind of urban
areas,” Kaufman observed. “Or, they are particularly concentrated
downwind of obviously natural sources, such as the streams of dust originating
from the Sahara Desert.”
Conversely, aerosols produced by humans are the result of urban pollution,
industrial combustion, or burning vegetation. These plumes of pollutants appear
in punctuated bursts of thick and concentrated plumes comprised of small
particles. Or, they are concentrated downwind of regions obviously altered by
human activities, such as deforested regions.
The authors find surprisingly good agreement between a new aerosol model
(developed jointly by NASA Goddard and Georgia Tech) and the measurements now
being made by the MODIS sensors. Examining global satellite images in concert
with global-scale models and globally distributed ground-based measurements
gives scientists the best tools they have ever had to estimate the effects of
aerosols on climate and weather patterns around the world.
The new aerosol measurements collected by the Terra and Aqua satellites
provide dramatic improvements over the measurements made by previous satellites
over the last two decades. Another instrument on Terra, the Multi-angle Imaging
SpectroRadiometer (MISR), observes aerosols by looking at the radiation
reflected and scattered by aerosols in nine different directions. This
multi-angle technique complements the multi-wavelength approach by NASA. NASA
plans to further expand global aerosol research with the launch of
satellite-based light imaging radars (lidars) that sends bursts of light to
Earth and, like a radar signal, provide a measure of the altitude and vertical
structure of aerosol plumes and clouds.
The Terra and Aqua satellites are part of NASA’s Earth Science
Enterprise, a long-term research effort to understand our home planet.
For more information, please see the MODIS website
For more information about POLDER and ADEOS, read Research Satellites for the Atmospheric Sciences, 1978 to the Present
Contact:
Lynn Chandler
Goddard Space Flight Center, Greenbelt, Md.
Phone: (301) 286-2806
lynn.chandler.1@gsfc.nasa.gov
The article can be downloaded from Nature.
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Animations:

Flying aboard NASA’s
Terra and Aqua satellites, the MODIS sensors measure atmospheric aerosols over
almost the entire globe every day. This movie shows “aerosol optical
depth,” which is a measure of how much sunlight is prevented from
traveling through a column of atmosphere. Basically, the movie shows where and
when aerosol plumes occur—the darker brown the pattern, the denser the
plume of particles and the less sunlight reaches the surface while more sunlight
is absorbed within the atmosphere or reflected back to space. Grey areas show
where no data were collected, such as over the poles during periods of darkness,
in cloudy areas, and over very bright land surfaces where MODIS does not make
aerosol measurements. (Animation by Reto Stockli, NASA Earth Observatory, based
upon data provided by the MODIS Atmosphere Science Team, NASA GSFC)

By measuring
precisely how much light is reflected at visible and near-infrared wavelengths,
the MODIS sensors can distinguish between plumes of large aerosol particles
(more than 1 micrometer) and small aerosol particles (less than 1 micrometer).
This new information, along with other data, helps scientists determine which
plumes are human produced and which occur naturally. In this movie, the green
patterns show plumes of large aerosol particles, red shows plumes of small
particles, and the brownish and whitish colors show where large and small
particles are intermingling. Grey areas show where no data were collected, such
as over the poles during periods of darkness, in cloudy areas, and over very
bright land surfaces (such as snow and ice, or the Sahara Desert) where MODIS
does not make aerosol measurements. (Animation by Reto Stockli, NASA Earth
Observatory, based upon data provided by the MODIS Atmosphere Science Team, NASA
GSFC)

Atmospheric scientists at NASA use the GOCART computer model to
simulate the transport of gases and aerosols through the atmosphere and around
the globe. (GOCART stands for Georgia Tech/Goddard Global Ozone Chemistry
Aerosol Radiation Transport.) In this movie, the green patterns show plumes of
large aerosol particles, red shows plumes of small particles, and the brownish
and whitish colors show where large and small particles are intermingling.
Driving this model are data gathered from many sources, including human
emissions from fossil fuels, biomass burning emissions, and natural sources of
gases and particulates such as vegetation, oceans, and volcanoes, and the
meteorological data provided by NASA’s Data Assimilation Office.
(Animation by Reto Stockli, NASA Earth Observatory, based upon GOCART Model data
provided by Mian Chin, Georgia Tech and NASA GSFC)

When comparing a movie of MODIS’ actual aerosol
observations to a movie produced by the GOCART Model, NASA scientists find
surprisingly good agreement between these two sources of information. The top
movie shows actual MODIS measurements, while the bottom movie shows the GOCART
simulation. In both movies, the green patterns show plumes of large aerosol
particles, red shows plumes of small particles, and the brownish and whitish
colors show where large and small particles are intermingling. Note that there
are no areas of missing data in the GOCART simulation, while the grey areas in
the MODIS data show where no measurements were made. Note also that the African
continent appears on both sides of the frame to illustrate how aerosol plumes
are transported across oceans and geopolitical boundaries alike. (Animation by
Reto Stockli, NASA Earth Observatory, based upon data provided by the MODIS
Atmosphere Science Team and GOCART Model data provided by Mian Chin, NASA
GSFC) |