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RELEASE NO: 02-137

September 17, 2002

NASA Scientists Use Satellites to Distinguish Human Pollution from Other Atmospheric Particles

   

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.

True
Color Dust Image
True Color Smoke Image

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).

Global Aerosol Optical Depth

Aerosol Optical Depth and Radius

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.

 

Animations:

Aerosol Optical Depth

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)

Global Aerosol Optical Depth and
Radius

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)

Modelled Global Aerosol Optical
Depth and Radius

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)

Comparison of Measured and
Modelled Aerosol Optical Depth and Radius

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)

 

   
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