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During
the dry-season in southern Africa,
large areas of grasslands burn each
year, but this year's burning season
was extremely large. SAFARI 2000 field
campaign scientists studied the extent
of these fires and the impact of the
rising smoke on air pollution, climate
change, and clouds.
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One
of the goals of the SAFARI 2000 field
campaign was to distinguish industrial
emissions from other sources of air
pollution, such as the smoke from
the extensive grassland fires in southern
Africa.
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NASA's
ER-2 high altitude aircraft (foreground)
observed the southern African haze
layer from 60,000 feet while the University
of Washington's Convair-580 aircraft
(background) used scientific instruments
to directly sample the haze. The planes
are shown at the base of flight operations
for the SAFARI 2000 dry-season campaign
in Pietersburg, South Africa.
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ER-2
pilot Ken Broda prepares for a flight
from Pietersburg airport, South Africa.
The high-altitude aircraft carried
several remote-sensing instruments
similar to those on NASA's Terra spacecraft.
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Instruments
onboard the University of Washington's
Convair-580 research aircraft sampled
the smoke plumes produced by the unprecedented
fire season this year in southern
Africa.
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hi-res
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Continuous
observations of an African savannah
ecosystem are being made from a NASA-funded
research tower in Kruger National
Park (South Africa). The ground-based
data are combined with observations
from aircraft and satellite to give
a complete picture of the region's
ecosystems and their role in climate
change.
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Satellite
View of Ozone
High
levels of ozone, a component of smog,
were produced by the fires in southern
Africa. Ozone from the inland fires
concentrates and flows east to the
Indian Ocean and west over the
Atlantic. The ozone levels were
frequently similar to those found in
air pollution alerts in major U.S.
cities. This data was also acquired by
Earth Probe TOMS in September
2000.This is a still from the movie
clip showing ozone levels over
southern Africa on Sept. 25, 2000.
Click
on pic to start animation. Click
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Satellite
Views of Fires and Aerosols
Multiple
fires are burning across the southern
part of the African continent in
September 2000, as shown by data from
the Advanced Very High Resolution
Radiometer (AVHRR) on board the
NOAA-14 satellite. The unprecedented
amount of fires generated large
amounts of aerosols (overlaid on top),
which were observed with the Earth
Probe Total Ozone Mapping Spectrometer
(TOMS) instrument. The still image is
from this movie clip showing fires and
resulting aerosols over southern
Africa.
Click
on pic to start animation. Click
here for high
res image of still. |
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Aerial View of Fires
On
August 20, 2000, a prescribed burn was
set in the Madikwe Game Reserve in
South Africa near the border of
Botswana. The fire was observed by the
MODIS airborne simulator aboard NASA's
ER-2 aircraft. The region is shown
first in visible light, with smoke
plumes. The simulator then peers
through the smoke to view the fires.
The burn was timed to coincide with
the overpass of NASA's Terra
spacecraft. The first still is
from the next animation showing the
MODIS airborne simulator view of the
rising smoke plume from the Madikwe
prescribed burn. (A cloud and shadow
appears at the upper edge of this
image.) The second still, also
from the animation, shows the MODIS
airborne simulator view of the Madikwe
fire and burn scar through the smoke.
Click
on the first pic to start
animation. Click here
for high res image of the first image
still. Click here
for high res of the second image
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Role
of Aerosol Haze Layer on Climate
Scientists
around the world are studying the
complex role of airborne particles
called aerosols on climate.
The
first image shows that aerosols
produced by biomass burning and other
types of emissions that were sampled
during the SAFARI 2000 campaign were
more heat-absorbing than expected.
Thus, the haze layer may have a
significant warming influence on the
region's atmosphere.
The
second image shows that aerosols
are usually thought to reflect
sunlight back into space, thereby
cooling the atmosphere.
Click
here for high res image of
the first still. Click
here for high res image of
the second still. |