Press Release

Measuring Earthshine: How New Terra Data Are Improving Weather and Climate Forecast Models

By SpaceRef Editor
July 15, 2002
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A sensor aboard NASA’s Terra satellite is helping scientists map how much
sunlight the Earth’s surface reflects back up into the atmosphere, and this
new detailed information should help to greatly improve weather and forecast
models.

The Moderate Resolution Imaging Spectroradiometer (MODIS) now routinely
provides daily global and local measurements of albedo, or the total amount
of light reflected from Earth’s surface out to space. These precise data may
allow scientists to better understand and predict how various surface
features absorb and reflect solar radiation, which influence both short-term
weather patterns and longer-term climate trends.

In a May 2002 issue of Geophysical Research Letters, a team of scientists at
Boston University reported that the new albedo measurements match up well
with the wide variance of geological features found across the Earth’s
barren landscapes.

“Zooming in on Africa’s Sahara Desert and the Arabian Peninsula, for
instance, MODIS observed considerable variability in reflectance across the
region-from the darkest volcanic terrains to the brightest sand sheets,”
said Elena Tsvetsinskaya, the paper’s lead author and a researcher at Boston
University. “So we can relate specific soil groups and rock types to
MODIS-derived albedo measurements.”

This correlation is important because most current weather forecast models
treat this region as if the surface is uniform and therefore reflects the
same amount of light all across its wide expanse. However, the terrain
across the Sahara Desert and Arabian Peninsula is actually quite varied.
Darker surface features (like rocks and plant canopies) absorb more light
than lighter surfaces (like sand) and therefore get hotter in the afternoon.
Over the course of a day, these heating differences can set up atmospheric
motions that influence clouds and rain.

By coupling the MODIS measurements with geologic information, Tsvetsinskaya
and her colleagues have provided weather and climate modelers with a new map
of albedo across Northern Africa and the Arabian Peninsula that they can use
to fine-tune their models. The team classified the region into eight
categories, each of which has a distinct reflectivity range.

“There is a certain scientific beauty in deriving albedos from something
else in the model (such as geologic information),” said Robert Dickinson,
project lead at the Georgia Institute of Technology. “But the more practical
reason is for ‘what if’ studies. For example, what if the wind in Africa
blew so hard it covered all the black rocks with white sand?”

This scenario hints at what both meteorologists and climate researchers
alike know well: albedo for a given region can change relatively quickly.
For example, the bright white snow- and ice-covered landscapes of Canada and
Siberia during the winter and early spring reflect most incoming solar
radiation back up into space, thereby helping to keep the surface cold.

But as the snow melts with the gradual onset of summer, the boreal forest
canopy is exposed to the sunlight. The vegetated surface is much darker and
strongly absorbs light, which helps to warm the surface.

NASA scientists discovered recently that once the snow melts in the Earth’s
boreal regions, densely-vegetated surfaces begin to release a significant
amount of heat into the overlying atmosphere. Yufang Jin, a Boston
University graduate student, uses MODIS albedo data to document the
difference between snow covered and snow-free vegetated surfaces in a
related paper in another May issue of Geophysical Research Letters.

Over the longer term, regular MODIS albedo measurements will allow
scientists to monitor how the Earth’s reflectivity changes on a global
scale. “This will help us determine how the Earth’s climate is changing,
both globally and locally,” said Crystal Schaaf, co-author and research
professor at Boston University. “When humans convert a vegetated region to a
more reflective surface type (such as an urban area), the albedo changes.”

Similarly, Schaaf added, when places like the grasslands of the African
Sahel contract, they leave more reflective, barren deserts, which increases
albedo.

Launched December 18, 1999, Terra is the flagship of the Earth Observing
System series of satellites and a central part of NASA’s Earth Science
Enterprise. The mission of the Earth Science Enterprise is to develop a
scientific understanding of the Earth system and its response to natural and
human-induced changes to enable improved prediction capability for climate,
weather, and natural hazards.

For more information and images:
http://www.gsfc.nasa.gov/topstory/20020624earthshine.html

SpaceRef staff editor.