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2001 EARTH SCIENCE VIDEOTAPES

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Synopsis

NASA'S TERRA SATELLITE CAPTURES A WORLD OF SUNLIGHT AND HEAT G01-050 06/20/01 00:15:28Earth's energy balance represents the sum total of all the interactions of sunlight with our planet's climate system (as both sunlight and heat). For the first time, a new NASA sensor can measure the radiant energy reflected and emitted back into space accurately enough to tell scientists which aspects of the Earth's climate system--such as clouds, aerosol particles, surface reflectivity--are changing, and exactly how much these changes affect our planet's total energy budget. NASA's Clouds and the Earth's Radiant Energy System instrument (CERES), flying aboard the TERRA satellite, measures radiant energy fluxes every day on a global scale. Today's release demonstrates the first year of CERES' measurements of the Earth's energy budget and what these measurements are teaching us about our changing climate.

TAPE CONTENTS:

ITEM (1): A Cloudy Climate Mystery Animation - Clouds cause the most dramatic and dynamic changes in radiation, especially in the tropics where three sets of thunderstorm clouds (stretching across South America, Africa, and Indonesia) are visible. These same clouds are one of the major puzzles in predicting how our future climate might change, as clouds have the power to amplify climate change or reduce it. CERES measurements will be used with other Terra instruments to help unscramble this "cloudy" picture and reduce uncertainties in climate change predictions.

The CERES data shown in this animation are 14-day running average 
values of thermal energy or heat emitted to space from March 2000 
through May 2001.  The smallest amount of Earth's radiation emitted 
to space is shown in white over Greenland and Antarctica.  The levels 
of energy increase from blue to red to yellow.   The greatest amounts 
of heat emitted are from the Sahara Desert and the Arabian Peninsula. 
Cold, blue-colored temperature ranges are found not only at high 
latitudes, but also in the tropics from cloud tops of thunderstorm 
systems so extensive that they span thousands of miles.

Courtesy:   NASA
ITEM (2): Capturing Dynamic Changes In The Climate System - Small water droplets or ice crystals in clouds, snow, and ice reflect most of the incoming solar energy back to space. People, however, can also affect how much solar energy the Earth receives and reflects. They do so in subtle, but significant ways, by adding aerosol particles to the atmosphere or causing deforestation or reforestation, which can change the amount of reflected sunlight. All of these elements are captured in the CERES observations. How do the aerosols affect the clouds? How are ice caps and snow packs changing Earth's surface area and reflection? How will clouds change in a warmer planet? These are just a few of the climate questions that scientists will seek to answer with the new CERES solar energy data.

The CERES data shown in this animation are 14-day running average 
values of sunlight reflected back to space from March 2000 through 
May 2001. The lowest amount of reflected solar energy, shown in blue, 
occurs over clear ocean areas. Green colors show gradually increasing 
amounts of reflected sunlight. The areas of greatest reflected solar 
energy, shown in white, occur both from the tops of thick clouds and 
from ice-covered regions on the Earth's surface during summer. Watch 
for white areas of clouds over China and India that show the growth 
and decay of the monsoon season and the changes from summer to winter 
seasons. a Notice how Greenland  appears as an island of ice alone in 
the Northern Hemisphere summer.

Courtesy:   NASA
ITEM (3): For Every Season, The Earth Turns, Turns, Turns - The amount of incoming solar energy the Earth receives on June 21, the first day of summer, is 30 percent higher at the North Pole than at the equator. Just 6 months later in winter, the entire polar cap receives no energy since Earth's movement along its orbit has pointed the North Pole away from the Sun. This swing of illumination and reflection is shown dramatically in this CERES animation. Critical to understanding future climate are the subtle changes in reflected solar energy, such as changes in the surface area of the arctic ice cap or in cloud thickness. Ever-changing cloud cover or the seasonal retreat and advance of sea ice cause motion in this image. This motion is visible especially near edges of the Arctic Ocean and the continent Antarctica.

  Courtesy:    NASA
ITEM (4): Record Setting U.S. Heat Wave - CERES measured the thermal radiation emitted from the United States, as shown in this image from May 2001. The record-setting high temperatures experienced in Southern California and Nevada on May 9 are visible in the yellow areas where great amounts of thermal energy are escaping to space. This example illustrates one of the most basic stabilizing forces in the Earth's climate system: clear hot regions lose more energy to space than cold areas. The moving blue regions of low thermal emission over the northern U.S. are cold cloud tops. CERES data will be used to verify the ability of climate models to accurately predict this emission as our world experiences changes in surface reflectivity, clouds, atmospheric temperatures, and key greenhouse gases such as water vapor.

Courtesy:    NASA
ITEM (5): Deadly May Heat Wave In Pakistan - CERES measured the thermal radiation emitted from the regions of the Indian subcontinent and northern Africa, as shown in this image from May 2001. The heat wave in Pakistan that killed at least 33 people the weekend of May 5-6 is seen in yellow as a region emitting high values of thermal energy. This example is one of the most basic stabilizing forces in the Earth's climate system: clear hot regions lose more energy to space than cold ones. High, cold thunderstorms cause the moving blue regions of low thermal emission over the Indian Ocean. CERES data will be used to verify the ability of climate models to accurately predict the Earth's changing thermal emission as our world experiences changes in surface reflection, clouds, atmospheric temperatures, and key greenhouse gases such as water vapor.

Courtesy:     NASA
ITEM (6): CERES Science Animation
ITEM (7): TERRA Satellite Animation
ITEM (8): Electromagnetic Spectrum Animation
ITEM (9): "B" Roll:
 a. Tropical Rainstorm Clouds

b. Summer Solstice Animation

c. SVS Image of Earth

d. People (Drought)  

ITEM (10): Dr. Bruce Wielicki, CERES Principle Investigator, NASA Langley Research Center
 
 


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