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| by John Weier - April 14, 1999 | |||
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| Since well before global warming became a heated political
issue, scientists have been trying to determine the rate at which our
planet’s temperature is increasing. While placing many thermometers around
the world would appear to be the solution, local temperatures can vary widely
across regions and from one year to the next. Instead, researchers have found
they can obtain a measure of average global temperatures by using
satellites to monitor heat-sensitive objects on the ground. Of these objects,
glaciers are among the most reliable indicators of climate change. |
Alpine glaciers, like this one near Mt. McKinley, Alaska, change in response to the local climate. By monitoring the change in size of glaciers around the world, scientists can learn about global climate change. (Photograph by Klaus J. Bayr, Keene State College, 1990) | ||
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One method of measuring glaciers is to send researchers onto the ice with surveying equipment. The Muir Glacier, shown here around 1950, has been studied for over 200 years. (Photograph from the American Geographic Society Collection archived at the National Snow and Ice Data Center, University of Colorado at Boulder) | ||
Despite typical glaciers’ massive sizes, monitoring them is not always an easy task. Only specific types of small glaciers are good measures of climate change. Some glaciers are too large to measure accurately, and others are simply too unpredictable. Once scientists find a suitable glacier, they must take satellite images of the ice for a minimum of five years and compare the results. They then have to look closely at the outside edge of the glacier (the glacier’s terminus). If a large percentage of the glacier’s edge is receding then the area around the ice is growing warmer, and if a large percentage is expanding then the area is growing cooler. When enough measurements from many different parts of the world have been gathered, the researchers can determine whether the earth is growing warmer or cooler. The data used in this study are available in one or more of NASA's Earth Science Data Centers. |
 The terminus of the Pasterze glacier, Austria. It dwarfs the three hikers at lower right. (Photograph by Klaus J. Bayr, Keene State College, 1988) | ||
Types of Glaciers