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Whereas magma erupted by volcanoes is initially extremely hot (>850 degrees Celsius), the top of an eruption cloud that is measured by satellite sensors is very cold (< -50 degrees Celsius). As the ash and gas in the cloud rises, it cools rapidly to the temperature of the surrounding atmosphere. When a high eruption cloud is within a few hundred kilometers of a volcano, the cloud can be "seen" easily in satellite images. |
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Satellite image showing the location of the August 18 eruption cloud about 1.5 hours after the eruption started. The blue color is relatively warm and the red color shows the colder, circular eruption cloud. |
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Satellite image showing the location of the August 18 eruption cloud about 3 hours after the eruption started. While the eruption continues, the leading edge of the eruption cloud has moved more than 200 km southeast over the Seward Peninsula. |
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The northern edge of the eruption cloud passed over Anchorage, where falling ash blanketed the city with an ash layer 1 to 3 mm thick. The ash temporarily prevented aircraft from landing or departing the Anchorage International Airport. |
Although it is relatively straightforward to detect eruption clouds in a thermal imagery during an eruption, it becomes more difficult as the cloud drifts hundreds or thousands of kilometers from the vent, and disperses in the atmosphere. Weather satellites used to detect volcanic clouds measure emitted energy at several different wavelengths. Scientists have developed a mathematical operation that uses data from two different thermal wavelengths to enhance the visibility of eruption clouds and and discriminate them from meteorological clouds. The images below show the results of the technique. This type of image processing can be very valuable for tracking eruption clouds in order to prevent aircraft from encountering volcanic ash. |
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Satellite image showing the location of the September 16-17 eruption cloud about 48 hours after the eruption started. This image shows data from a single thermal band of the satellite sensor, the Advanced Very High Resolution Radiometer (AVHRR). The eruption cloud from the September, 1992 eruption of Mt. Spurr, Alaska is in this image, but it is difficult to see. |
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Satellite image showing the location of the September 16-17 eruption cloud about 48 hours after the eruption started. This image shows the result of using the difference between two thermal bands of the AVHRR sensor. The eruption cloud is clearly visible extending in an arc from northern Quebec, southwest above Ontario, Michigan and Wisconsin. |
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