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Detecting Eruption Clouds with Weather Satellites

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Eruption Clouds from Mt. Spurr volcano, Alaska

Eruption column at Mount Spurr, Alaska
Photograph by R. McGimsey on 18 August 1992
Mount Spurr eruption column reached 14 km above sea level.

Satellite data of Mount Spurr's three eruption clouds in 1992 were extremely useful in identifying the initial clouds and tracking their movement downwind. Explosive eruptions inject enormous volumes of volcanic ash and gases into the atmosphere, where the ash is carried downwind or hundreds or thousands of kilometers and often remains airborne for days to weeks. As the ash and gas move and disperse downwind, it becomes increasingly difficult for aircraft pilots and scientists to distinguish an eruption cloud visually from weather clouds, especially at night or in poor weather. Since ash cannot yet be detected by weather radar aboard an aircraft, satellite images and pilot reports of unexpected ash encounters provide the critical information needed to keep commercial aircraft from entering an eruption cloud downwind from an erupting volcano.

Image data from several geostationary and polar orbiting satellites are now received directly at some volcano observatories or it can be accessed via computer networks. Sensors aboard these weather satellites record the amount of thermal energy in several different wavelengths emitted (or radiated) from weather and eruption clouds and the Earth's surface. Scientists use the image data from these different wavelengths in different ways to detect and track an eruption cloud.

 

Near Mount Spurr: tracking the eruption cloud

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.

Eruption cloud from Mount Spurr, Alaska 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.
Eruption cloud from Mount Spurr, Alaska 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.
Ash atop car, Anchorage, Alaska 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.

 

Far From Mount Spurr: tracking the eruption cloud

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.

Eruption cloud from Mount Spurr, Alaska

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.
Eruption cloud from Mount Spurr, Alaska

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.

 

Applications of Satellite Monitoring

 

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Last modification: Tuesday, 30-Jan-2001 19:44:22 EST (SRB)