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Exercise 2: Hot spot and plume detection Hot spot detection Volcanic activity can be identified by detecting thermal hot spots. Hot thermal anomalies of volcanoes detected by infrared sensors can be due to the lava flow of any thermal anomaly (e.g. fumaroles). A warning is given when indices calculated by infrared bands exceed a certain threshold (see Hot spot monitoring with MODIS). The term ‘hot spot’ must not be confused with ‘hotspot volcanism’. Open the Bands 21 and 22 and apply stretching:
File > Open > etna_mod_2001-205_bd21 > Enhance > Interactive Stretching
Volcanic Plume Detection A volcanic plume is a mixture of particles and gas emitted by an eruption. The plume is generated by fragmentation of magma. Plumes may reach heights of 80 km in large eruptions. Volcanic ash can be transported to the atmosphere and reach the height of air traffic within ten minutes. The detection, monitoring, and forecasting of plumes is essential to provide safety for air traffic. To find out more about this, have a look at the Toulouse Volcanic Ash Advisory Center. Open these two images and stretch them:
File > Open > etna_mod_2001-205_bd31 > Enhance > Interactive Stretching
Page Last update: 17 April 2013
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