Detecting Volcanic Ash Clouds Making Use of Satellite Images and Machine
Learning Algorithms
Abstract
Volcanic ash detection is important for effective emergency management.
Ash emitted by volcanoes is injected at high altitudes into the
atmosphere, dispersed and driven by wind and extended for kilometres
away from volcanoes. It can affect communities in different ways
including health, agriculture, the environment and air traffic. Thus,
detecting and tracking the volcanic ash clouds using satellite images
can help civil protection authorities and volcanic ash advisory centres
respond rapidly to a volcanic event. Satellite based detection of
volcanic ash has traditionally entailed the implementation of radiances,
reflectances, brightness temperatures (BT), brightness temperature
differences (BTD), beta ratios and cloud objects tracking tools. The aim
of this study is to test machine learning algorithms on satellite data
in order to identify volcanic ash in the atmosphere as an attempt to
enhance the space-borne ash detection capabilities especially in
ambiguous cases, where image classification is hard, such as when ash,
clear land and cirrus clouds coexist within a scene. We used a set of 10
satellite images acquired by the Moderate Resolution Imaging
Spectroradiometer (MODIS) on board the satellites Terra and Aqua just
after the 4 June 2011 eruption of the Puyehue Cordon Caulle Volcanic
Complex to train and test two supervised classification algorithms:
K-Nearest Neighbours and Support Vector Machine, for volcanic ash
detection in the atmosphere. We first built a database that consists of
217,859 pixels identified and labelled, on the basis of visual
interpretation of color composites, according to seven classes: volcanic
ash above the emission centre, land and sea, meteorological clouds above
land and sea, and clear sky above land and sea. For each of the seven
classes, sample pixel values were retrieved for six features, which are
given by the BT at 11𝝁m and the BTDs between 11 and 12 𝝁m, 11 and 3.9
𝝁m, 11 and 6.7 𝝁m, 11 and 8.5 𝝁m and a BTD that combines the BTs
measured at 11, 12 and 8.5 𝝁m. We show preliminary results on
statistical analysis of the training datasets and performance of both
algorithms for volcanic ash detection above land and sea including
verification tests with MODIS datasets that cover the April 2015
eruption of Volcan Calbuco (Chile).