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Volcanologists utilise a technique called infrasound monitoring to pick up low-frequency pitches that are inaudible to human hearing and to pick up rumblings and explosions inside volcanoes.
In order to keep track of volcanoes, scientists employ a wide range of methods, such as seismographic detection of the earthquakes and tremor that almost always precede eruptions, exact measurements of the ground deformation that frequently occurs in conjunction with magma rise, changes in volcanic gas emissions, and changes in gravity and magnetic fields.
Although not diagnostic on their own, these methods have been combined at well-monitored volcanoes to produce accurate predictions.
The Global Volcano Monitoring System Market accounted for $XX Billion in 2021 and is anticipated to reach $XX Billion by 2030, registering a CAGR of XX% from 2022 to 2030.
This heat can be detected from space, and measuring it is a highly helpful method for spotting global volcanic activity.
Based on the analysis of MODIS data, MIROVA (Middle Infrared Observation of Volcanic Activity) is an autonomous volcano hot spot identification method (Moderate Resolution Imaging Spectroradiometer) from Frontiers in Earth Science.
By delivering infrared photos and thermal flux time-series on more than 200 volcanoes globally on a dedicated website (www.mirovaweb.it), the system is able to detect, localise, and quantify thermal abnormalities in close to real-time.
Several volcanic observatories presently use MIROVA for daily monitoring activities and reporting due to its user-friendly interface and understandable data representation.
In light of the experience gained in recent years within the volcanological community, the present restrictions and requirements to improve the quality of the data, their distribution,
