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  5. Processing Thermal Infrared Imagery Time-Series from Volcano Permanent Ground-Based Monitoring Network. Latest Methodological Improvements to Characterize Surface Temperatures Behavior of Thermal Anomaly Areas
 
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Processing Thermal Infrared Imagery Time-Series from Volcano Permanent Ground-Based Monitoring Network. Latest Methodological Improvements to Characterize Surface Temperatures Behavior of Thermal Anomaly Areas

Author(s)
Sansivero, Fabio  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia  
Vilardo, Giuseppe  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia  
Language
English
Obiettivo Specifico
1IT. Reti di monitoraggio e sorveglianza
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Remote Sensing  
Issue/vol(year)
/11 (2019)
Pages (printed)
id 553
Date Issued
March 6, 2019
DOI
10.3390/rs11050553
Alternative Location
https://www.mdpi.com/2072-4292/11/5/553/htm
URI
https://www.earth-prints.org/handle/2122/12479
Subjects
05.06. Methods
Subjects

volcano monitoring

thermal imaging

time series

Seasonal-Trend Decomp...

heat flux

Abstract
Abstract: In this technical paper, the state-of-art of automated procedures to process thermal infrared (TIR) scenes acquired by a permanent ground-based surveillance system, is discussed. TIR scenes regard diffuse degassing areas at Campi Flegrei and Vesuvio in the Neapolitan volcanic district (Italy). The processing system was developed in-house by using the flexible and fast processing Matlab© environment. The multi-step procedure, starting from raw infrared (IR) frames, generates a final product consisting mainly of de-seasoned temperatures and heat fluxes time-series as well as maps of
yearly rates of temperature change of the IR frames. Accurate descriptions of all operational phases and of the procedures of analysis are illustrated; a Matlab© code (Natick, MA, USA) is provided as supplementary material. This product is ordinarily addressed to study volcanic dynamics and improve the forecasting of the volcanic activity. Nevertheless, it can be a useful tool to investigate the surface temperature field of any areas subjected to thermal anomalies, both of natural and anthropic origin.
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