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  5. Volcanic Ash and SO2 retrievals using synthetic MODIS TIR data: comparison between inversion procedures and sensitivity analysis
 
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Volcanic Ash and SO2 retrievals using synthetic MODIS TIR data: comparison between inversion procedures and sensitivity analysis

Author(s)
Corradini, S.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Pugnaghi, S.  
University of Modena and Reggio Emilia  
Piscini, A.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Guerrieri, L.  
University of Modena and Reggio Emilia  
Merucci, L.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Picchiani, M.  
Chini, M.  
Language
English
Obiettivo Specifico
5V. Sorveglianza vulcanica ed emergenze
5IT. Osservazioni satellitari
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Annals of Geophysics  
Issue/vol(year)
fast track 2/57(2014)
Date Issued
2014
DOI
10.4401/ag-6616
URI
https://www.earth-prints.org/handle/2122/9699
Subjects
04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring  
04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques  
05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions  
Subjects

ash and SO2 volcanic ...

Abstract
In this work the volcanic ash and SO2 retrievals obtained by applying three different procedures (LUT - Look Up Table, NN - Neural Network and VPR - Volcanic Plume Removal) on MODIS Thermal InfraRed (TIR)
synthetic measurements have been compared. The synthetic measurements are generated using MODTRAN Radiative Transfer Model (RTM) for defined volcanic cloud configurations. The results, presented as the percentage
difference between the retrieved ash and SO2 total masses and the true values used for the synthetic data generation, indicate maximum differences of +/- 15% and +/- 10% for all the procedures and for ash and
SO2 retrievals respectively. A sensitivity analysis has been also realized to investigate the influence of volcanic
cloud altitude and water vapour profile on SO2 retrievals at 7.3 and 8.6 mm. Results confirm the high sensitivity of the 7.3 mm retrieval to the volcanic cloud altitude and show that the SO2 total masses estimated at
7.3 and 8.6 mm separately can be used to improve the information on the plume height. Finally, the water vapour profile is used to compute the minimum altitude over which the 7.3 mm retrieval is effective.
Type
article
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Corradini-et-al_Annals-of-Geophysics_2014.pdf

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