V23B-3096
Characterization and initial field test of a long wave thermal infrared hyperspectral imager for measuring SO2 in volcanic plumes

Tuesday, 15 December 2015
Poster Hall (Moscone South)
Andrea Gabrieli1, Robert Wright2, John Nolan Porter1, Paul G Lucey3, Sarah Crites2, Harold Garbeil4, Eric J Pilger3,4 and Mark Wood3,4, (1)Univ. of Hawaii, Hawaii Institute of Geophysics and Planetology, Honolulu, HI, United States, (2)University of Hawaii at Manoa, Honolulu, HI, United States, (3)Hawaii Inst Geophys & Planetol, Honolulu, HI, United States, (4)HIGP, Honolulu, HI, United States
Abstract:
The ability to quantify volcanic SO2 and image the spatial distribution in plumes either by day or by night would be beneficial to volcanologists. In this project, a newly developed remote sensing long-wave thermal infrared imaging hyperspectral sensor, was tested. The system employs a Sagnac interferometer and an uncooled microbolometer in rapid scanning configuration. This instrument is able to collect hyperspectral images of the scene between 8 and 14 and for each pixel a spectrum containing 50 samples can be retrieved. Images are spectrally and radiometrically calibrated using an IR source with a narrow band filter and two black bodies. The sensitivity of the system was studied by using a gas cell containing various known concentrations of SO2, which are representative of those found in volcanic plumes. Measured spectra were compared with theoretical spectra obtained from MODTRAN5 with the same viewing geometry and spectral resolution as the sensor. The MODTRAN5 calculations were carried out using a radiative transfer algorithm which accounts for the transmission and emission both inside and outside of the gas cell. These preliminary results and field measurements at Kīlauea volcano, Hawai’i will be discussed demonstrating the performance of the system and the ability of retrieving SO2 plume concentrations.