Open AccessVolcanic ash and SO 2 in the 2008 Kasatochi eruption: Retrievals comparison from different IR satellite sensors
Author(s) -
Corradini S.,
Merucci L.,
Prata A. J.,
Piscini A.
Publication year - 2010
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2009jd013634
Subject(s) - volcanic ash , atmospheric infrared sounder , moderate resolution imaging spectroradiometer , environmental science , volcano , satellite , vulcanian eruption , remote sensing , spectroradiometer , radiative transfer , atmosphere (unit) , atmospheric sciences , geology , explosive eruption , meteorology , reflectivity , magma , troposphere , physics , seismology , astronomy , quantum mechanics , optics
The Kasatochi 2008 eruption was detected by several infrared satellite sensors including Moderate Resolution Imaging Spectroradiometer (MODIS), Advanced Very High Resolution Radiometer (AVHRR), and Atmospheric Infrared Sounder (AIRS). In this work a comparison between the volcanic cloud SO 2 and ash retrievals derived from these instruments has been undertaken. The SO 2 retrieval is carried out by using both the 7.3 and 8.7 μ m absorption features while ash retrieval exploits the 10–12 μ m atmospheric window. A radiative transfer scheme is also used to correct the volcanic ash effect on the 8.7 μ m SO 2 signature. As test cases, three near‐contemporary images for each sensor, collected during the first days of the eruption, have been analyzed. The results show that the volcanic SO 2 and ash are simultaneously present and generally collocated. The MODIS and AVHRR total ash mass loadings are in good agreement and estimated to be about 0.5 Tg, while the AIRS retrievals are slightly lower and equal to about 0.3 Tg. The AIRS and MODIS 7.3 μ m SO 2 mass loadings are also in good agreement and vary between 0.3 and 1.2 Tg, while the MODIS ash corrected 8.7 μ m SO 2 masses vary between 0.4 and 2.7 Tg. The mass increase with time confirms the continuous SO 2 injection in the atmosphere after the main explosive episodes. Moreover the difference between the 7.3 and 8.7 μ m retrievals suggests a vertical stratification of the volcanic cloud. The results also confirm the importance of the ash correction; the corrected 8.7 μ m SO 2 total masses are less than 30–40% of the uncorrected values.