Retrieval of volcanic SO2 from HIRS/2 using optimal estimation

We present an optimal-estimation (OE) retrieval scheme for stratospheric sulfur dioxide from the HighResolution Infrared Radiation Sounder 2 (HIRS/2) instruments on the NOAA and MetOp platforms, an infrared radiometer that has been operational since 1979. This algorithm is an improvement upon a prev...

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Main Authors: Miles, G, Siddans, R, Grainger, R, Prata, A, Fisher, B, Krotkov, N, Kerridge, B
Format: Journal article
Published: European Geosciences Union 2018
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author Miles, G
Siddans, R
Grainger, R
Prata, A
Fisher, B
Krotkov, N
Kerridge, B
author_facet Miles, G
Siddans, R
Grainger, R
Prata, A
Fisher, B
Krotkov, N
Kerridge, B
author_sort Miles, G
collection OXFORD
description We present an optimal-estimation (OE) retrieval scheme for stratospheric sulfur dioxide from the HighResolution Infrared Radiation Sounder 2 (HIRS/2) instruments on the NOAA and MetOp platforms, an infrared radiometer that has been operational since 1979. This algorithm is an improvement upon a previous method based on channel brightness temperature differences, which demonstrated the potential for monitoring volcanic SO2 using HIRS/2. The Prata method is fast but of limited accuracy. This algorithm uses an optimal-estimation retrieval approach yielding increased accuracy for only moderate computational cost. This is principally achieved by fitting the column water vapour and accounting for its interference in the retrieval of SO2. A cloud and aerosol model is used to evaluate the sensitivity of the scheme to the presence of ash and water/ice cloud. This identifies that cloud or ash above 6 km limits the accuracy of the water vapour fit, increasing the error in the SO2 estimate. Cloud top height is also retrieved. The scheme is applied to a case study event, the 1991 eruption of Cerro Hudson in Chile. The total erupted mass of SO2 is estimated to be 2300 kT ± 600 kT. This confirms it as one of the largest events since the 1991 eruption of Pinatubo, and of comparable scale to the Northern Hemisphere eruption of Kasatochi in 2008. This retrieval method yields a minimum mass per unit area detection limit of 3 DU, which is slightly less than that for the Total Ozone Mapping Spectrometer (TOMS), the only other instrument capable of monitoring SO2 from 1979 to 1996. We show an initial comparison to TOMS for part of this eruption, with broadly consistent results. Operating in the infrared (IR), HIRS has the advantage of being able to measure both during the day and at night, and there have frequently been multiple HIRS instruments operated simultaneously for better than daily sampling. If applied to all data from the series of past and future HIRS instruments, this method presents the opportunity to produce a comprehensive and consistent volcanic SO2 time series spanning over 40 years.
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spelling oxford-uuid:7845dd57-2e7e-474d-9d28-ccfe447bd6d22022-03-26T20:29:36ZRetrieval of volcanic SO2 from HIRS/2 using optimal estimationJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:7845dd57-2e7e-474d-9d28-ccfe447bd6d2Symplectic Elements at OxfordEuropean Geosciences Union2018Miles, GSiddans, RGrainger, RPrata, AFisher, BKrotkov, NKerridge, BWe present an optimal-estimation (OE) retrieval scheme for stratospheric sulfur dioxide from the HighResolution Infrared Radiation Sounder 2 (HIRS/2) instruments on the NOAA and MetOp platforms, an infrared radiometer that has been operational since 1979. This algorithm is an improvement upon a previous method based on channel brightness temperature differences, which demonstrated the potential for monitoring volcanic SO2 using HIRS/2. The Prata method is fast but of limited accuracy. This algorithm uses an optimal-estimation retrieval approach yielding increased accuracy for only moderate computational cost. This is principally achieved by fitting the column water vapour and accounting for its interference in the retrieval of SO2. A cloud and aerosol model is used to evaluate the sensitivity of the scheme to the presence of ash and water/ice cloud. This identifies that cloud or ash above 6 km limits the accuracy of the water vapour fit, increasing the error in the SO2 estimate. Cloud top height is also retrieved. The scheme is applied to a case study event, the 1991 eruption of Cerro Hudson in Chile. The total erupted mass of SO2 is estimated to be 2300 kT ± 600 kT. This confirms it as one of the largest events since the 1991 eruption of Pinatubo, and of comparable scale to the Northern Hemisphere eruption of Kasatochi in 2008. This retrieval method yields a minimum mass per unit area detection limit of 3 DU, which is slightly less than that for the Total Ozone Mapping Spectrometer (TOMS), the only other instrument capable of monitoring SO2 from 1979 to 1996. We show an initial comparison to TOMS for part of this eruption, with broadly consistent results. Operating in the infrared (IR), HIRS has the advantage of being able to measure both during the day and at night, and there have frequently been multiple HIRS instruments operated simultaneously for better than daily sampling. If applied to all data from the series of past and future HIRS instruments, this method presents the opportunity to produce a comprehensive and consistent volcanic SO2 time series spanning over 40 years.
spellingShingle Miles, G
Siddans, R
Grainger, R
Prata, A
Fisher, B
Krotkov, N
Kerridge, B
Retrieval of volcanic SO2 from HIRS/2 using optimal estimation
title Retrieval of volcanic SO2 from HIRS/2 using optimal estimation
title_full Retrieval of volcanic SO2 from HIRS/2 using optimal estimation
title_fullStr Retrieval of volcanic SO2 from HIRS/2 using optimal estimation
title_full_unstemmed Retrieval of volcanic SO2 from HIRS/2 using optimal estimation
title_short Retrieval of volcanic SO2 from HIRS/2 using optimal estimation
title_sort retrieval of volcanic so2 from hirs 2 using optimal estimation
work_keys_str_mv AT milesg retrievalofvolcanicso2fromhirs2usingoptimalestimation
AT siddansr retrievalofvolcanicso2fromhirs2usingoptimalestimation
AT graingerr retrievalofvolcanicso2fromhirs2usingoptimalestimation
AT prataa retrievalofvolcanicso2fromhirs2usingoptimalestimation
AT fisherb retrievalofvolcanicso2fromhirs2usingoptimalestimation
AT krotkovn retrievalofvolcanicso2fromhirs2usingoptimalestimation
AT kerridgeb retrievalofvolcanicso2fromhirs2usingoptimalestimation