Tomographic Retrievals of Hunga Tonga‐Hunga Ha'apai Volcanic Aerosol. Issue 3 (1st February 2023)

• Record Type: Journal Article
• Authors: Bourassa, Adam E.; Zawada, Daniel J.; Rieger, Landon A.; Warnock, Taran W.; Toohey, Matthew; Degenstein, Doug A.
• Is Part Of: Geophysical research letters. Volume 50:Issue 3(2023)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2023-02-01
• Subjects: Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1029/2022GL101978
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: The 2022 eruption of the Hunga Tonga‐Hunga Ha'apai volcano caused substantial impacts on the atmosphere, including a massive injection of water vapor, and the largest increase in stratospheric aerosol for 30 years. The Ozone Mapping and Profiler Suite (OMPS) Limb Profiler instrument has been critical in monitoring the amount and spread of the volcanic aerosol in the stratosphere. We show that the rapid imagery from the OMPS instrument enables a tomographic retrieval of the aerosol extinction that reduces a critical bias of up to a factor of two, and improves vertical structure and agreement with coincident lidar and occultation observations. Due to the vertically thin and heterogeneous nature of the volcanic aerosol, this impacts integrated values of aerosol across latitude, altitude, and time for several months. We also investigate the systematic impact of uncertainty in assumed particle size that result in an underestimation of the aerosol extinction at the peak of the volcanic aerosol layer. Plain Language Summary: The Hunga Tonga‐Hunga Ha'apai volcano erupted in 2022. The eruption plume went higher into the atmosphere than ever observed before in the modern age. It also carried large amounts of water vapor and other gases and particles, called aerosols, into the stratosphere. The NASA satellite instrument, called the Ozone Mapping and Profiler Suite (OMPS) Limb Profiler, has given us valuable measurements of these aerosols, which are helpful in understanding the impact the volcanic eruption might have on climate. We use an advanced technique to analyze the OMPS measurements that provides a clearer view of the plume. This analysis gives somewhat different results about the thickness of the volcanic plume than the standard method. Key Points: Tomographic retrievals reduce a critical bias in Ozone Mapping and Profiler Suite Limb Profiler volcanic aerosol extinction, improving agreement with Cloud‐Aerosol Lidar and Infrared Pathfinder Satellite Observation and Stratospheric Aerosol and Gas Experiment III/International Space Station Biases of up to a factor of two extend beyond the early plume, with zonal, temporal, and altitude integrated values affected for months Uncertainty in particle size distribution also has an impact that should be considered when analyzing aerosol loading