Synergetic aerosol layer observation after the 2015 Calbuco volcanic eruption event

• Published in: Remote Sensing
• Main Authors: LOPES, FABIO J.S., SILVA, JONATAN J., MARRERO, JUAN C.A., TAHA, GHASSAN, LANDULFO, EDUARDO
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2019
• Subjects: volcanoes; ashes; aerosols; boundary layers; atmospheric circulation; optical radar; south america; air quality; Argentina; Pacific; Uruguay; Aerosol Robotic Network
• Online Access: http://repositorio.ipen.br/handle/123456789/30036; https://doi.org/10.3390/rs11020195

On 22 April 2015, the Calbuco volcano in Chile (Lat: 41.33 S, Long: 72.62 W) erupted after 43 years of inactivity followed by a great amount of aerosol injection into the atmosphere. The pyroclastic material dispersed into the atmosphere posed a potential threat to aviation traffic and air quality over affected a large area. The plumes and debris spread from its location to Patagonian and Pampean regions, reaching the Atlantic and Pacific Oceans and neighboring countries, such as Argentina, Brazil and Uruguay, driven by the westerly winds at these latitudes. The presence of volcanic aerosol layers could be identified promptly at the proximities of Calbuco and afterwards by remote sensing using satellites and lidars in the path of the dispersed aerosols. The Cloud-Aerosol Lidar and Pathfinder Satellite Observations (CALIPSO), Moderate Resolution Imaging Spectroradiometer (MODIS) on board of AQUA/TERRA satellites and Ozone Mapping and Profiler Suite (OMPS) on board of Suomi National Polar-orbiting Partnership (Suomi NPP) satellite were the space platforms used to track the injected layers and a multi-channel lidar system from Latin America Lidar Network (LALINET) SPU Lidar station in South America allowed us to get the spatial and temporal distribution of Calbuco ashes after its occurrence. The SPU lidar stations co-located Aerosol Robotic Network (AERONET) sunphotometers to help in the optical characterization. Here, we present the volcanic layer transported over S??o Paulo area and the detection of aerosol plume between 18 and 20 km. The path traveled by the volcanic aerosol to reach the Metropolitan Area of S??o Paulo (MASP) was tracked by CALIPSO and the aerosol optical and geometrical properties were retrieved at some points to monitor the plume evolution. Total attenuated backscatter profile at 532 nm obtained by CALIPSO revealed the height range extension of the aerosol plume between 18 and 20 km and are in agreement with SPU lidar range corrected signal at 532 nm. The daily evolution of Aerosol Optical ...