Spatiotemporal evolution of stratospheric smoke plume during late Summer 2017 from CALIPSO and Haute-Provence lidar observations

• Main Authors: Khaykin, Sergey, Godin-Beekmann, Sophie, Hauchecorne, Alain, Pelon, Jacques, Ravetta, François, Keckhut, Philippe
• Other Authors: TROPO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), STRATO - LATMOS
• Format: Conference Object
• Language: English
• Published: HAL CCSD 2018
• Subjects: [SDU.OCEAN]Sciences of the Universe [physics]/Ocean; Atmosphere; Canada; Lake Athabasca
• Online Access: https://insu.hal.science/insu-04415573

International audience Extreme pyro-convection (PyroCb) events triggered by wildfires in northwest Canada and U.S. during Summer 2017 resulted in vast injection of combustion products into the stratosphere. The stratospheric smoke plume was observed by 532 nm and 355 nm lidars at Observatoire de Haute-Provence (OHP) in southern France during many weeks that followed PyroCb events as distinct aerosol layers at altitudes between 14 and 19.5 km. The aerosol backscatter and optical depth of the smoke layers were reaching unprecedentedly high values for a non-volcanic aerosol layer in the three-decade OHP lidar observation record. We use space-borne CALIPSO lidar (CALIOP) and OMPS UV aerosol index (AI) observations together with trajectory analysis to track the spatiotemporal evolution of the smoke plume in the stratosphere during the first 3 weeks after the major PyroCb events around the lake Athabasca in northwest Canada. While the major stratospheric smoke plume was caused by Athabasca fires in mid-August, other clusters of forest fires in North America have also contributed to polluting the stratosphere. In particular, backward trajectories suggest that stratospheric smoke layer seen above OHP in early September likely originate from PyroCb clusters in northern California and Oregon that occurred in late August. Vertically-resolved CALIOP observations put in evidence that in 19 days the stratospheric smoke plume has ascended from 340 K ( 12 km) to a maximum of 560 K ( 22 km), presumably due to radiative heating of highly-absorptive smoke particles. We note that the primary optically-thick patches of smoke have ascended diabatically with a rate of up to 30 K/day. With that, thinner plumes, mostly remaining at lower levels, have been subjected to fast zonal transport within the jet stream and circled the globe in about two weeks. A remarkable agreement between OHP lidar and CALIOP sampling the same air mass on a particular date allowed us to extrapolate OHP observations to a regional scale, where CALIOP reported ...