TY - JOUR
T1 - Smoke of extreme Australian bushfires observed in the stratosphere over Punta Arenas, Chile, in January 2020
T2 - Optical thickness, lidar ratios, and depolarization ratios at 355 and 532 nm
AU - Ohneiser, Kevin
AU - Ansmann, Albert
AU - Baars, Holger
AU - Seifert, Patric
AU - Barja, Boris
AU - Jimenez, Cristofer
AU - Radenz, Martin
AU - Teisseire, Audrey
AU - Floutsi, Athina
AU - Haarig, Moritz
AU - Foth, Andreas
AU - Chudnovsky, Alexandra
AU - Engelmann, Ronny
AU - Zamorano, Felix
AU - Bühl, Johannes
AU - Wandinger, Ulla
N1 - Publisher Copyright: © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.
PY - 2020/7/10
Y1 - 2020/7/10
N2 - We present particle optical properties of stratospheric smoke layers observed with multiwavelength polarization Raman lidar over Punta Arenas (53.2 S, 70.9 W), Chile, at the southernmost tip of South America in January 2020. The smoke originated from the record-breaking bushfires in Australia. The stratospheric aerosol optical thickness reached values up to 0.85 at 532 nm in mid- January 2020. The main goal of this rapid communication letter is to provide first stratospheric measurements of smoke extinction-to-backscatter ratios (lidar ratios) and particle linear depolarization ratios at 355 and 532 nm wavelengths. These aerosol parameters are important input parameters in the analysis of spaceborne CALIPSO and Aeolus lidar observations of the Australian smoke spreading over large parts of the Southern Hemisphere in January and February 2020 up to heights of around 30 km. Lidar and depolarization ratios, simultaneously measured at 355 and 532 nm, are of key importance regarding the homogenization of the overall Aeolus (355 nm wavelength) and CALIPSO (532 nm wavelength) lidar data sets documenting the spread of the smoke and the decay of the stratospheric perturbation, which will be observable over the entire year of 2020. We found typical values and spectral dependencies of the lidar ratio and linear depolarization ratio for aged stratospheric smoke. At 355 nm, the lidar ratio and depolarization ratio ranged from 53 to 97 sr (mean 71 sr) and 0.2 to 0.26 (mean 0.23), respectively. At 532 nm, the lidar ratios were higher (75-112 sr, mean 97 sr) and the depolarization ratios were lower with values of 0.14- 0.22 (mean 0.18). The determined depolarization ratios for aged Australian smoke are in very good agreement with respective ones for aged Canadian smoke, observed with lidar in stratospheric smoke layers over central Europe in the summer of 2017. The much higher 532 nm lidar ratios, however, indicate stronger absorption by the Australian smoke particles.
AB - We present particle optical properties of stratospheric smoke layers observed with multiwavelength polarization Raman lidar over Punta Arenas (53.2 S, 70.9 W), Chile, at the southernmost tip of South America in January 2020. The smoke originated from the record-breaking bushfires in Australia. The stratospheric aerosol optical thickness reached values up to 0.85 at 532 nm in mid- January 2020. The main goal of this rapid communication letter is to provide first stratospheric measurements of smoke extinction-to-backscatter ratios (lidar ratios) and particle linear depolarization ratios at 355 and 532 nm wavelengths. These aerosol parameters are important input parameters in the analysis of spaceborne CALIPSO and Aeolus lidar observations of the Australian smoke spreading over large parts of the Southern Hemisphere in January and February 2020 up to heights of around 30 km. Lidar and depolarization ratios, simultaneously measured at 355 and 532 nm, are of key importance regarding the homogenization of the overall Aeolus (355 nm wavelength) and CALIPSO (532 nm wavelength) lidar data sets documenting the spread of the smoke and the decay of the stratospheric perturbation, which will be observable over the entire year of 2020. We found typical values and spectral dependencies of the lidar ratio and linear depolarization ratio for aged stratospheric smoke. At 355 nm, the lidar ratio and depolarization ratio ranged from 53 to 97 sr (mean 71 sr) and 0.2 to 0.26 (mean 0.23), respectively. At 532 nm, the lidar ratios were higher (75-112 sr, mean 97 sr) and the depolarization ratios were lower with values of 0.14- 0.22 (mean 0.18). The determined depolarization ratios for aged Australian smoke are in very good agreement with respective ones for aged Canadian smoke, observed with lidar in stratospheric smoke layers over central Europe in the summer of 2017. The much higher 532 nm lidar ratios, however, indicate stronger absorption by the Australian smoke particles.
UR - http://www.scopus.com/inward/record.url?scp=85088412398&partnerID=8YFLogxK
U2 - 10.5194/acp-20-8003-2020
DO - 10.5194/acp-20-8003-2020
M3 - مقالة
SN - 1680-7316
VL - 20
SP - 8003
EP - 8015
JO - Atmospheric Chemistry and Physics
JF - Atmospheric Chemistry and Physics
IS - 13
M1 - angeo-38-815-2020
ER -