Arctic spring and summertime aerosol optical depth baseline from long-term observations and model reanalyses – Part 2: Statistics of extreme AOD events, and implications for the impact of regional biomass burning processes

• Published in: Atmospheric chemistry and physics Vol. 22; no. 15; pp. 9949 - 9967
• Main Authors: Xian, Peng, Zhang, Jianglong, O'Neill, Norm T, Reid, Jeffrey S, Toth, Travis D, Sorenson, Blake, Hyer, Edward J, Campbell, James R, Ranjbar, Keyvan
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau Copernicus GmbH 03.08.2022; Copernicus Publications
• Subjects: Aerosol analysis; Aerosol optical depth; Aerosol particles; Aerosol Robotic Network; Aerosols; Agriculture; Analysis; Anthropogenic factors; Arctic aerosols; Biomass; Biomass burning; Burning; Climate; Climate change; Climatic analysis; Climatic changes; Climatology; Clouds; Extreme values; Human influences; Lightning; Lightning frequencies; Optical analysis; Optical thickness; Photometers; Polar environments; Pollution; Precipitation; Remote sensing; Satellites; Smoke; Spring; Spring (season); Statistical analysis; Statistical methods; Statistics; Summer; Trend analysis; Trends; Arctic Ocean; United States > US; Arctic region
• ISSN: 1680-7324; 1680-7316; 1680-7324
• DOI: 10.5194/acp-22-9949-2022

In a companion paper (Xian et al., 2022, part 1 of the study), we present an Arctic aerosol optical depth (AOD) climatology and trend analysis for 2003-2019 spring and summertime periods derived from a combination of aerosol reanalyses, remote-sensing retrievals, and ground observations. Continued from the previous discussion and as the second part of the study, we report the statistics and trends of Arctic AOD extreme events using the U.S. Navy Aerosol Analysis and Prediction System ReAnalysis version 1 (NAAPS-RA v1), the sun photometer data from the AErosol RObotic NETwork (AERONET) sites, and the oceanic Maritime Aerosol Network (MAN) measurements. Here, extreme AOD events are defined as events with AOD exceeding the 95th percentile (denoted "AOD.sub.95 ") of AOD distributions for given locations using 6-hourly or daily AOD data. While AERONET and MAN data estimate the Arctic median 550 nm AOD value to be 0.07, the 95th percentile value is 0.24. Such extreme events are dominated by fine-mode aerosol particles, largely attributable to biomass burning (BB) smoke events for the North American Arctic, the Asian Arctic, and most areas of the Arctic Ocean. However, extreme AOD events for the lower European Arctic are more attributable to anthropogenic and biogenic fine particles. The extreme-event occurrence dominance of sea salt is largely limited to the North Atlantic and Norwegian Sea. The extreme AOD amplitudes of anthropogenic and biogenic fine-mode and sea salt AOD are, however, significantly lower than those regions where extreme smoke AOD is dominant. Even for sites distant from BB source regions, BB smoke is the principal driver of AOD variation above the AOD.sub.95 threshold.