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30-year lidar observations of the stratospheric aerosol layer state over Tomsk (Western Siberia, Russia)

DOI:10.5194/acp-2016-792 期刊:Atmospheric Chemistry and Physics Discussions 出版年份:2016 更新时间:2025-09-09 09:28:46
摘要: There are only four lidar stations in the world, which have almost continuously performed observations of the stratospheric aerosol layer (SAL) state for over the last 30 years. The longest time series of the SAL lidar measurements have been accumulated at the Mauna Loa Observatory (Hawaii) since 1973, the NASA Langley Research Center (Hampton, Virginia) since 1974, and Garmisch-Partenkirchen (Germany) since 1976. The fourth lidar station we present started to perform routine observations of the SAL parameters in Tomsk (56.48° N, 85.05° E, Western Siberia, Russia) in 1986. In this paper, we mainly focus on and discuss the stratospheric background period from 2000 to 2005 and the causes of the SAL perturbations over Tomsk in the 2006–2015 period. During the last decade, volcanic aerosol plumes from tropical Mt. Manam, Soufriere Hills, Rabaul, Merapi, Nabro, and Kelut, and extratropical (northern) Mt. Okmok, Kasatochi, Redoubt, Sarychev Peak, Eyjafjallaj?kull, and Grimsv?tn were detected in the stratosphere over Tomsk. When it was possible, we used the NOAA HYSPLIT trajectory model to assign aerosol layers observed over Tomsk to the corresponding volcanic eruptions. The trajectory analysis highlighted some surprising results. For example, in cases of the Okmok, Kasatochi, and Eyjafjallaj?kull eruptions, the HYSPLIT air-mass backward trajectories, started from altitudes of aerosol layers detected over Tomsk with a lidar, passed over these volcanoes on their eruption days at altitudes higher than the maximum plume altitudes given by the Smithsonian Institution Global Volcanism Program. An explanation of these facts is suggested. The role of both tropical and northern volcanoes eruptions in volcanogenic aerosol loading of the mid-latitude stratosphere is also discussed. In addition to volcanoes, we considered other possible causes of the SAL perturbations over Tomsk, i.e. the polar stratospheric cloud (PSC) events and smoke plumes from strong forest fires. At least two PSC events were detected in 1995 and 2007. We also make an assumption that both the Kelut volcano plume (Indonesia, February 2014) and smoke plumes from massive forest fires occurred in Canada (137 fires in the Northwest Territories, July 2014) and the USA (the Happy Camp Complex fire in California, August–October 2014), with equal probability, could be the cause of the SAL perturbations over Tomsk during the first quarter of 2015.
作者: Vladimir V. Zuev,Vladimir D. Burlakov,Aleksei V. Nevzorov,Vladimir L. Pravdin,Ekaterina S. Savelieva,Vladislav V. Gerasimov
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To analyze the state of the stratospheric aerosol layer over Tomsk, Western Siberia, Russia, over a 30-year period, focusing on the background period from 2000 to 2005 and the causes of perturbations from 2006 to 2015, including volcanic eruptions, polar stratospheric clouds, and forest fires.

The 30-year lidar observations in Tomsk have provided valuable insights into the state of the stratospheric aerosol layer, highlighting the dominant role of tropical volcanoes in volcanogenic aerosol loading of the mid-latitude stratosphere. The study also identified the contributions of northern volcanoes, polar stratospheric clouds, and forest fires to SAL perturbations. The findings underscore the importance of continuous monitoring and the need for an extensive network of lidar stations to better understand stratospheric aerosol dynamics.

The study is limited by the geographical coverage of the lidar station in Tomsk, which may not capture all SAL perturbations over the vast area of Siberia. Additionally, the identification of aerosol layers' sources relies on trajectory analysis, which may not always be precise due to the complexity of atmospheric transport processes.

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