Summer daily dynamics of the vertical structure of atmospheric aerosol over Baikal coastal area from ground-based lidar measurements

• Published in: International journal of remote sensing Vol. 45; no. 22; pp. 8576 - 8593
• Main Authors: Nasonov, S. V., Balin, Yu. S., Klemasheva, M. G., Kokhanenko, G. P., Nasonova, A.S., Novoselov, M. M., Penner, I. E.
• Format: Journal Article
• Language: English
• Published: London Taylor & Francis 16-11-2024; Taylor & Francis Ltd
• Subjects: Aerosol layers; Aerosols; Air circulation; Air flow; Air masses; Altitude; Anticyclones; Atmosphere; Atmospheric aerosols; Atmospheric boundary layer; Atmospheric circulation; Atmospheric fronts; Breeze circulation; Circulation types; Coastal structures; Coastal zone; Coastal zones; Cyclones; Dynamic structural analysis; Fronts; Lake Baikal; Lakes; LIDAR; Lidar measurements; Lower atmosphere; Meteorological parameters; Parameter identification; Regional analysis; Summer; Vertical profiles; Volume transport
• ISSN: 0143-1161; 1366-5901
• DOI: 10.1080/01431161.2024.2403623

The spatial structure of atmospheric aerosol over Baikal in summer is studied on a regular basis with the use of ground-based LOSA-M2 lidar measurements at the Boyarsky scientific station of the Institute of Physical Material Science, Siberian Branch, Russian Academy of Sciences (51.83°N, 106.06°E, 456 m a.s.l.), Republic of Buryatia, Russia. The lake is located in a basin surrounded by mountain ranges on all side; its water volume is large. The lidar data are analysed along with the regional meteorological situation and meteorological parameters of the atmosphere. The daily dynamics of aerosol distribution over the atmospheric is examined for the period from 2015 to 2023 accounting the effect of different air masses in the region. Three main typical air circulation types are identified for the coastal zone of southern Baikal in summer, which determine the atmospheric aerosol generation and transport. The first and most common type relates to breeze circulation, where the main changes in the spatial structure of aerosol occur in the 2-3-km layer and are determined by changes in the transport direction within a breeze cell during the day. The main feature of this type is a decrease in the altitude of an air layer which contains most of aerosol in the lower atmosphere up to 1 km. The second type refers to southwestern transport under the presence of an anticyclone over the region. The maximal altitude of the aerosol layers attains 7 km in this case. The most complex and dynamic changes in the daily spatial structure of atmospheric aerosol occurred under transport of cyclones and associated atmospheric fronts over Lake Baikal. Under this third type, the altitude of the aerosol layers decreases throughout the day within the altitude range from the surface to 3-4 km.