Complex Aerosol Experiment in Western Siberia (April – October 2013)

• Main Authors: Matvienko G.G., Belan B.D., Panchenko M.V., Romanovskii O.A., Sakerin S.M., Kabanov D.M., Turchinovich S.A., Turchinovich Yu.S., Eremina T.A., Kozlov V.S., Terpugova S.A., Pol’kin V.V., Yausheva E.P., Chernov D.G., Zuravleva T.B., Bedareva T.V., Odintsov S.L., Burlakov V.D., Arshinov M.Yu., Ivlev G.A., Savkin D.E., Fofonov A.V., Gladkikh V.A., Kamardin A.P., Balin Yu.S., Kokhanenko G.P., Penner I.E., Samoilova S.V., Antokhin P.N., Arshinova V.G., Davydov D.K., Kozlov A.V., Pestunov D.A., Rasskazchikova T.M., Simonenkov D.V., Sklyadneva T.K., Tolmachev G.N., Belan S.B., Shmargunov V.P.
• Format: Article
• Language: English
• Published: EDP Sciences 2016-01-01
• Series: EPJ Web of Conferences
• Online Access: http://dx.doi.org/10.1051/epjconf/201611924003

The primary project objective was to accomplish the Complex Aerosol Experiment, during which the aerosol properties should be measured in the near-ground layer and free atmosphere. Three measurement cycles were performed during the project implementation: in spring period (April), when the maximum of aerosol generation is observed; in summer (July), when atmospheric boundary layer height and mixing layer height are maximal; and in late summer – early autumn (October), when the secondary particle nucleation period is recorded. Numerical calculations were compared with measurements of fluxes of downward solar radiation. It was shown that the relative differences between model and experimental values of fluxes of direct and total radiation, on the average, do not exceed 1% and 3% respectively.