EPJ Web of Conferences (Jan 2016)
Complex Aerosol Experiment in Western Siberia (April – October 2013)
- 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.
Affiliations
- 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.
- DOI
- https://doi.org/10.1051/epjconf/201611924003
- Journal volume & issue
-
Vol. 119
p. 24003
Abstract
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.
