15 research outputs found
Genetic diversity of wild reindeer Rangifer tarandus L. from the eastern part of the Kola Peninsula: Polymorphism of the mtDNA control region
Full text linkValue of comparative studies of "real clinical practice" in modern cardiology Position paper based on the expert council discussion dated 12/18/2020
Full text linkMechanism of the Intensification of a Heterogeneous Reduction Reaction with the Liberation of Gas Bubbles
Full text linkEstimating the Abundance of Bottom Fish at the Shelf and Continental Slope in Northern Primorye
Full text linkSpecies composition and seasonal dynamics of ichthyoplankton of the coastal zone of the western part of Peter the Great Bay of the Sea of Japan in 2007–2010
Full text linkRole of microorganisms in water purification of compounds of iron and manganese in a dense layer of sorbent–catalyst
Full text linkComplex Aerosol Experiment in Western Siberia (April – October 2013)
Full text linkThe 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
Complex Aerosol Experiment in Western Siberia (April – October 2013)
Full text linkThe 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
