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The Lower Atmosphere Response to Seismic Events Using Satellite Data waves excited during seismic events. The temperature time series of the atmosphere temperature
Coherence of temporal variations (2-30 days) in the wind field of the midlatitude middle atmosphere of the EarthCurrent work is dedicated to the investigation of the coherency between wave processes at heights
Waves in air impurities and their influence on atmospheric optical properties with respect to periodicity and wave structure of the pollutants/gases. The gas and aerosol concentrations
Anomalous seismo-electromagnetic emission related with seismic waves, with different to atmospherics spectrum signature. On the base of actual data records, the cases of generation
Wave Activity and Its Changes in the Troposphere and Stratosphere of the Northern Hemisphere in Winters of 1979–2016 on the latitude, atmospheric layer, and zonal wave number.
Waves in air impurities and their influence on atmospheric optical properties with respect to periodicity and wave structure of the pollutants/gases. The gas and aerosol concentrations
Coherence of temporal variations (2-30 days) in the wind field of the midlatitude middle atmosphere of the EarthCurrent work is dedicated to the investigation of the coherency between wave processes at heights
Local and planetary scales of wave disturbances for synchronous measurements of atmospheric admixturesThat atmospheric waves exist at different spatiotemporal scales has been demonstrated
Structure of rotational spectra of vectorial wave fields in the middle atmosphere velocity was investigated. An analysis is carried out using Atmospheric Assimilated Data acquired from
Wave interactions in midlatitude middle atmosphere of the EarthInvestigation of wave interactions in heights of the upper mesosphere - lower thermosphere
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