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TitleTropospheric weather influenced by solar wind through atmospheric vertical coupling downward control
AuthorPrikryl, P; Bruntz, R; Tsukijihara, T; Iwao, K; Muldrew, D B; Rusin, V; Rybanský, M; Turna, M; Stastný, P
SourceJournal of Atmospheric and Terrestrial Physics ., https://doi.org/10.1016/j.jastp.2017.07.023
Alt SeriesNatural Resources Canada, Contribution Series 20170092
PublisherElsevier
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
Illustrationsgraphs; plots
ProgramNorthern Canada Geohazards Project, Public Safety Geoscience
AbstractOccurrence of severe weather in the context of solar wind coupling to the magnetosphere-ionosphere-atmosphere (MIA) system is investigated. It is observed that significant snowfall, wind and heavy rain, particularly if caused by low pressure systems in winter, tend to follow arrivals of high-speed solar wind. Previously published statistical evidence that explosive extratropical cyclones in the northern hemisphere tend to occur within a few days after arrivals of high-speed solar wind streams from coronal holes (Prikryl et al., 2009; 2016) is corroborated for the southern hemisphere. Cases of severe weather events are examined in the context of the magnetosphere-ionosphere-atmosphere (MIA) coupling. Physical mechanism to explain these observations is proposed. The leading edge of high-speed solar wind streams is a locus of large-amplitude magneto-hydrodynamic waves that modulate Joule heating and/or Lorentz forcing of the high-latitude lower thermosphere generating medium-scale atmospheric gravity waves that propagate upward and downward through the atmosphere. Simulations of gravity wave propagation in a model atmosphere using the Transfer Function Model (Mayr et al., 1990) reveal that propagating waves originating in the lower thermosphere can excite a spectrum of gravity waves in the lower atmosphere. In spite of significantly reduced amplitudes but subject to amplification upon reflection in the upper troposphere, these gravity waves can provide a lift of unstable air to release instabilities in the troposphere and initiate convection to form cloud/precipitation bands. It is primarily the energy provided by release of latent heat that leads to intensification of storms. These results indicate that vertical coupling in the atmosphere exerts downward control from solar wind to the lower atmospheric levels influencing tropospheric weather development.
Summary(Plain Language Summary, not published)
Space weather refers to the dynamic conditions on the Sun and in the space environment, in particular, in the near-Earth environment, that can affect critical infrastructure. NRCan operates the Canadian Space Weather Forecast Centre and conducts research into space weather effects on power systems, pipelines, radio communications and GNSS positioning to help Canadian industry understand and mitigate the effects of space weather. This paper examines a possible influence of solar wind disturbances on the lower atmosphere affecting tropospheric weather through vertical coupling between the upper and lower atmosphere.
GEOSCAN ID302706