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We present theoretical work directed toward improving our understanding of the mesoscale influence of deep convection on its tropospheric environment through forced gravity waves. From the linear, hydrostatic, non-rotating, incompressible equations,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::04676eb09eb1d1c5cddb76b86f5726de
https://eprints.whiterose.ac.uk/128507/8/Halliday_et_al-2018-Quarterly_Journal_of_the_Royal_Meteorological_Society.pdf
https://eprints.whiterose.ac.uk/128507/8/Halliday_et_al-2018-Quarterly_Journal_of_the_Royal_Meteorological_Society.pdf
Autor:
Spendlove J; Materials & Engineering Research Institute, Sheffield Hallam University, Howard Street, Sheffield S1 1WB, United Kingdom., Xu X; Materials & Engineering Research Institute, Sheffield Hallam University, Howard Street, Sheffield S1 1WB, United Kingdom.; Department of Engineering and Mathematics, Sheffield Hallam University, Howard Street, Sheffield S1 1WB, United Kingdom., Halliday OJ; National Centre for Atmospheric Science, Department of Meteorology, University of Reading, Reading RG6 6AH, United Kingdom., Schenkel T; Materials & Engineering Research Institute, Sheffield Hallam University, Howard Street, Sheffield S1 1WB, United Kingdom.; Department of Engineering and Mathematics, Sheffield Hallam University, Howard Street, Sheffield S1 1WB, United Kingdom., Halliday I; Materials & Engineering Research Institute, Sheffield Hallam University, Howard Street, Sheffield S1 1WB, United Kingdom.
Publikováno v:
Physical review. E [Phys Rev E] 2020 Jul; Vol. 102 (1-1), pp. 013309.
