비의류제품

numerical study of an observed orographic mesoscale convective system. i. simulated genesis and comparison with observations

  • 출판일1999.03
  • 저자
  • 서지사항
  • 등록일 2016.11.02
  • 조회수 476
the interaction of topographically induced thermally and mechanically driven diurnal flow regimes in the lee of the rockies is shown to lead to the growth of a mesoscale convective system (mcs). an orographic mcs observed during the 1977 combined south park area cumulus experiment and high plains experiment is numerically simulated with a two-dimensional nonhydrostatic cloud model covering spatial scales of 1000 km. in this numerical investigation, meso gamma -, meso beta - and meso alpha -scales of motion are represented simultaneously. as a result, interesting features of cloud-mesoscale interaction are predicted that cannot be represented in cloud parameterization frameworks
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