본문 바로 가기

로고

국내 최대 기계 및 로봇 연구정보
통합검색 화살표
  • AFDEX 2D/3D
  • 기술보고서

    기술보고서 게시판 내용
    타이틀 LEE WAVES: BENIGN AND MALIGNANT
    저자 M. G. Wurtele, A. Datta and R. D. Sharman
    Keyword Clear air turbulence; Gravity waves; Inertia-gravity waves; Lee waves
    URL http://www.dfrc.nasa.gov/DTRS/1993/PDF/H-1890.pdf
    보고서번호 NASA-CR-186024
    발행년도 1993
    출처 NASA Dryden Flight Research Center
    ABSTRACT The flow of an incompressible fluid over an obstacle will produce an oscillation in which buoyancy is the restoring force, called a gravity wave. For disturbances of this scale, the atmosphere may be treated as dynamically incompressible, even though there exists a mean static upward density gradient. Even in the linear approximation - i.e., for small disturbances - this model explains a great many of the flow phenomena observed in the lee of mountains. However, nonlinearities do arise importantly, in three ways: (i) through amplification due to the decrease of mean density with height; (ii) through the large (scaled) size of the obstacle, such as a mountain range; and (iii) from dynamically singular levels in the fluid field. These effects produce a complicated array of phenomena - Large departure of the streamlines from their equilibrium levels, high winds, generation of small scales,turbulence, etc. - that present hazards to aircraft and to lee surface areas. The nonlinear disturbances also interact with the larger-scale flow in such a manner as to impact global weather forecasts and the climatological momentum balance. If there is no dynamic barrier, these waves can penetrate vertically into the middle atmosphere (30-100 km), where recent observations show them to be of a length scale that must involve the coriolis force in any modeling. At these altitudes, the amplitude of the waves is very large, and the phenomena associated with these wave dynamics are being studied with a view to their potential impact on high performance aircraft, including the projected National Aerospace Plane (NASP). The presentation herein will show the results of analysis and of state-of-the-art numerical simulations, validated where possible by observational data, and illustrated with photographs from nature.

    서브 사이드

    서브 우측상단1