大氣對流層重力波研究進展
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國家自然科學基金項目41005027、廣西科學基金項目(2011GXNSFA018002、2013GXNSFBB053010、2013GXNSFAA019273)資助


Progresses in Researches on Tropospheric Gravity Waves
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    摘要:

    重力波對暴雨等強對流天氣有著觸發機制的作用,甚至影響著大氣環流、大氣結構和演變。綜合近50年來國內外有關大氣對流層重力波的研究成果,為重力波的進一步研究提供參考。多年研究表明:暴雨等強對流系統、山脈地形等為對流層重力波波源;重力波強度與風垂直切變、背景絕對渦度成正比,傳播速度與波的振幅、水平波寬成正比,重力波在穩定大氣中得到了加強,潛熱加熱有利于重力波的形成;重力波的探測手段為微壓器、衛星、雷達觀測等,通過重力波探測目前基本掌握了重力波的日、月、季節的活動規律。

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    Gravity waves (GWs) play a role in exciting and enhancing typhoons,rainstorms and hail storms, and have myriad effects and major contributions to the circulation, structure, and variability of the atmospheric.The main advancements in tropospheric GWs researches in last 50 years are summarized,which include the sources, dynamical mechanisms, and observation of GWs. Results show that GWs are mainly excited by jet streams, followed by deep convection, mountain terrain, and water vapor. Normally,the strength of GWs is proportional to the vertical wind shear, absolute vorticity, buoyancy frequency, and the frequency of GWs. GWs propagation velocity is proportional to the amplitude and pulse width of GWs. GWs is strengthened in the stability atmosphere. Latent heating is favorable to the formation of GWs, and thermal heating is not. The means of GWs detection include micro pressure devices, satellites,radar, etc. The basic activity regularity of GWs has been founded out through detection in recent years.

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覃衛堅,壽紹文,王詠青.大氣對流層重力波研究進展[J].氣象科技,2013,41(5):864~869

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  • 收稿日期:2012-04-27
  • 定稿日期:2013-03-25
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  • 在線發布日期: 2013-10-31
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