Forcing Mechanism of Normal Mode Rossby Waves

简正模罗斯贝波的强迫机制

基本信息

  • 批准号:
    07640574
  • 负责人:
  • 金额:
    $ 1.41万
  • 依托单位:
  • 依托单位国家:
    日本
  • 项目类别:
    Grant-in-Aid for Scientific Research (C)
  • 财政年份:
    1995
  • 资助国家:
    日本
  • 起止时间:
    1995 至 1996
  • 项目状态:
    已结题

项目摘要

Normal mode Rossby waves are westward traveling free waves of the atmosphere with characteristic periods of 5-20 days. The present study consists of analyzes of observed data obtained by satellite measurements and numerical simulation by the use of general circulation models (GCMs).1 Results based on analyzes of observed data :(1) Global structures of 5-day and 10-day waves are firstly shown in the mesosphere by the use of UARS/ISAMS data obtained through NASA.(2) Both the 5-day and 10-day waves are gradually with height in the upper mesosphere ; nonetheless 10-day waves have large amplitudes in the winter hemisphere.2 Results based on GCM simulation :(1) Simulated 5-day waves have vertical and horizontal structure very similar to that of observed ones and appear irregularly with a lifetime of about one month.(2) Detailed analyzes for 5-day waves and precipitations show the evidence that 5-days wave activities are inclined to be largely enhanced when anomalies in the precipitation field of zonal wavenumber 1 are large with a westward period of 5 days.(3) 5-day waves also appear in conditions of no mountains and/or no land-sea contrast ; hence these are probably unimportant for excitation of the waves. However, 5-day wave activities are significantly weak in case of removal of the latent heat release.
常模Rossby波是大气中向西传播的自由波,其特征周期为5-20天。本文分析了卫星观测资料和利用大气环流模式(GCMS)进行数值模拟的结果:(1)利用美国国家航空航天局(NASA)的UARS/ISAMS资料首次在中层显示了全球5天和10天波的结构,(2)5天波和10天波在中层上层都是逐渐变高的;基于GCM模拟的结果表明:(1)模拟的5日波与实测波的垂直和水平结构非常相似,出现的周期约为1个月.(2)对5日波和降水的详细分析表明,当纬向波数1的降水场异常较大,且周期为5天时,5天波的活动倾向于显著增强.(3)5天波在无山和/或无海陆对比的情况下也出现,因此对激发浪可能不重要.然而,在潜热释放去除的情况下,5日波活动明显较弱。

项目成果

期刊论文数量(2)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
A.Kohsiek: "Periods of planetary waves in geomagnetic variations" Ann.Geophysicae. 13. 168-176 (1995)
A.Kohsiek:“地磁变化中的行星波周期”Ann.Geophysicae。
  • DOI:
  • 发表时间:
  • 期刊:
  • 影响因子:
    0
  • 作者:
  • 通讯作者:
三好勉信: "大気大循環モデル中のノーマルモード・ロスビー波の構造と出現特性について" 大気圏シンポジウム. 10. 13-16 (1996)
三好勉信:“论大气环流模式中正态罗斯贝波的结构和表现特征”,大气研讨会,10. 13-16 (1996)。
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  • 影响因子:
    0
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HIROOKA Toshihiko其他文献

HIROOKA Toshihiko的其他文献

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{{ truncateString('HIROOKA Toshihiko', 18)}}的其他基金

Dynamical processes in the mesosphere and the lower thermosphere during sudden stratospheric warmings
平流层突然变暖期间中层和低层热层的动力学过程
  • 批准号:
    24340113
  • 财政年份:
    2012
  • 资助金额:
    $ 1.41万
  • 项目类别:
    Grant-in-Aid for Scientific Research (B)
Research on 320 Gbit/s-500 km OTDM Transmission Technology
320 Gbit/s-500 km OTDM传输技术研究
  • 批准号:
    19686024
  • 财政年份:
    2007
  • 资助金额:
    $ 1.41万
  • 项目类别:
    Grant-in-Aid for Young Scientists (A)
Modeling and quantification of the solar influence on the terrestrial atmosphere
太阳对陆地大气影响的建模和量化
  • 批准号:
    17340140
  • 财政年份:
    2005
  • 资助金额:
    $ 1.41万
  • 项目类别:
    Grant-in-Aid for Scientific Research (B)
DYNAMICAL STUDIES ON THE FORMATION OF PLANETARY WAVES.
行星波形成的动力学研究。
  • 批准号:
    13640440
  • 财政年份:
    2001
  • 资助金额:
    $ 1.41万
  • 项目类别:
    Grant-in-Aid for Scientific Research (C)
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