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.
简正模Rossby波是一种向西传播的大气自由波,其特征周期为5-20天。本研究包括对卫星观测资料的分析和利用大气环流模式进行的数值模拟。1基于观测资料分析的结果:(1)利用NASA提供的UARS/ISAMS资料,首次显示了5天和10天波在中层的全球结构。(2)结果表明:(1)模拟的5日波与观测的5日波具有相似的垂直和水平结构,且不规则,其存在期约为1个月。(2)对5天波和降水的详细分析表明,当纬向波数为1的降水场有较大的向西向周期时,5天波活动有明显增强的趋势。(3)5日波也出现在没有山脉和/或没有海陆对比的条件下;因此这些对于波的激发可能不重要。但在潜热释放消除后,5日波活动明显减弱。

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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    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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