首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >The quasi-2day wave activities during 2007 boreal summer period as revealed by Whole Atmosphere Community Climate Model
【24h】

The quasi-2day wave activities during 2007 boreal summer period as revealed by Whole Atmosphere Community Climate Model

机译:整个大气社区气候模式揭示的2007年夏季寒潮的准2天波活动

获取原文
获取原文并翻译 | 示例
           

摘要

The ensemble data assimilation version of the Whole Atmosphere Community Climate Model + Data Assimilation Research Testbed developed at National Center for Atmospheric Research is utilized to study the quasi-2 day wave (QTDW) activities during boreal summer period of 2007. The westward wave number 3 (W3) and 4 (W4) modes intermittently dominated the QTDW oscillations at different times. The W3 peaked 4 times from day 172 to day 224 with the major peak at around days 199–206 being much stronger than the others. The W4 also showed a quadruple structure during the whole summer period but with their amplitudes comparable with each other. The period of W4 increases from ~42 h on day 186 (with stronger easterly jet) to 56 h on day 225 (with weaker easterly jet), while the W3 period is more stable with the maximum perturbation occurring at ~52 h. Thus, the W3 exhibits more normal mode features than W4. Further diagnostic analysis shows that the barotropically/baroclinically unstable regions at middle and low latitudes are more effective for the amplification of W3 with stronger instabilities providing larger forcing. Moreover, the temporal variability of the refractive indexes and critical layers of W4, which are related to the background wind, are responsible for its period variations. We also find that the absence of a westward wave number 2 (W2) QTDW during boreal summer of 2007 is due to the weaker easterly jet compared with that during austral summer.
机译:国家大气研究中心开发的整体大气群落气候模型+数据同化研究试验台的集合数据同化版本用于研究2007年夏季夏季的准2天波(QTDW)活动。西风3号(W3)和4(W4)模式在不同时间间歇性地控制QTDW振荡。从172天到224天,W3达到4次峰值,主要峰值在199-206天左右,比其他峰值要强得多。 W4在整个夏季期间也显示出四重结构,但它们的振幅彼此可比。 W4的时间段从第186天的约42小时(具有较强的东风急流)增加到第225天的56小时(具有较弱的东风急流),而W3的时期更稳定,最大扰动发生在〜52 h。因此,W3比W4具有更多的正常模式功能。进一步的诊断分析表明,中纬度和低纬度的正压/斜压不稳定区域对于W3的放大更为有效,具有更大的不稳定性,从而提供了更大的强迫。此外,与背景风有关的W4的折射率和临界层的时间变化是造成其周期变化的原因。我们还发现,与北方夏季相比,2007年北方夏季缺少西风2号(W2)QTDW是由于东风急流减弱。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号