首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Equatorial waves in High Resolution Dynamics Limb Sounder (HIRDLS) data
【24h】

Equatorial waves in High Resolution Dynamics Limb Sounder (HIRDLS) data

机译:高分辨率动力学肢体测深仪(HIRDLS)数据中的赤道波

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

We examine equatorial wave structure in temperature measurements from the High Resolution Dynamics Limb Sounder (HIRDLS) on the Aura satellite. Waves with periods longer than 1 day and zonal wave numbers up to 8 (depending on frequency) are derived from an asynoptic Fourier transform analysis. HIRDLS measurement sampling and resolution afford unprecedented views of the latitude-height structure of equatorial Rossby wave, mixed Rossby-gravity wave, and Kelvin wave modes at altitudes above cloud tops in the tropical upper troposphere and stratosphere. Wave modes with vertical wavelength as short as 4 km can be clearly seen in the data. Kelvin waves comprise a dominant signal throughout the 3 years of HIRDLS measurements, and we further examine time, height, and longitude variations observed in the Kelvin waves. An annual cycle of Kelvin wave temperature amplitudes near the tropopause is observed that may have implications for annual variations in wave-cirrus formation in the tropics. This annual variation can be largely explained by effects of the background wind and stability on Kelvin wave propagation and potential energy in the tropical tropopause layer. At altitudes 20 km and above, the annual cycle gives way to an interannual cycle in Kelvin wave amplitudes that is related to the quasi-biennial oscillation in stratospheric winds. This interannual variation is a signature of Kelvin wave forcing of the descent of westerly winds in the oscillation, and we compute the Kelvin wave fractional contribution to the forcing.
机译:我们通过Aura卫星上的高分辨率动力学肢体测深仪(HIRDLS)在温度测量中检查了赤道波结构。周期大于1天的波和最多8个纬向波数(取决于频率)均来自非光学傅里叶变换分析。 HIRDLS测量采样和分辨率为热带对流层和平流层云顶以上的高度提供了赤道Rossby波,混合Rossby重力波和Kelvin波模式的纬度-高度结构的前所未有的视图。数据中可以清楚地看到垂直波长短至4 km的波模。开尔文波在HIRDLS的3年测量中一直是主要信号,我们将进一步检查开尔文波中观察到的时间,高度和经度变化。观测到对流层顶附近的开尔文波温度振幅的年度周期,这可能对热带地区波浪卷云形成的年度变化有影响。这种年度变化很大程度上可以通过背景风和稳定性对开尔文波传播以及热带对流层顶层中势能的影响来解释。在20公里及以上的海拔高度,年循环被开尔文波振幅的年际循环所取代,这与平流层风的准两年一次振荡有关。这种年际变化是西风在振荡中下降的开尔文波强迫的特征,我们计算了开尔文波对强迫的分数贡献。

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