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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Equatorial Kelvin waves as revealed by EOS Microwave Limb Sounder observations and European Centre for Medium-Range Weather Forecasts analyses: Evidence for slow Kelvin waves of zonal wave number 3
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Equatorial Kelvin waves as revealed by EOS Microwave Limb Sounder observations and European Centre for Medium-Range Weather Forecasts analyses: Evidence for slow Kelvin waves of zonal wave number 3

机译:EOS微波肢体测深仪观测和欧洲中距离天气预报中心分析显示的赤道开尔文波:纬向波数为3的慢开尔文波的证据

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摘要

Temperature and ozone observations from the Microwave Limb Sounder (MLS) on the EOS Aura satellite are used to study equatorial wave activity in the autumn of 2005. In contrast to previous observations for the same season in other years, the temperature anomalies in the middle and lower tropical stratosphere are found to be characterized by a strong wave-like eastward progression with zonal wave number equal to 3. Extended empirical orthogonal function (EOF) analysis reveals that the wave 3 components detected in the temperature anomalies correspond to a slow Kelvin wave with a period of 8 days and a phase speed of 19 m/s. Fluctuations associated with this Kelvin wave mode are also apparent in ozone profiles. Moreover, as expected by linear theory, the ozone fluctuations observed in the lower stratosphere are in phase with the temperature perturbations, and peak around 20–30 hPa where the mean ozone mixing ratios have the steepest vertical gradient. A search for other Kelvin wave modes has also been made using both the MLS observations and the analyses from one experiment where MLS ozone profiles are assimilated into the European Centre for Medium-Range Weather Forecasts (ECMWF) data assimilation system via a 6-hourly 3D var scheme. Our results show that the characteristics of the wave activity detected in the ECMWF temperature and ozone analyses are in good agreement with MLS data.
机译:利用EOS Aura卫星上的微波探空仪(MLS)测得的温度和臭氧,可用于研究2005年秋季的赤道波活动。与其他年份之前同一季节的观测结果相比,中部和中部的温度异常较低的热带平流层以强波状向东传播为特征,纬向波数等于3。扩展的经验正交函数(EOF)分析显示,在温度异常中检测到的波3分量对应于一个慢开尔文波,持续8天,相位速度为19 m / s。与这种开尔文波模式有关的波动在臭氧剖面中也很明显。此外,正如线性理论所期望的那样,在平流层下部观测到的臭氧波动与温度扰动同相,并在20-30 hPa左右达到峰值,其中平均臭氧混合比具有最陡的垂直梯度。还使用MLS观测值和一项实验的分析来搜索其他开尔文波模式,在该实验中,MLS臭氧剖面通过6小时的3D吸收到了欧洲中程天气预报(ECMWF)数据吸收系统var方案。我们的结果表明,在ECMWF温度和臭氧分析中检测到的波活动特征与MLS数据非常吻合。

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