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Aircraft measurements of gravity waves in the upper troposphere and lower stratosphere during the START08 field experiment

机译:Start08现场实验期间对流层上层和较低平流层中的重力波的飞机测量

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This study analyzes in situ airborne measurements from the 2008 Stratosphere-Troposphere Analyses of Regional Transport (START08) experiment to characterize gravity waves in the extratropical upper troposphere and lower stratosphere (ExUTLS). The focus is on the second research flight (RF02), which took place on 21-22 April 2008. This was the first airborne mission dedicated to probing gravity waves associated with strong upper-tropospheric jet-front systems. Based on spectral and wavelet analyses of the in situ observations, along with a diagnosis of the polarization relationships, clear signals of mesoscale variations with wavelengths similar to 50-500 km are found in almost every segment of the 8 h flight, which took place mostly in the lower stratosphere. The aircraft sampled a wide range of background conditions including the region near the jet core, the jet exit and over the Rocky Mountains with clear evidence of vertically propagating gravity waves of along-track wavelength between 100 and 120 km. The power spectra of the horizontal velocity components and potential temperature for the scale approximately between similar to 8 and similar to 256 km display an approximate -5/3 power law in agreement with past studies on aircraft measurements, while the fluctuations roll over to a -3 power law for the scale approximately between similar to 0.5 and similar to 8 km (except when this part of the spectrum is activated, as recorded clearly by one of the flight segments). However, at least part of the high-frequency signals with sampled periods of similar to 20-similar to 60s and wavelengths of similar to 5-similar to 15 km might be due to intrinsic observational errors in the aircraft measurements, even though the possibilities that these fluctuations may be due to other physical phenomena (e.g., nonlinear dynamics, shear instability and/or turbulence) cannot be completely ruled out.
机译:本研究分析了来自2008年地区运输(Start08)实验的2008年平流层 - 对流层分析的原位空中测量分析,以表征具有额外上层对流层和较低平流层(Exutls)的重力波。该重点是在2008年4月21日至22日举行的第二次研究航班(RF02)。这是第一个专门用于探测与强大上层射流射流系统相关的重力波的机载任务。基于原位观察的光谱和小波分析,随着偏振关系的诊断,几乎在8小时飞行中的几乎每个段中都发现了波长的Mesoscale变化的清晰信号,其中几乎每一段都在大部分时间在较低的平流层中。该飞机采样了各种背景条件,包括射流附近的区域,喷射射流和落基山脉,清晰地证明沿轨道波长在100到120 km之间的重力波。水平速度分量的功率光谱和尺寸的潜在温度大致与8之间的尺寸和类似于256km显示近似-5/3电力法,同时与飞机测量的过去的研究相一致,同时波动滚动到a - 3尺度大约与0.5之间的尺度且类似于8km的权力法(除了通过其中一个飞行段清楚地记录的频谱被激活而被激活。然而,具有类似于20-相似的预测周期的至少一部分高频信号,类似于60秒和波长的相似与5 km相似,这可能是由于飞机测量中的内在观测误差,即使可能性这些波动可能是由于其他物理现象(例如,非线性动力学,剪切不稳定性和/或湍流)不能完全排除出来。

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