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Regional and global trace gas distributions and inferred transports in the upper troposphere and lower stratosphere

机译:对流层和平流层下部的区域和全球痕量气体分布和推断的运移

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Trace gas mixing ratios were measured in the upper troposphere and lower stratosphere during the second mission of the Cryogenic Infrared Spectrometers and Telescopes (CRISTA) experiment in August 1997. Water vapor data at high vertical and horizontal resolution are presented here. Respective data for CFC 11 (CFCl3) are given in a future paper by V. Kuell et al. (Tropopause region temperatures and CFC 11 mixing ratios from CRISTA 2, submitted to Journal of Geophysical Research, 2004). Some ozone data are also available. Zonal mean mixing ratios of water vapor are compared to several other measurements, and good agreement is obtained. Data variance of all three gases is high and is mostly attributable to atmospheric fluctuations rather than instrument noise. Diffusive (“eddy”) fluxes were derived from these fluctuations for all three gases. They were converted to meridional eddy coefficients Kyy by means of respective mixing ratio gradients.
机译:在1997年8月进行的低温红外光谱仪和望远镜(CRISTA)实验的第二个任务期间,测量了对流层上层和平流层下层的痕量气体混合比。此处显示了高垂直和水平分辨率下的水蒸气数据。 V. Kuell等人在未来的论文中提供了CFC 11(CFCl3)的相应数据。 (来自CRISTA 2的更年期区域温度和CFC 11混合比已提交给《地球物理研究杂志》,2004年)。还提供了一些臭氧数据。将水蒸气的区域平均混合比与其他几个测量结果进行比较,可以得出很好的一致性。三种气体的数据差异很大,并且主要是由于大气波动而不是仪器噪声引起的。从所有三种气体的这些波动中得出了扩散(“涡”)通量。通过各自的混合比梯度将它们转换为子午涡流系数Kyy。

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