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首页> 外文期刊>Geophysical Research Letters >DISTINCTIVE OZONE STRUCTURE IN THE HIGH-LATITUDE STRATOSPHERE - MEASUREMENTS BY THE MILLIMETER-WAVE ATMOSPHERIC SOUNDER
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DISTINCTIVE OZONE STRUCTURE IN THE HIGH-LATITUDE STRATOSPHERE - MEASUREMENTS BY THE MILLIMETER-WAVE ATMOSPHERIC SOUNDER

机译:高纬度平流层的独特臭氧结构-毫米波大气声场测量

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摘要

MAS (Millimeter-wave Atmospheric Sounder) observations from the shuttle ATLAS spacelab pallet have revealed some little known (and unexplained) structure in stratospheric ozone mixing ratio profiles at sub-polar latitudes, of both hemispheres. Qualitatively similar features are observed by UARS instruments. Another possibly related feature has been observed by ground-based remote sensing from the South Pole over an extended season. In all these cases, it seems likely that active photochemistry and highly structured horizontal and vertical transport play important roles. Some evidence of a similar feature is also present in a current 2-D photochemical model. This high latitude phenomenon is both an intriguing challenge for current 3-D models and potentially useful test for validating remote sensing experiments. [References: 11]
机译:从航天飞机ATLAS航天器托盘进行的MAS(毫米波大气探测仪)观测发现,在两个半球的亚极纬度的平流层臭氧混合比剖面中,存在一些鲜为人知(且无法解释)的结构。 UARS仪器观察到质上相似的特征。在延长的季节中,通过南极的地面遥感观测到了另一个可能相关的特征。在所有这些情况下,活跃的光化学和高度结构化的水平和垂直传输似乎都可能发挥重要作用。当前的二维光化学模型中也存在类似特征的一些证据。这种高纬度现象既是当前3-D模型的一个有趣挑战,也是验证遥感实验的潜在有用测试。 [参考:11]

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