首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >The SPARC Data Initiative: Comparison of upper troposphere/lower stratosphere ozone climatologies from limb-viewing instruments and the nadir-viewing Tropospheric Emission Spectrometer
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The SPARC Data Initiative: Comparison of upper troposphere/lower stratosphere ozone climatologies from limb-viewing instruments and the nadir-viewing Tropospheric Emission Spectrometer

机译:SPARC数据计划:通过肢体观测仪器和天底观测对流层发射光谱仪比较对流层/平流层下部臭氧的气候

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We present the first comprehensive intercomparison of currently available satellite ozone climatologies in the upper troposphere/lower stratosphere (UTLS) (300–70 hPa) as part of the Stratosphere-troposphere Processes and their Role in Climate (SPARC) Data Initiative. The Tropospheric Emission Spectrometer (TES) instrument is the only nadir-viewing instrument in this initiative, as well as the only instrument with a focus on tropospheric composition. We apply the TES observational operator to ozone climatologies from the more highly vertically resolved limb-viewing instruments. This minimizes the impact of differences in vertical resolution among the instruments and allows identification of systematic differences in the large-scale structure and variability of UTLS ozone. We find that the climatologies from most of the limb-viewing instruments show positive differences (ranging from 5 to 75%) with respect to TES in the tropical UTLS, and comparison to a "zonal mean" ozonesonde climatology indicates that these differences likely represent a positive bias for p ≤ 100 hPa. In the extratropics, there is good agreement among the climatologies regarding the timing andmagnitude of the ozone seasonal cycle (differences in the peak-to-peak amplitude of <15%) when the TES observational operator is applied, as well as very consistent midlatitude interannual variability. The discrepancies in ozone temporal variability are larger in the tropics, with differences between the data sets of up to 55% in the seasonal cycle amplitude. However, the differences among the climatologies are everywhere much smaller than the range produced by current chemistry-climate models, indicating that the multiple-instrument ensemble is useful for quantitatively evaluating these models.
机译:作为平流层-对流层过程及其在气候(SPARC)数据计划中的作用的一部分,我们将对流层上/平流层较低(UTLS)(300–70 hPa)中当前可用的卫星臭氧气候进行首次全面的比对。对流层发射光谱仪(TES)仪器是该计划中唯一的最低点观测仪器,也是唯一关注对流层组成的仪器。我们将TES观测员从垂直分辨率更高的肢体观测仪器应用于臭氧气候。这样可以最大程度地减少仪器之间垂直分辨率差异的影响,并可以识别UTLS臭氧的大规模结构和变异性中的系统差异。我们发现,大多数肢体观察仪器的气候相对于热带UTLS中的TES表现出正差异(从5%到75%),并且与“区域平均”臭氧探空仪气候相比,这些差异可能代表了p≤100 hPa的正偏压。在温带地区,当使用TES观测算子时,关于臭氧季节周期的时间和幅度(峰-峰幅度的差异<15%)以及非常一致的中纬度年际气候之间存在着很好的一致性。变化性。在热带地区,臭氧的时间变异性差异更大,数据集之间的差异最大为季节性周期幅度的55%。然而,气候之间的差异到处都比当前化学-气候模型所产生的范围小得多,这表明多仪器合奏可用于定量评估这些模型。

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