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The SPARC water vapour assessment II: comparison of annual, semi-annual and quasi-biennial variations in stratospheric and lower mesospheric water vapour observed from satellites

机译:SPARC水蒸气评估II:从卫星观测到的平流层和中低层水蒸气的年度,半年度和准两年期变化的比较

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摘要

In the framework of the second SPARC (Stratosphere-troposphere Processes Andtheir Role in Climate) water vapour assessment (WAVAS-II), the amplitudes andphases of the annual, semi-annual and quasi-biennial variation instratospheric and lower mesospheric water were compared using 30 datasets from 13 different satellite instruments. These comparisons aimed toprovide a comprehensive overview of the typical uncertainties in theobservational database which can be considered in subsequent observationaland modelling studies. For the amplitudes, a good agreement of their latitudeand altitude distribution was found. Quantitatively there were differences inparticular at high latitudes, close to the tropopause and in the lowermesosphere. In these regions, the standard deviation over all data setstypically exceeded 0.2 ppmv for the annual variation and 0.1 ppmv for thesemi-annual and quasi-biennial variation. For the phase, larger differencesbetween the data sets were found in the lower mesosphere. Generally thesmallest phase uncertainties can be observed in regions where the amplitudeof the variability is large. The standard deviations of the phases for alldata sets were typically smaller than a month for the annual and semi-annualvariation and smaller than 5 months for the quasi-biennial variation. Theamplitude and phase differences among the data sets are caused by acombination of factors. In general, differences in the temporal variation ofsystematic errors and in the observational sampling play a dominant role. Inaddition, differences in the vertical resolution of the data, the consideredtime periods and influences of clouds, aerosols as well as non-localthermodynamic equilibrium (NLTE) effects cause differences between theindividual data sets.
机译:在第二次SPARC(平流层-对流层过程及其在气候中的作用)水蒸气评估(WAVAS-II)的框架中,使用30来比较平流层和较低中层水的年,半年度和准两年期变化的幅度和阶段。来自13种不同卫星仪器的数据集。这些比较旨在对观测数据库中典型的不确定性提供全面的概述,这些不确定性可以在后续的观测和陆地建模研究中加以考虑。对于振幅,发现了它们的纬度和高度分布的良好一致性。定量上存在差异,特别是在高纬度,对流层顶和中下层地区。在这些区域中,所有数据的标准偏差通常每年变化超过0.2µppmv,而这些半年度和准两年期变化均超过0.1µppmv。对于该阶段,在较低的中球层中发现了数据集之间的较大差异。通常,在变化幅度较大的区域中可以观察到最小的相位不确定性。所有数据集的阶段标准偏差通常小于一个月的年度和半年度变化,小于五个月的准每两年变化。数据集之间的幅度和相位差异是由多种因素引起的。通常,系统误差的时间变化和观测采样的差异起主要作用。此外,数据垂直分辨率的差异,考虑的时间段以及云,气溶胶的影响以及非局部热力学平衡(NLTE)的影响会导致各个数据集之间的差异。

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