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A new method for the validation of the GOMOS high resolution temperature profiles products

机译:用于验证Gomos高分辨率温度型材产品的新方法

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摘要

This article proposes a new validation method for GOMOS HRTP atmospheric temperature and density profiles, with the aim of detecting and removing 0.2 to 5 km scale vertical structures in order to minimise the impact of atmospheric artefacts in the comparison exercises. The proposed approach is based on the use of the “Morlet” Continuous Wavelet Transformation (CWT), for the characterisation and removal of non-stationary and localised vertical structures, in order to produce wave-free profiles of atmospheric temperature and density. Comparison of wave-free temperature/density profiles and wavy structures profiles with those estimated from a limited number of collocated SHADOZ soundings for the years of 2003, 2004 and 2008, is discussed in detail. First results suggest that the proposed approach could lead to a significantly improved HRTP validation scheme, in terms of reduced uncertainties in the estimated biases. Furthermore, this method may be adopted for the study of the vertical component of gravity waves from high spatial/temporal resolution data.
机译:本文提出了一种用于Gomos HRTP大气温度和密度型材的新验证方法,目的是检测和去除0.2至5km刻度垂直结构,以最小化大气人工制品在比较练习中的影响。所提出的方法基于使用“Morlet”连续小波变换(CWT),用于表征和去除非静止和局部垂直结构,以产生大气温度和密度的无波形轮廓。有限于2003年,2004和2008年的有限数量的并置ShadoOZooz探测的波动温度/密度谱和波浪结构谱的比较是详细讨论的。第一个结果表明,就估计偏见的不确定性降低了,该方法可能导致HRTP验证方案显着改善。此外,可以采用该方法来研究来自高空间/时间分辨率数据的重心波的垂直分量。

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