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

<p>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...

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Main Authors: Rosario Quirino Iannone, Stefano Casadio, Bojan Bojkov
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2014-10-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/6487
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spelling doaj-22ca5284b5ac479aa1109f265ca380432020-11-24T22:49:57ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2014-10-0157510.4401/ag-64875974A new method for the validation of the GOMOS high resolution temperature profiles productsRosario Quirino Iannone0Stefano Casadio1Bojan Bojkov2SERCO S.p.A., Frascati,SERCO S.p.A., Frascati, Italy; ESA/ESRIN, Frascati,ESA/ESRIN, Frascati,<p>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.</p>http://www.annalsofgeophysics.eu/index.php/annals/article/view/6487Gomos HRTPAtmospheric wavesTemperature profilesValidationWavelet transform
collection DOAJ
language English
format Article
sources DOAJ
author Rosario Quirino Iannone
Stefano Casadio
Bojan Bojkov
spellingShingle Rosario Quirino Iannone
Stefano Casadio
Bojan Bojkov
A new method for the validation of the GOMOS high resolution temperature profiles products
Annals of Geophysics
Gomos HRTP
Atmospheric waves
Temperature profiles
Validation
Wavelet transform
author_facet Rosario Quirino Iannone
Stefano Casadio
Bojan Bojkov
author_sort Rosario Quirino Iannone
title A new method for the validation of the GOMOS high resolution temperature profiles products
title_short A new method for the validation of the GOMOS high resolution temperature profiles products
title_full A new method for the validation of the GOMOS high resolution temperature profiles products
title_fullStr A new method for the validation of the GOMOS high resolution temperature profiles products
title_full_unstemmed A new method for the validation of the GOMOS high resolution temperature profiles products
title_sort new method for the validation of the gomos high resolution temperature profiles products
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2014-10-01
description <p>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.</p>
topic Gomos HRTP
Atmospheric waves
Temperature profiles
Validation
Wavelet transform
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/6487
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