Impact of Infrared Atmospheric Sounding Interferometer (IASI) thermal infrared measurements on global ozone reanalyses

<p>The information content of thermal infrared measurements for tropospheric ozone (O<span class="inline-formula"><sub>3</sub></span>) estimation has already been well demonstrated. However, the impact of such measurements to constrain modelled O<span class...

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Main Authors: E. Emili, M. El Aabaribaoune
Format: Article
Language:English
Published: Copernicus Publications 2021-10-01
Series:Geoscientific Model Development
Online Access:https://gmd.copernicus.org/articles/14/6291/2021/gmd-14-6291-2021.pdf
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author E. Emili
M. El Aabaribaoune
author_facet E. Emili
M. El Aabaribaoune
author_sort E. Emili
collection DOAJ
description <p>The information content of thermal infrared measurements for tropospheric ozone (O<span class="inline-formula"><sub>3</sub></span>) estimation has already been well demonstrated. However, the impact of such measurements to constrain modelled O<span class="inline-formula"><sub>3</sub></span> distributions within global assimilation systems is not yet unequivocal. A new tropospheric O<span class="inline-formula"><sub>3</sub></span> reanalysis is computed for the year 2010 by means of assimilating measurements from the Infrared Atmospheric Sounding Interferometer (IASI) within the MOdéle pour la Chimie Á Grande Echelle (MOCAGE) chemical transport model. The objective is to evaluate the impact of recent methodological improvements of the data assimilation scheme on the O<span class="inline-formula"><sub>3</sub></span> distribution. The new O<span class="inline-formula"><sub>3</sub></span> reanalysis (named IASI-r) and its precursor (IASI-a) have been validated against ozonesondes, and compared to independent estimations of tropospheric O<span class="inline-formula"><sub>3</sub></span> and to results from two state-of-the-art products based on detailed tropospheric chemistry (the Goddard Earth Observing System with a coupled chemistry–climate model, GEOS-CCM, and the Copernicus Atmosphere Monitoring Service, CAMS, reanalysis). The main difference between IASI-r and IASI-a concerns the treatment of IASI observations, with radiances being assimilated directly in IASI-r instead of intermediate Level 2 O<span class="inline-formula"><sub>3</sub></span> retrievals. IASI-r is found to correct major issues with IASI-a, such as the neutral or negative impact of IASI assimilation in the extra-tropics and the presence of residual biases in the tropics. IASI-r also compares relatively well to the CAMS reanalysis, which is based on a more comprehensive chemical mechanism and the assimilation of several ultraviolet (UV) and microwave measurements.</p>
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spelling doaj.art-c14f553421e04a8c89ea2e6b344073542022-12-21T23:11:21ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032021-10-01146291630810.5194/gmd-14-6291-2021Impact of Infrared Atmospheric Sounding Interferometer (IASI) thermal infrared measurements on global ozone reanalysesE. EmiliM. El Aabaribaoune<p>The information content of thermal infrared measurements for tropospheric ozone (O<span class="inline-formula"><sub>3</sub></span>) estimation has already been well demonstrated. However, the impact of such measurements to constrain modelled O<span class="inline-formula"><sub>3</sub></span> distributions within global assimilation systems is not yet unequivocal. A new tropospheric O<span class="inline-formula"><sub>3</sub></span> reanalysis is computed for the year 2010 by means of assimilating measurements from the Infrared Atmospheric Sounding Interferometer (IASI) within the MOdéle pour la Chimie Á Grande Echelle (MOCAGE) chemical transport model. The objective is to evaluate the impact of recent methodological improvements of the data assimilation scheme on the O<span class="inline-formula"><sub>3</sub></span> distribution. The new O<span class="inline-formula"><sub>3</sub></span> reanalysis (named IASI-r) and its precursor (IASI-a) have been validated against ozonesondes, and compared to independent estimations of tropospheric O<span class="inline-formula"><sub>3</sub></span> and to results from two state-of-the-art products based on detailed tropospheric chemistry (the Goddard Earth Observing System with a coupled chemistry–climate model, GEOS-CCM, and the Copernicus Atmosphere Monitoring Service, CAMS, reanalysis). The main difference between IASI-r and IASI-a concerns the treatment of IASI observations, with radiances being assimilated directly in IASI-r instead of intermediate Level 2 O<span class="inline-formula"><sub>3</sub></span> retrievals. IASI-r is found to correct major issues with IASI-a, such as the neutral or negative impact of IASI assimilation in the extra-tropics and the presence of residual biases in the tropics. IASI-r also compares relatively well to the CAMS reanalysis, which is based on a more comprehensive chemical mechanism and the assimilation of several ultraviolet (UV) and microwave measurements.</p>https://gmd.copernicus.org/articles/14/6291/2021/gmd-14-6291-2021.pdf
spellingShingle E. Emili
M. El Aabaribaoune
Impact of Infrared Atmospheric Sounding Interferometer (IASI) thermal infrared measurements on global ozone reanalyses
Geoscientific Model Development
title Impact of Infrared Atmospheric Sounding Interferometer (IASI) thermal infrared measurements on global ozone reanalyses
title_full Impact of Infrared Atmospheric Sounding Interferometer (IASI) thermal infrared measurements on global ozone reanalyses
title_fullStr Impact of Infrared Atmospheric Sounding Interferometer (IASI) thermal infrared measurements on global ozone reanalyses
title_full_unstemmed Impact of Infrared Atmospheric Sounding Interferometer (IASI) thermal infrared measurements on global ozone reanalyses
title_short Impact of Infrared Atmospheric Sounding Interferometer (IASI) thermal infrared measurements on global ozone reanalyses
title_sort impact of infrared atmospheric sounding interferometer iasi thermal infrared measurements on global ozone reanalyses
url https://gmd.copernicus.org/articles/14/6291/2021/gmd-14-6291-2021.pdf
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