A global total column ozone climate data record

<p>Total column ozone (TCO) data from multiple satellite-based instruments have been combined to create a single near-global daily time series of ozone fields at 1.25<span class="inline-formula"><sup>∘</sup></span> longitude by 1<span class="inline-for...

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Main Authors: G. E. Bodeker, J. Nitzbon, J. S. Tradowsky, S. Kremser, A. Schwertheim, J. Lewis
Format: Article
Language:English
Published: Copernicus Publications 2021-08-01
Series:Earth System Science Data
Online Access:https://essd.copernicus.org/articles/13/3885/2021/essd-13-3885-2021.pdf
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spelling doaj-ae3659bff7bf4043b4addae6e49e58f92021-08-11T09:34:06ZengCopernicus PublicationsEarth System Science Data1866-35081866-35162021-08-01133885390610.5194/essd-13-3885-2021A global total column ozone climate data recordG. E. Bodeker0G. E. Bodeker1J. Nitzbon2J. Nitzbon3J. S. Tradowsky4S. Kremser5A. Schwertheim6J. Lewis7Bodeker Scientific, 42 Russell Street, Alexandra, 9320, New ZealandSchool of Geography, Environment and Earth Sciences, Victoria University of Wellington, Wellington, New ZealandBodeker Scientific, 42 Russell Street, Alexandra, 9320, New ZealandPermafrost Research Section, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, GermanyBodeker Scientific, 42 Russell Street, Alexandra, 9320, New ZealandBodeker Scientific, 42 Russell Street, Alexandra, 9320, New ZealandBodeker Scientific, 42 Russell Street, Alexandra, 9320, New ZealandBodeker Scientific, 42 Russell Street, Alexandra, 9320, New Zealand<p>Total column ozone (TCO) data from multiple satellite-based instruments have been combined to create a single near-global daily time series of ozone fields at 1.25<span class="inline-formula"><sup>∘</sup></span> longitude by 1<span class="inline-formula"><sup>∘</sup></span> latitude spanning the period 31 October 1978 to 31 December 2016. Comparisons against TCO measurements from the ground-based Dobson and Brewer spectrophotometer networks are used to remove offsets and drifts between the ground-based measurements and a subset of the satellite-based measurements. The corrected subset is then used as a basis for homogenizing the remaining data sets. The construction of this database improves on earlier versions of the database maintained first by the National Institute of Water and Atmospheric Research (NIWA) and now by Bodeker Scientific (BS), referred to as the NIWA-BS TCO database. The intention is for the NIWA-BS TCO database to serve as a climate data record for TCO, and to this end, the requirements for constructing climate data records, as detailed by GCOS (the Global Climate Observing System), have been followed as closely as possible.</p> <p>This new version includes a wider range of satellite-based instruments, uses updated sources of satellite data, extends the period covered, uses improved statistical methods to model the difference fields when homogenizing the data sets, and, perhaps most importantly, robustly tracks uncertainties from the source data sets through to the final climate data record which is now accompanied by associated uncertainty fields. Furthermore, a gap-free TCO database (referred to as the BS-filled TCO database) has been created and is documented in this paper. The utility of the NIWA-BS TCO database is demonstrated through an analysis of ozone trends from November 1978 to December 2016. Both databases are freely available for non-commercial purposes: the DOI for the NIWA-BS TCO database is <a href="https://doi.org/10.5281/zenodo.1346424">https://doi.org/10.5281/zenodo.1346424</a> <span class="cit" id="xref_paren.1">(<a href="#bib1.bibx10">Bodeker et al.</a>, <a href="#bib1.bibx10">2018</a>)</span> and is available from <span class="uri">https://zenodo.org/record/1346424</span>. The DOI for the BS-filled TCO database is <a href="https://doi.org/10.5281/zenodo.3908787">https://doi.org/10.5281/zenodo.3908787</a> <span class="cit" id="xref_paren.2">(<a href="#bib1.bibx11">Bodeker et al.</a>, <a href="#bib1.bibx11">2020</a>)</span> and is available from <span class="uri">https://zenodo.org/record/3908787</span>. In addition, both data sets are available from <span class="uri">http://www.bodekerscientific.com/data/total-column-ozone</span> (last access: June 2021).</p>https://essd.copernicus.org/articles/13/3885/2021/essd-13-3885-2021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author G. E. Bodeker
G. E. Bodeker
J. Nitzbon
J. Nitzbon
J. S. Tradowsky
S. Kremser
A. Schwertheim
J. Lewis
spellingShingle G. E. Bodeker
G. E. Bodeker
J. Nitzbon
J. Nitzbon
J. S. Tradowsky
S. Kremser
A. Schwertheim
J. Lewis
A global total column ozone climate data record
Earth System Science Data
author_facet G. E. Bodeker
G. E. Bodeker
J. Nitzbon
J. Nitzbon
J. S. Tradowsky
S. Kremser
A. Schwertheim
J. Lewis
author_sort G. E. Bodeker
title A global total column ozone climate data record
title_short A global total column ozone climate data record
title_full A global total column ozone climate data record
title_fullStr A global total column ozone climate data record
title_full_unstemmed A global total column ozone climate data record
title_sort global total column ozone climate data record
publisher Copernicus Publications
series Earth System Science Data
issn 1866-3508
1866-3516
publishDate 2021-08-01
description <p>Total column ozone (TCO) data from multiple satellite-based instruments have been combined to create a single near-global daily time series of ozone fields at 1.25<span class="inline-formula"><sup>∘</sup></span> longitude by 1<span class="inline-formula"><sup>∘</sup></span> latitude spanning the period 31 October 1978 to 31 December 2016. Comparisons against TCO measurements from the ground-based Dobson and Brewer spectrophotometer networks are used to remove offsets and drifts between the ground-based measurements and a subset of the satellite-based measurements. The corrected subset is then used as a basis for homogenizing the remaining data sets. The construction of this database improves on earlier versions of the database maintained first by the National Institute of Water and Atmospheric Research (NIWA) and now by Bodeker Scientific (BS), referred to as the NIWA-BS TCO database. The intention is for the NIWA-BS TCO database to serve as a climate data record for TCO, and to this end, the requirements for constructing climate data records, as detailed by GCOS (the Global Climate Observing System), have been followed as closely as possible.</p> <p>This new version includes a wider range of satellite-based instruments, uses updated sources of satellite data, extends the period covered, uses improved statistical methods to model the difference fields when homogenizing the data sets, and, perhaps most importantly, robustly tracks uncertainties from the source data sets through to the final climate data record which is now accompanied by associated uncertainty fields. Furthermore, a gap-free TCO database (referred to as the BS-filled TCO database) has been created and is documented in this paper. The utility of the NIWA-BS TCO database is demonstrated through an analysis of ozone trends from November 1978 to December 2016. Both databases are freely available for non-commercial purposes: the DOI for the NIWA-BS TCO database is <a href="https://doi.org/10.5281/zenodo.1346424">https://doi.org/10.5281/zenodo.1346424</a> <span class="cit" id="xref_paren.1">(<a href="#bib1.bibx10">Bodeker et al.</a>, <a href="#bib1.bibx10">2018</a>)</span> and is available from <span class="uri">https://zenodo.org/record/1346424</span>. The DOI for the BS-filled TCO database is <a href="https://doi.org/10.5281/zenodo.3908787">https://doi.org/10.5281/zenodo.3908787</a> <span class="cit" id="xref_paren.2">(<a href="#bib1.bibx11">Bodeker et al.</a>, <a href="#bib1.bibx11">2020</a>)</span> and is available from <span class="uri">https://zenodo.org/record/3908787</span>. In addition, both data sets are available from <span class="uri">http://www.bodekerscientific.com/data/total-column-ozone</span> (last access: June 2021).</p>
url https://essd.copernicus.org/articles/13/3885/2021/essd-13-3885-2021.pdf
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