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| Format: | Recurso digital |
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Zenodo
2026
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| Online Access: | https://doi.org/10.5281/zenodo.20157201 |
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Table of Contents:
- <p>Code for calculating thermal tropopause height based on the <span class="hover:entity-accent entity-underline inline cursor-pointer align-baseline"><span class="whitespace-normal">World Meteorological Organization</span></span> definition (1957), following the method of <span class="hover:entity-accent entity-underline inline cursor-pointer align-baseline"><span class="whitespace-normal">Reichler et al (2003). The datasets contain tropopause heights over Antarctica derived from radiosonde observations and multiple reanalyses.</span></span></p> <p><strong><span class="hover:entity-accent entity-underline inline cursor-pointer align-baseline"><span class="whitespace-normal">References</span></span></strong></p> <p><span class="hover:entity-accent entity-underline inline cursor-pointer align-baseline"><span class="whitespace-normal">Reichler, T., Dameris, M., & Sausen, R. (2003). Determining the tropopause height from gridded data. <em>Geophysical Research Letters</em>, <em>30(20)</em>, 2042. https://doi.org/10.1029/2003GL018240</span></span></p> <p class="MsoNormal">World Meteorological Organization. (1957). Meteorology: a three–dimensional science, second session of the commission for aerology. <em>WMO Bull</em>, <em>4(4)</em>, 134–138.</p>