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    Upper-tropospheric pollutants observed by MIPAS: geographic and seasonal variations by N. Glatthor, G. P. Stiller, T. von Clarmann, B. Funke, S. Kellmann, A. Linden

    Published 2025-01-01
    “…The southern hemispheric <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M10" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi mathvariant="normal">Δ</mi><mrow class="chem"><msub><mi mathvariant="normal">C</mi><mn mathvariant="normal">2</mn></msub><msub><mi mathvariant="normal">H</mi><mn mathvariant="normal">6</mn></msub></mrow><mo>/</mo><mi mathvariant="normal">Δ</mi><mrow class="chem"><mi mathvariant="normal">HCN</mi></mrow></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="74pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="ef4c16a1fc51e58a967532eec31bd8b5"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-25-1175-2025-ie00001.svg" width="74pt" height="14pt" src="acp-25-1175-2025-ie00001.png"/></svg:svg></span></span> ERs obtained during August to October are in good agreement with the emission ratio for savanna fires. …”
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