Can we explain the observed methane variability after the Mount Pinatubo eruption?
The CH<sub>4</sub> growth rate in the atmosphere showed large variations after the Pinatubo eruption in June 1991. A decrease of more than 10 ppb yr<sup>−1</sup> in the growth rate over the course of 1992 was reported, and a partial recovery in the following year. Although several reasons h...
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| Principais autores: | , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Copernicus Publications
2016-01-01
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| coleção: | Atmospheric Chemistry and Physics |
| Assuntos: | |
| Acesso em linha: | https://www.atmos-chem-phys.net/16/195/2016/acp-16-195-2016.pdf |
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