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Systematic change in global patterns of streamflow following volcanic eruptions
Following large explosive volcanic eruptions precipitation decreases over much of the globe1–6, particularly in climatologically wet regions4,5. Stratospheric volcanic aerosols reflect sunlight, which reduces evaporation, whilst surface cooling stabilises the atmosphere and reduces its water-holding...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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2015
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4894545/ https://www.ncbi.nlm.nih.gov/pubmed/27279897 http://dx.doi.org/10.1038/ngeo2545 |