The distribution of dust particles in the stratosphere affects the location of the tropical rainband. The possible implications of this for geoengineering — by injection of particles — need to be taken into account before implementation.
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References
Guha-Sapir, D., Santos, I. & Borde, A. (eds) The Economic Impacts of Natural Disasters (Oxford Univ. Press, 2013).
Hsiang, S. M., Meng, K. C. & Cane, M. A. Nature 476, 438–441 (2011).
Haywood, J. M., Jones, A., Bellouin, N. & Stephenson, D. Nature Clim. Change 3, 660–665 (2013).
Sinclair, A. R. E. & Fryxell, J. M. Can. J. Zool. 63, 987–994 (1985).
Giannini, A., Biasutti, M., Held, I. M. & Sobel, A. H. Climatic Change 90, 359–383 (2008).
Goddard, L. et al. Int. J. Climatol. 21, 1111–1152 (2001).
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Kushnir, Y. Volcanic rain shift. Nature Clim Change 3, 619–620 (2013). https://doi.org/10.1038/nclimate1941
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DOI: https://doi.org/10.1038/nclimate1941