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Can ozone depletion and global warming interact to produce rapid climate change?

The atmosphere displays modes of variability whose structures exhibit a strong longitudinally symmetric (annular) component that extends from the surface to the stratosphere in middle and high latitudes of both hemispheres. In the past 30 years, these modes have exhibited trends that seem larger tha...

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Detalhes bibliográficos
Main Authors: Hartmann, Dennis L., Wallace, John M., Limpasuvan, Varavut, Thompson, David W. J., Holton, James R.
Formato: Artigo
Idioma:Inglês
Publicado em: The National Academy of Sciences 2000
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC26447/
https://ncbi.nlm.nih.gov/pubmed/10677475
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