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Updated: Aug 15, 2026

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Cuantificación del transporte entre las latitudes tropicales y medias de la estratosfera inferior

Volk1, Elkins, Fahey

  • 1C. M. Volk, G. S. Dutton, and J. M. Gilligan are with the Climate Monitoring and Diagnostics Laboratory (CMDL), National Oceanic and Atmospheric Administration (NOAA), Boulder, CO 80303, and the Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, CO 80309, USA. J. W. Elkins is with NOAA/CMDL, Boulder, CO 80303, USA. D. W. Fahey is with the NOAA Aeronomy Laboratory, Boulder, CO 80303, USA. R. J. Salawitch and J. J. Margitan are with the Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA. M. H. Proffitt is with the NOAA Aeronomy Laboratory, Boulder, CO 80303, and CIRES, University of Colorado, Boulder, CO 80309, USA. M. Loewenstein, J. R. Podolske, and K. R. Chan are with the NASA Ames Research Center, Moffett Field, CA 94035, USA. K. Minschwaner is with the Department of Physics, New Mexico Institute of Mining and Technology, Socorro, NM 87801, USA.

Science (New York, N.Y.)
|June 21, 1996
PubMed
Resumen

El aire de latitudes medias entra en la estratosfera tropical más lentamente de lo que se suponía, lo que hace que el ozono de latitudes medias sea más sensible al cloro industrial. Este hallazgo impacta las predicciones para el agotamiento del ozono y las emisiones de aviones supersónicos.

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