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La restricción isotópica sobre el aumento del ozono troposférico en el siglo XX
Laurence Y Yeung1, Lee T Murray2, Patricia Martinerie3
1Department of Earth, Environmental and Planetary Sciences, Rice University, Houston, TX, USA. lyeung@rice.edu.
Nature
|June 14, 2019
Resumen
El ozono troposférico (O3) aumentó en menos del 40% a finales del siglo XX, según nuevos datos de núcleos de hielo. Este hallazgo se alinea con los modelos climáticos, lo que sugiere un menor impacto que algunas mediciones históricas indicadas.
Área de la Ciencia:
- Química atmosférica
- Paleoclimatología
- Investigación de los gases de efecto invernadero
Sus antecedentes:
- El ozono troposférico (O3) es un importante contaminante del aire y un gas de efecto invernadero.
- La industrialización del siglo XX condujo a un aumento del O3, pero su magnitud se debate.
- Las mediciones anteriores de O3 son controvertidas, lo que crea incertidumbre en las tendencias históricas.
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