Differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth
Correctly detecting surface temperature responses to a climate forcing requires consideration of their spatio-temporal variability. Here, the authors demonstrate that forcing efficacy is governed by the effective heat capacity of the atmosphere, itself a function of planetary boundary layer depth.
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| Autores principales: | , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2016
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/ca0193d1df154184ae98981f8a7c2f69 |
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