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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Detalles Bibliográficos
Autores principales:	Richard Davy, Igor Esau
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2016
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/ca0193d1df154184ae98981f8a7c2f69
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spelling	oai:doaj.org-article:ca0193d1df154184ae98981f8a7c2f692021-12-02T17:31:20ZDifferences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth10.1038/ncomms116902041-1723https://doaj.org/article/ca0193d1df154184ae98981f8a7c2f692016-05-01T00:00:00Zhttps://doi.org/10.1038/ncomms11690https://doaj.org/toc/2041-1723Correctly 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.Richard DavyIgor EsauNature PortfolioarticleScienceQENNature Communications, Vol 7, Iss 1, Pp 1-8 (2016)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Richard Davy Igor Esau Differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth
description	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.
format	article
author	Richard Davy Igor Esau
author_facet	Richard Davy Igor Esau
author_sort	Richard Davy
title	Differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth
title_short	Differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth
title_full	Differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth
title_fullStr	Differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth
title_full_unstemmed	Differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth
title_sort	differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth
publisher	Nature Portfolio
publishDate	2016
url	https://doaj.org/article/ca0193d1df154184ae98981f8a7c2f69
work_keys_str_mv	AT richarddavy differencesintheefficacyofclimateforcingsexplainedbyvariationsinatmosphericboundarylayerdepth AT igoresau differencesintheefficacyofclimateforcingsexplainedbyvariationsinatmosphericboundarylayerdepth
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Differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth

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