Articles | Volume 16, issue 22
Research article
17 Nov 2016
Research article |  | 17 Nov 2016

Observational evidence for aerosols increasing upper tropospheric humidity

Laura Riuttanen, Marja Bister, Veli-Matti Kerminen, Viju O. John, Anu-Maija Sundström, Miikka Dal Maso, Jouni Räisänen, Victoria A. Sinclair, Risto Makkonen, Filippo Xausa, Gerrit de Leeuw, and Markku Kulmala


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Laura Riuttanen on behalf of the Authors (14 Oct 2016)  Author's response   Manuscript 
ED: Publish as is (19 Oct 2016) by Aijun Ding
AR by Laura Riuttanen on behalf of the Authors (28 Oct 2016)
Short summary
Here we show observational evidence that aerosols increase upper tropospheric humidity (UTH) via changes in the microphysics of deep convection. Using remote sensing data over the ocean east of China in summer, we show that increased aerosol loads are associated with an UTH increase of 2.2 ± 1.5 in units of relative humidity. We show that humidification of aerosols or other meteorological covariation is very unlikely to be the cause for this result indicating relevance for the global climate.
Final-revised paper