Quantifying horizontal and vertical tracer mass fluxes in an idealized valley during daytime

Leukauf, Daniel; Gohm, Alexander; Rotach, Mathias W.

doi:https://doi.org/10.5194/acp-16-13049-2016

Articles | Volume 16, issue 20

https://doi.org/10.5194/acp-16-13049-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-16-13049-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 16, issue 20

Research article

|

21 Oct 2016

Research article |

| 21 Oct 2016

Quantifying horizontal and vertical tracer mass fluxes in an idealized valley during daytime

Daniel Leukauf, Alexander Gohm, and Mathias W. Rotach

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Final revised paper (published on 21 Oct 2016)
Supplement to the final revised paper
Preprint (discussion started on 09 Jun 2016)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review of Leukauf et al', Anonymous Referee #2, 16 Jun 2016
RC2: 'review', Anonymous Referee #1, 07 Jul 2016
AC1: 'Response to the Reviewers', Daniel Leukauf, 26 Aug 2016
AC2: 'Revised Paper', Daniel Leukauf, 26 Aug 2016
AC3: 'Revised Paper, changes in red', Daniel Leukauf, 26 Aug 2016

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Daniel Leukauf on behalf of the Authors (26 Aug 2016) Manuscript

ED: Publish subject to technical corrections (21 Sep 2016) by Bernhard Vogel

AR by Daniel Leukauf on behalf of the Authors (27 Sep 2016) Author's response Manuscript

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Short summary

Since populated valleys suffer often from poor air quality, it is of interest to better understand the various mechanisms relevant to remove pollutants from the valley atmosphere. One mechanism is the transport by along-slope flows, which are generated during fair-weather days. In this study we quantify the amount of tracer that is removed from a valley atmosphere and the amount that is re-circulated within the valleys. For this study we are using the numerical weather model WRF.