Turbulence vertical structure of the boundary layer during the afternoon transition

Darbieu, C.; Lohou, F.; Lothon, M.; Vilà-Guerau de Arellano, J.; Couvreux, F.; Durand, P.; Pino, D.; Patton, E. G.; Nilsson, E.; Blay-Carreras, E.; Gioli, B.

doi:https://doi.org/10.5194/acp-15-10071-2015

Articles | Volume 15, issue 17

https://doi.org/10.5194/acp-15-10071-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue:

The Boundary-Layer Late Afternoon and Sunset Turbulence (BLLAST)...

https://doi.org/10.5194/acp-15-10071-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 15, issue 17

Research article

|

09 Sep 2015

Research article |

| 09 Sep 2015

Turbulence vertical structure of the boundary layer during the afternoon transition

C. Darbieu, F. Lohou, M. Lothon, J. Vilà-Guerau de Arellano, F. Couvreux, P. Durand, D. Pino, E. G. Patton, E. Nilsson, E. Blay-Carreras, and B. Gioli

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Final revised paper (published on 09 Sep 2015)
Preprint (discussion started on 22 Dec 2014)

Interactive discussion

Status: closed

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

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- Supplement

RC C11258: 'atmospheric simulations', Anonymous Referee #1, 16 Jan 2015
- AC C13232: 'Response to reviewer 1', C. Darbieu, 28 May 2015
RC C11264: 'LES of afternoon transition', Anonymous Referee #2, 16 Jan 2015
- AC C13233: 'Response to reviewer 2', C. Darbieu, 28 May 2015

Peer-review completion

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

AR by C. Darbieu on behalf of the Authors (05 Jun 2015) Author's response Manuscript

ED: Reconsider after minor revisions (Editor review) (06 Jul 2015) by Eric Pardyjak

AR by C. Darbieu on behalf of the Authors (24 Jul 2015) Author's response Manuscript

ED: Publish as is (24 Jul 2015) by Eric Pardyjak

Short summary

A case study of the BLLAST experiment is considered to explore the decay of turbulence that occurs in the convective boundary layer over land during the afternoon. Based on observations and on a large-eddy simulation, the analysis reveals two phases in the afternoon: a first quasi-stationary phase when the turbulent kinetic energy slowly decays without significant change in the turbulence structure and a second phase of more rapid decay with a change in spectral turbulence characteristics.