The new BELUGA setup for collocated turbulence and radiation measurements using a tethered balloon: first applications in the cloudy Arctic boundary layer

Egerer, Ulrike; Gottschalk, Matthias; Siebert, Holger; Ehrlich, André; Wendisch, Manfred

doi:https://doi.org/10.5194/amt-12-4019-2019

Articles | Volume 12, issue 7

Atmos. Meas. Tech., 12, 4019–4038, 2019

https://doi.org/10.5194/amt-12-4019-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Arctic mixed-phase clouds as studied during the ACLOUD/PASCAL...

Atmos. Meas. Tech., 12, 4019–4038, 2019

https://doi.org/10.5194/amt-12-4019-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 12, issue 7

Research article 22 Jul 2019

Research article | 22 Jul 2019

The new BELUGA setup for collocated turbulence and radiation measurements using a tethered balloon: first applications in the cloudy Arctic boundary layer

Ulrike Egerer et al.

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Final revised paper (published on 22 Jul 2019)
Preprint (discussion started on 08 Mar 2019)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'See attachment', Ian Brooks, 09 Apr 2019
- AC1: 'Author's response to Ian Brook's review', Ulrike Egerer, 21 Jun 2019
RC2: 'Review of Egerer et al. (2019)', Anonymous Referee #2, 31 May 2019
- AC2: 'Author's response to anonymous referee #2', Ulrike Egerer, 21 Jun 2019

Peer-review completion

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

AR by Ulrike Egerer on behalf of the Authors (21 Jun 2019) Author's response Manuscript

ED: Publish as is (26 Jun 2019) by Amy Solomon

Short summary

In this study, we introduce the new tethered balloon system BELUGA, which includes different modular instrument packages for measuring turbulence and radiation in the atmospheric boundary layer. BELUGA was deployed in an Arctic field campaign in 2017, providing details of boundary layer processes in combination with low-level clouds. Those processes are still not fully understood and in situ measurements in the Arctic improve our understanding of the Arctic response in terms of global warming.