Articles | Volume 14, issue 2
Earth Syst. Sci. Data, 14, 885–906, 2022
https://doi.org/10.5194/essd-14-885-2022
Earth Syst. Sci. Data, 14, 885–906, 2022
https://doi.org/10.5194/essd-14-885-2022

Data description paper 24 Feb 2022

Data description paper | 24 Feb 2022

The Large eddy Observatory, Voitsumra Experiment 2019 (LOVE19) with high-resolution, spatially distributed observations of air temperature, wind speed, and wind direction from fiber-optic distributed sensing, towers, and ground-based remote sensing

Karl Lapo et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on essd-2020-392', Anonymous Referee #1, 12 Apr 2021
  • RC2: 'Comment on essd-2020-392', Anonymous Referee #2, 03 May 2021
  • AC1: 'Comment on essd-2020-392', Karl Lapo, 28 May 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Karl Lapo on behalf of the Authors (24 Jun 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (24 Jun 2021) by Lukas Gudmundsson
RR by Anonymous Referee #3 (12 Aug 2021)
ED: Publish subject to minor revisions (review by editor) (16 Aug 2021) by Lukas Gudmundsson
AR by Christoph Thomas on behalf of the Authors (18 Sep 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (07 Oct 2021) by Lukas Gudmundsson
AR by Christoph Thomas on behalf of the Authors (18 Jan 2022)  Author's response    Manuscript
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Short summary
The layer of air near the surface is poorly understood during conditions with weak winds. Further, it is even difficult to observe. In this experiment we used distributed temperature sensing to observe air temperature and wind speed at thousands of points simultaneously every couple of seconds. This incredibly rich data set can be used to examine and understand what drives the mixing between the atmosphere and surface during these weak-wind periods.