Articles | Volume 18, issue 3
https://doi.org/10.5194/essd-18-2023-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
The Loobos ecosystem first tower dataset: meteorology, turbulent fluxes and net ecosystem exchange (1996 to 2021)
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- Final revised paper (published on 17 Mar 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 01 Sep 2025)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on essd-2025-372', Anonymous Referee #1, 09 Oct 2025
- AC3: 'Response to Anonymous Reviewer #1', Michiel van der Molen, 20 Jan 2026
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RC2: 'Comment on essd-2025-372', Anonymous Referee #2, 16 Dec 2025
- AC2: 'Response to Anonymous reviewer #2', Michiel van der Molen, 20 Jan 2026
- AC1: 'Comment on essd-2025-372 Anonymous Referee #1', Michiel van der Molen, 20 Jan 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Michiel van der Molen on behalf of the Authors (21 Jan 2026)
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EF by Mario Ebel (23 Jan 2026)
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Author's tracked changes
ED: Referee Nomination & Report Request started (13 Feb 2026) by Hanqin Tian
ED: Publish subject to minor revisions (review by editor) (13 Feb 2026) by Hanqin Tian
AR by Michiel van der Molen on behalf of the Authors (18 Feb 2026)
Author's response
Author's tracked changes
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ED: Publish as is (20 Feb 2026) by Hanqin Tian
AR by Michiel van der Molen on behalf of the Authors (02 Mar 2026)
Author's response
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General comments.
The manuscript “The Loobos ecosystem first tower dataset: meteorology, turbulent fluxes and net ecosystem exchange (1996 to 2021)” by Zhao et al. describes an impressive bulk of data collected over 25 years at one of the earliest micrometeorological towers installed in Europe for the systematic monitoring of CO2 and energy fluxes. The dataset includes, beyond flux variables, numerous parallel measurements of biophysical parameters and biological processes of the forest ecosystem such as LAI, foliage chemistry, biomass carbon stocks, sap flow density and water table depth.
A dedicated section explains in detail the flux data processing pipeline and the quality check procedures for flux and partly for meteorological variables. Finally, a synthesis of the dataset is illustrated by plots showing the consistency of the flux data, the mean diurnal variation and in particular the mean monthly NEE fluxes from which the trend towards a stronger carbon sequestration can be observed.
The presented dataset is undoubtedly of interest to the readers of ESSD and the well-structured manuscript delivers an overall clear and detailed description of it. Said that, I recommend the publication of the manuscript but only after a minor revision mainly to : (i)fix some issues concerning the terminology used to describe the ecosystem-atmosphere CO2 exchanges,; (ii) provide more information about the quality of meteorological measurements and the instruments maintenance routines.
Specific comments.
Introduction section (ca. L60): I suggest including a map of the area showing the location of the measurements (eddy covariance, meteorological, forest transects, sap flow, etc.).
Introduction – par 2.1.1: Some instruments were operated continuously for long periods of time (eg. pyranometers, quantum sensors, etc.). Report about the maintenance routine and its frequency to ensure accurate measurements, mentioning if the sensors were periodically calibrated and if the calibration drift was accounted for in processing the data.
L223: I guess that the “depth of 15 cm” refers to insertion of the collar into the soil and not to the depth of the chamber which would be placed on top of the collar. Please confirm.
L444: the negative storage at sunrise should not be associated only to a “release of carbon dioxide” to the atmosphere, but also to the photosynthetic uptake of CO2 by the vegetation below the eddy covariance sensors height.
L460: fig. 8 shows mean monthly NEE, that is, by definition, the net flux resulting from the difference between the processes of photosynthesis and respiration. Therefore, in the case of this evergreen needle forest, I would not talk about a decrease of “winter respiration” but rather of the intensity of the CO2 source.
Appendix (L570-571): Replace “left photo” and “ right photo” with “photo on the right” and “photo on the left” respectively.