Articles | Volume 23, issue 18
https://doi.org/10.5194/bg-23-6359-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Exploring alternative SMAP Level-4 carbon model formulations for the North American Arctic–Subarctic growing season
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- Final revised paper (published on 15 Sep 2026)
- Preprint (discussion started on 16 Feb 2026)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on egusphere-2026-720', Anonymous Referee #1, 29 Mar 2026
- AC1: 'Reply on RC1', Rémi Madelon, 12 May 2026
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RC2: 'Comment on egusphere-2026-720', Anonymous Referee #2, 22 Apr 2026
- AC2: 'Reply on RC2', Rémi Madelon, 12 May 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Submit a revised manuscript (28 May 2026) by Andrew Feldman
AR by Rémi Madelon on behalf of the Authors (09 Jun 2026)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (22 Jun 2026) by Andrew Feldman
RR by Preet Lal (05 Jul 2026)
RR by Anonymous Referee #2 (12 Jul 2026)
ED: Publish subject to minor revisions (review by editor) (14 Jul 2026) by Andrew Feldman
AR by Rémi Madelon on behalf of the Authors (23 Jul 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (08 Aug 2026) by Andrew Feldman
AR by Rémi Madelon on behalf of the Authors (31 Aug 2026)
Manuscript
This paper by Madelon et al. tests whether adjusting, how SMAP L4C model responds to light, temperature, soil moisture, and vapor pressure deficit can improve GPP and ER estimates across Arctic-Subarctic tundra, taiga forests, and wetlands in North America. Twenty eddy covariance towers across western Canada and Alaska provide the reference data, covering 2015 to 2022. The study is well-timed, and the incremental formulation design is genuinely useful because it lets you see what each modification actually does, rather than attributing a combined effect to several changes at once. The finding that energy proxies, specifically the nonlinear light-response and growing degree days, consistently outperform moisture adjustments across all three ecosystem types is a clean and practically useful result. The discussion in section 6.5, where the authors frankly acknowledge the circular relationship between flux-partitioning methods and model calibration targets, is one of the stronger parts of the paper and a point that rarely gets enough attention in similar work. That said, several issues need to be addressed before the manuscript is ready for publication. The following comments are for further improvement.
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