Preprints
https://doi.org/10.5194/egusphere-2025-4522
https://doi.org/10.5194/egusphere-2025-4522
20 Oct 2025
 | 20 Oct 2025

Uncertainties in long-term ensemble estimates of contextual evapotranspiration over Southern France

Samuel Mwangi, Albert Olioso, Jordi Etchanchu, Kanishka Mallick, Aolin Jia, Jérôme Demarty, Nesrine Farhani, Emmanuelle Sarrazin, Philippe Gamet, Jean-Louis Roujean, and Gilles Boulet

Abstract. Estimating evapotranspiration (ET) beyond the local or point scale is critical for water resources and ecosystem studies. Remote sensing offers a unique advantage by enabling ET monitoring at larger spatial scales than in-situ instruments. By leveraging relationships between surface biophysical parameters and terrestrial thermal emission, continuous ET can be retrieved across diverse landscapes. Herein, we apply the EVapotranspiration Assessment from SPAce (EVASPA) contextual tool over southern France, using MODIS-derived land surface temperature / emissivity (LST/E), NDVI and albedo products. The dataset spans 2004–2024, yielding 972 instantaneous ET estimates. The EVASPA ensemble integrates multiple member outputs generated from: 1) alternative formulations of the evaporative fraction (EF) and ground heat flux (G), and 2) different LST and radiation inputs. Evaluation against flux tower data shows that even a simple ensemble average provides reasonable agreement, though individual member performance varies substantially. Uncertainty analyses were also performed where we looked at how each of the distinct variables (i.e., LST, radiation, evaporative fraction (EF), and ground heat flux (G) methods) influenced the modelled ET. The analyses reveal that LST inputs and EF formulations are the dominant sources of variability, with seasonal dependence–uncertainties peak during summer (tending to follow the annual cycle of radiation) and are partly influenced by satellite characteristics. Generally the satellite's overpass time introduces more incertitude to the gap filled daily ET estimates compared to the LST/LSE separation methods; as such, the uncertainties in LST could, by extension, be partially attributed to uncertainties in the radiations during the acquisition time. Radiation inputs also contribute to the variations in the ensemble, while G flux methods exert comparatively minor influence, especially for estimates derived from TERRA morning overpasses. Overall, our results demonstrate that ensemble-based contextual modelling can provide both reliable flux estimates and a meaningful uncertainty spread. By allowing optimal member selection according to surface and climatic conditions, ensemble modelling using EVASPA enhances ET retrieval robustness thus providing more resilient and informative estimates. Such ensemble frameworks are especially valuable for forthcoming missions like TRISHNA, where consistent and accurate, high-resolution ET monitoring will be crucial for operational water and ecosystem management.

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Journal article(s) based on this preprint

26 Feb 2026
Uncertainties in long-term ensemble estimates of contextual evapotranspiration over southern France
Samuel Mwangi, Albert Olioso, Jordi Etchanchu, Kanishka Mallick, Aolin Jia, Jérôme Demarty, Nesrine Farhani, Emmanuelle Sarrazin, Philippe Gamet, Jean-Louis Roujean, and Gilles Boulet
Hydrol. Earth Syst. Sci., 30, 1117–1142, https://doi.org/10.5194/hess-30-1117-2026,https://doi.org/10.5194/hess-30-1117-2026, 2026
Short summary
Samuel Mwangi, Albert Olioso, Jordi Etchanchu, Kanishka Mallick, Aolin Jia, Jérôme Demarty, Nesrine Farhani, Emmanuelle Sarrazin, Philippe Gamet, Jean-Louis Roujean, and Gilles Boulet

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-4522', Anonymous Referee #1, 24 Nov 2025
    • AC1: 'Reply on RC1', Samuel Mwangi, 05 Feb 2026
  • RC2: 'Comment on egusphere-2025-4522', Anonymous Referee #2, 15 Jan 2026
    • AC2: 'Reply on RC2', Samuel Mwangi, 05 Feb 2026

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-4522', Anonymous Referee #1, 24 Nov 2025
    • AC1: 'Reply on RC1', Samuel Mwangi, 05 Feb 2026
  • RC2: 'Comment on egusphere-2025-4522', Anonymous Referee #2, 15 Jan 2026
    • AC2: 'Reply on RC2', Samuel Mwangi, 05 Feb 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Publish subject to technical corrections (09 Feb 2026) by Serena Ceola
AR by Samuel Mwangi on behalf of the Authors (11 Feb 2026)  Author's response   Manuscript 

Post-review adjustments

AA – Author's adjustment | EA – Editor approval
AA by Samuel Mwangi on behalf of the Authors (19 Feb 2026)   Author's adjustment   Manuscript
EA: Adjustments approved (23 Feb 2026) by Serena Ceola

Journal article(s) based on this preprint

26 Feb 2026
Uncertainties in long-term ensemble estimates of contextual evapotranspiration over southern France
Samuel Mwangi, Albert Olioso, Jordi Etchanchu, Kanishka Mallick, Aolin Jia, Jérôme Demarty, Nesrine Farhani, Emmanuelle Sarrazin, Philippe Gamet, Jean-Louis Roujean, and Gilles Boulet
Hydrol. Earth Syst. Sci., 30, 1117–1142, https://doi.org/10.5194/hess-30-1117-2026,https://doi.org/10.5194/hess-30-1117-2026, 2026
Short summary
Samuel Mwangi, Albert Olioso, Jordi Etchanchu, Kanishka Mallick, Aolin Jia, Jérôme Demarty, Nesrine Farhani, Emmanuelle Sarrazin, Philippe Gamet, Jean-Louis Roujean, and Gilles Boulet
Samuel Mwangi, Albert Olioso, Jordi Etchanchu, Kanishka Mallick, Aolin Jia, Jérôme Demarty, Nesrine Farhani, Emmanuelle Sarrazin, Philippe Gamet, Jean-Louis Roujean, and Gilles Boulet

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Short summary
The EVapotranspiration Assessment from SPAce (EVASPA) algorithm that will generate TRISHNA evapotranspiration (TRISHNA ET) products shows good agreement with observations. Analyses conducted on 4 variables used in contextual ET modelling showed that land surface temperature and evaporative fraction methods introduce the largest uncertainty in ensemble estimates, followed by radiation. Soil heat flux methods contribute the least. Robust ET products will require optimizing the sensitive variables.
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