the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Methane emission quantification using UAV-based mass balance: Validation through controlled release experiments
Abstract. Uncrewed aerial vehicles (UAVs) offer flexible and cost-effective access to monitoring methane sources that can be otherwise difficult to sample, but confidence in UAV-derived fluxes requires robust validation and uncertainty characterisation. Here, we evaluate a variant UAV-based mass-balance method using single-blind controlled-release experiments at two UK sites: An aerodrome in Bedford and the Centre for Dairy Research (CEDAR), Reading. Controlled methane releases ranged from 0.021 to 2.16 kg h-1 in Bedford and 8.3 to 40.6 kg h-1 in CEDAR, including point and extended source configurations. Methane concentrations were measured in situ using an ABB GLA133-GPC analyser mounted on a hexacopter UAV equipped with a 2D sonic anemometer, and fluxes were derived from downwind horizontal transects.
Two validation approaches are considered: (i) using all individual flights to capture operational variability, and (ii) grouping flights by release rate to assess underlying method performance. Overall, fluxes calculated using the method show good correlation but substantial scatter at the individual flight level (CEDAR: slope = 1.01, r = 0.84, RMSE = 38.8 %; Bedford: slope = 0.71, r = 0.85, RMSE = 46.2 %) and substantially improved agreement when averaged by release rate (CEDAR: slope = 1.01, r = 0.94, RMSE = 19.9 %; Bedford: slope = 0.68, r = 0.99, RMSE = 38.4 %). This demonstrates that averaging reduces random variability while preserving systematic bias.
A method variant, which accounts for incomplete near-surface sampling by extrapolating the lowest available measurements and incorporating the associated uncertainty, substantially improves consistency, increasing the fraction of cases (46 % to 72 %) in which the known release rate falls within the one-standard-deviation uncertainty of the calculated release rate. We find that mean wind speed is the dominant environmental factor influencing the quality of agreement, with higher wind speeds associated with reduced bias (above 2.2 m s-1, bias ≤ 50 %), likely due to reduced turbulence under such conditions. Wind direction variability alone shows little direct influence on flux precision; instead, a wide lateral extent of the measurement plane is noted to be critical for minimising plume sampling loss under changing wind conditions. Lower emission rates exhibit greater relative bias due to increased sensitivity to smaller signal-to-noise (due to both wind variability and lower plume concentration enhancements relative to natural background variability).
The improved performance after averaging is consistent with previous studies indicating that multiple flights per release rate (e.g. n ≥ 3) enhance representativeness by reducing the influence of environmental variability. These results demonstrate that UAV-based mass-balance methods can provide methane flux estimates accurate to within 20 %, for fluxes greater than 10 kg h-1, under controlled conditions, but may suffer from systematic (but accountable) under-bias due to incomplete sampling. We also offer insights on methodological and environmental requirements to deliver robust measurements.
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Status: final response (author comments only)
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RC1: 'Comment on egusphere-2026-1665', Anonymous Referee #1, 27 May 2026
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2026/egusphere-2026-1665/egusphere-2026-1665-RC1-supplement.pdfCitation: https://doi.org/
10.5194/egusphere-2026-1665-RC1 -
AC1: 'Reply on RC1', Maria Tsivlidou, 16 Sep 2026
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2026/egusphere-2026-1665/egusphere-2026-1665-AC1-supplement.pdf
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AC1: 'Reply on RC1', Maria Tsivlidou, 16 Sep 2026
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RC2: 'Comment on egusphere-2026-1665', Thomas Lauvaux, 11 Aug 2026
Review of the paper entitled « Methane emission quantification using UAV-based mass balance: Validation through controlled release experiments” by M. Tsivlidou et al.
General comment:
The study presents an evaluation of a UAV-based mass balance approach tested over two locations where controlled releases of methane have been performed. The emission rates vary from low (0.02 kg/hr) to large (40.6 kg/hr) amounts, released from single tubes to vertical pipes to ring pipes to long horizontal lines. The sensitivity experiments examine the influence of environmental conditions and flight designs on the final emissions uncertainties. Compared to previous studies, this work brings new insights on the requirements to achieve higher accuracy and precision when using UAV to assess emissions from various types of sources. Overall, the study is fairly complete, with clear explanations regarding the campaign setup and the data analyses, and well-written. The controlled releases have been correctly designed to explore many parameters in real-world applications. Despite a lack of turbulence characterization, which would have been highly valuable to better understand the measured uncertainties, the study remains a significant contribution to this research field. Hence, we recommend this study for publication in ACP once the following points are addressed.
Main points:
Causes of the observed biases: While the study has explored some of the potential causes for the observed biases, it remains unclear which ones are responsible for the under-estimation. The absence of turbulence measurements during the flights limits the interpretation of the diagnosed errors in emissions. It is understandable that the additional cost of a 3D sonic is far from negligible, but considering your conclusions (wind direction variability, distance to the source), it seems obvious that a turbulence analysis would have helped you diagnose the relation between advection and turbulence, and their potential impact on the retrieved emissions.
While the authors have noted the relation to the wind direction variability, one can wonder if the variability arises from the turbulence at high frequency or to slower motions of the plume due to large-scale eddies. This parameter is critical to determine the most favorable environmental conditions for future campaigns, as the motion of the plumes within the perpendicular plane is proportional to the mean wind speed and to the turbulent structures. An additional 3D sonic anemometer would have provided additional insights on the size and impact of eddies, especially when flying near the source. We recommend that you discuss that point, and to the extent possible, you could use the 2D sonic data to examine the frequencies of wind direction changes over the sampling periods.
Averaging to reduce the bias: Based on Figure 2, and as observed by most UAV studies, the motion of the plume due to passing eddies results in random intercepts of the CH4 plume by the drone, at various locations across the flight plane. Clearly, the displacement of the observed peaks is a testimony of the plume fluctuations driven by turbulent structures. Hence, as one collects data over multiple flights, it may reduce the bias (CEDAR) or not (Bedford). The distance to the source becomes critical as one observes more fluctuations near the release location, thanks to diffusion. Assuming that the method is unbiased, averaging is then recommended to reduce the measured errors. Therefore, it would be more valuable to discuss how long (or how many flights/transects) are needed to reach the minimum level of uncertainties (bias).
Low-level transect: The authors have highlighted the importance of the lowest transects when calculating the overall mass flux. However, the method of interpolation (and more specifically extrapolation near the ground) used here was never discussed nor tested. While these methods are widely used to interpolate 2D fields, the mass conservation is not guaranteed and can pose significant challenges in such applications. A brief examination of the interpolation method would be beneficial to better understand if the interpolation/extrapolation technique is not causing additional positive biases, compensating for the lack of data (plume intercepts).
Technical comments:
Line 325: How did you determine the atmospheric conditions?
Line 331-336: the ratio between turbulence and advection is likely to define the variability, which can explain why one of the two alone is insufficient to explain the discrepancies.
Figure 2: Looking at the highest transect, it seems quite obvious that you have missed the vertical extent of the plume motions. While you discuss the impact of missing low-altitude transects, you never discussed the potential lack of high-altitude transects.
Figure 5: the separation by emission rates could also be seen as a split between the two sites, or by distance. You should indicate these important facts to clearly separate if the errors scale by source level or due to other parameters.
Figure 7: Some of these regressions are far from convincing, with some of the lines being decided by few points (e.g. distance). The overall fits are statistically limited by the lack of points. Add some statistical metrics to evaluate the goodness to the fit, and add a discussion about the level of confidence for each variable.
Citation: https://doi.org/10.5194/egusphere-2026-1665-RC2 -
AC2: 'Reply on RC2', Maria Tsivlidou, 16 Sep 2026
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2026/egusphere-2026-1665/egusphere-2026-1665-AC2-supplement.pdf
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AC2: 'Reply on RC2', Maria Tsivlidou, 16 Sep 2026
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