the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Water level variation at a beaver pond significantly impacts net CO2 uptake of a continental bog
- 1Department of Geography, McGill University, Montreal, Quebec H3A OB9, Canada
- 2Geography and Environmental Studies, Carleton University, Ottawa, ON, Canada
- 3School of Environment, Trent University, Peterborough, ON, Canada
- 1Department of Geography, McGill University, Montreal, Quebec H3A OB9, Canada
- 2Geography and Environmental Studies, Carleton University, Ottawa, ON, Canada
- 3School of Environment, Trent University, Peterborough, ON, Canada
Abstract. The carbon (C) dynamics of northern peatlands are sensitive to hydrological changes owing to ecohydrological feedback. We quantified and evaluated the impact of water level variations in a beaver pond (BP) on the CO2 flux dynamics of an adjacent, raised Sphagnum – shrub-dominated bog in southern Canada. We applied the CoupModel to the Mer Bleue bog, where the hydrological, energy and CO2 fluxes have been measured continuously for over 20 years. The lateral flow from the bog to the BP was estimated by the hydraulic gradient between the peatland and the BP's water level and the vertical profile of peat hydraulic conductivity. The model outputs were compared with the measured hydrological components, CO2 flux and energy flux data (1998–2019). CoupModel was able to reproduce the measured data well. The simulation shows that variation in the BP water level (naturally occurring or due to management) influenced the bog net ecosystem exchange of CO2 (NEE). Over 1998–2004, the BP water level was 0.75 to 1.0 m lower than during 2017–2019. Simulated net CO2 uptake was 55 g C m−2 yr−1 lower during 1998–2004 compared to 2017–2019 when there was no BP disturbance, which was similar to the differences in measured NEE between those periods. Peatland annual NEE was well correlated with water table depth within the bog, and NEE also shows a linear relation with the water level at the BP, with a slope of −120 g CO2-C m−2 yr−1 m−1. The current modelling predicts the bog may switch from CO2 sink to source when the BP water levels drop lower than ~ 1.7 m below the peat surface at the eddy covariance tower, 250 m from the BP. This study highlights the importance of natural and human disturbances to adjacent water bodies in regulating net CO2 uptake function of northern peatlands.
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Hongxing He et al.
Status: open (extended)
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RC1: 'Comment on hess-2021-585', Joshua Ratcliffe, 28 Mar 2022
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In this manuscript the authors investigate how the management of a beaver dam has affected the lateral flow of water, and the vertical CO2 fluxes, from a well known and long-running GHG monitoring site at Mer Bleue peatland. They use a modelling approach to provide several ‘what-if’ scenarios to model what the CO2 flux may have been without any alteration of the beaver pond level.
This is a very innovative paper which addresses an important and overlooked aspect of the peatland GHG flux, i.e. what is going on at the margins. It will additionally be good to see this published as it concerns Mer Bleue,the longest running EC record on a boreal peatlands and a site from which much of our understanding of boreal peatland ecology and gas flux is derived.
I really like the approach the authors have used to tease out the effect of the beaver pond from the background variability. I think it is clear from the measured data in Figure 2 and Figure 3 and Figure 6 that there was a major change in the ecosystem corresponding with the rise in the water level of the beaver pond, the coup model nicely confirms this as a mechanism.
Importantly, this confirms the wide-ranging ecological effects water table management can have hundreds of meters from the flux measurement site. This has important implications for other sites and boreal ecosystems, including other long-running flux measurement sites. I know some researchers who work on relatively degraded peatlands, with low horizontal hydraulic conductivity, who are sceptical that water level management hundreds of meters away can have any affect at all and I think it would be good to discuss how Mer Bleue might contrast to other peatlands. See my comment to this further below.
The coup model itself preforms adequately, and the authors discuss the limitations of the model in appropriate detail.
While I generally think this is a very good paper, I thought it was lacking some detail which would ensure it’s comparability to other sites and situations. While hydrological feedbacks are mentioned, it’s not really clear just how strong these feedbacks can be. In the discussion I would like to see a short paragraph about the horizontal hydrologic conductivity and how Mer Bleaur compares to other peatlands and how we might expect this to change if the water table was to undergo sustained lowering for a period of decades or more.
One thing that bothers me rather a lot is that the increase in ER with the beaver pond level listed in Figure 7 seems to contradict what was established in Lafleur et al., 2005 (Ecosystem Respiration in a Cool Temperate Bog Depends on Peat Temperature But Not Water Table) where water table fluctuations were found to have little or no effect on ER, this is maybe due to Lafleur et al., 2005 only having the early data available, before the beaver dam raising, but I would like to see this addressed. At the moment this paper is not cited.
Additionally, I have a comment about the measured data. I do not believe (nor would it be correct) that the methodology used to process the fluxes is the same as in Roulet et al., 2007. There have been several large changes in best practice for flux processing in the last 15 years that I am sure the authors are aware of. I would like to see the detailed method for flux processing included in the SI
Could the authors state why the flux simulations in 2013 and 2017 performed so poorly compared to other years?
I wish the authors the best of luck with the revisions.
Figure 2:
Should be clear what is generated data and what is measured. Suggest the generated data is presented in a different colour/style
The measured water level at the peatlands also looks rather spiky and a bit suspect (2006 and 2007). Please check for and remove outliers if present. It would be good to state the temporal resolution in the caption.
Other than this I have some minor comments the authors may wish to consider.
L9: should be “feedbacks”
L12: consider “lateral flow of water”
L29:30 This range listed is too low, see the following. Suggest an upper range of ~200 g m-2 yr
https://doi.org/10.1111/gcb.13424
https://doi.org/10.1111/j.1365-2486.2010.02378.x.
L54-L55: There are a few analogous studies looking at road construction and how that have raised and lowered water table levels for instance: https://doi.org/10.1007/s10021-016-0092-x
L83: Should mention that it is a downward slope (being a bog I would assume so…)
L101 Please state the total number of periodic measurements (n=?)
L103: This is probably fine, given the change in mean across treatments. Please differentiate this data somehow in the plots (particularly in Figure 2)
L207: Really nice to see these numbers!
213: suggest “the disturbance level”
226: Water table is relatively meaningless over winter, not really a problem.
240: Again, it would be worth discussing (briefly) how the shrub dominance of GPP at Mer Bleue might cause it to respond differently to other peatlands, see discussion in https://doi.org/10.1016/j.scitotenv.2018.11.151
L339: Other sites see very large changes, see https://doi.org/10.1111/jvs.12602
L341: suggest also the following as a site where there has been major changes in GPP and plant cover following WT lowering https://doi.org/10.1016/j.scitotenv.2019.134613
L384-385: These models are almost totally useless without incorporating feedbacks.
L387: This is a reasonable statement, I agree.
L390: I’d say this is not as well established as it might be believed there are odd sites such as pocosin and restiad peatlands where C accumulation can be high even under a very low water table again see: https://doi.org/10.1016/j.scitotenv.2018.11.151
Hongxing He et al.
Hongxing He et al.
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