the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Multi-year observations reveal a larger than expected autumn respiration signal across northeast Eurasia
- 1Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA
- 2Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA
- 3Joint Institute for Regional Earth System Science and Engineering, University of California, Los Angeles, CA, USA
- 4College of Surveying and Geo-Informatics, Tongji University, China
- 5Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, MD, USA
- 6Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USA
- 7College of Atmospheric and Geographic Sciences, University of Oklahoma, Norman, OK USA
- 8Laboratoire des Sciences du Climat et de l’Environnement/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, 91191 Gif-sur-Yvette, France
- 9Research Institute of Agriculture and Life Sciences, Seoul National University, Seoul, South Korea
- 10Earth Systems Research Center, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH, USA
- 11College of Life and Environmental Sciences, University of Exeter, Exeter EX4 4RJ, UK
- 12Laboratoire de Géologie, Ecole Normale Supérieure/CNRS UMR8538, IPSL, PSL Research University, Paris, France
- 13Department of Physics, University of Toronto, Toronto, Ontario, Canada
- 14NASA Ames Research Center, Moffett Field, CA, USA
- 15Centre for Atmospheric Sciences, Indian Institute of Technology Delhi, New Delhi, India
- 16Department of Meteorology and National Centre for Atmospheric Science, University of Reading, Reading, UK
- 1Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA
- 2Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA
- 3Joint Institute for Regional Earth System Science and Engineering, University of California, Los Angeles, CA, USA
- 4College of Surveying and Geo-Informatics, Tongji University, China
- 5Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, MD, USA
- 6Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USA
- 7College of Atmospheric and Geographic Sciences, University of Oklahoma, Norman, OK USA
- 8Laboratoire des Sciences du Climat et de l’Environnement/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, 91191 Gif-sur-Yvette, France
- 9Research Institute of Agriculture and Life Sciences, Seoul National University, Seoul, South Korea
- 10Earth Systems Research Center, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH, USA
- 11College of Life and Environmental Sciences, University of Exeter, Exeter EX4 4RJ, UK
- 12Laboratoire de Géologie, Ecole Normale Supérieure/CNRS UMR8538, IPSL, PSL Research University, Paris, France
- 13Department of Physics, University of Toronto, Toronto, Ontario, Canada
- 14NASA Ames Research Center, Moffett Field, CA, USA
- 15Centre for Atmospheric Sciences, Indian Institute of Technology Delhi, New Delhi, India
- 16Department of Meteorology and National Centre for Atmospheric Science, University of Reading, Reading, UK
Abstract. Site-level observations have shown pervasive cold season CO2 release across Arctic and boreal ecosystems, impacting annual carbon budgets. Still, the seasonality of CO2 emissions are poorly quantified across much of the high latitudes due to the sparse coverage of site-level observations. Space-based observations provide the opportunity to fill some observational gaps for studying these high latitude ecosystems, particularly across poorly sampled regions of Eurasia. Here, we show that data-driven net ecosystem exchange (NEE) from atmospheric CO2 observations implies strong summer uptake followed by strong autumn release of CO2 over the entire cold northeastern region of Eurasia during the 2015–2019 study period. Combining data-driven NEE with satellite-based estimates of gross primary production (GPP), we show that this seasonality implies less summer heterotrophic respiration (Rh) and greater autumn Rh than would be expected given an exponential relationship between respiration and surface temperature. Furthermore, we show that this seasonality of NEE and Rh over northeastern Eurasia is not captured by the TRENDY v8 ensemble of dynamic global vegetation models (DGVMs), which estimate that only 52 % of annual Rh occurs during Aug–Apr, while the data-driven estimate suggests 64–70 % of annual Rh occurs over this period. We explain this seasonal shift in Rh by respiration from soils at depth during the zero curtain period, when sub-surface soils remain unfrozen up to several months after the surface has frozen. Additional impacts of physical processes related to freeze-thaw dynamics may contribute to the seasonality of Rh. This study confirms a significant and spatially extensive early cold season CO2 efflux in the permafrost rich region of northeast Eurasia, and suggests that autumn Rh from subsurface soils in the northern high latitudes is not well captured by current DGVMs.
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Brendan Byrne et al.
Status: final response (author comments only)
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RC1: 'Comment on bg-2022-40', Ashley Ballantyne, 30 Mar 2022
Review of Byrne et al: Multi-year observations reveal a larger than expected autumn respiration signal across northeast Eurasia
Summary:
In this paper Byrne et al. evaluate the seasonal distribution of NEE at high latitudes using a combination of atmospheric CO2 measurements to inform model inversions of net C exchange in combination with satellite estimates of GPP to infer respiration. They note that anomalously low NEE in autumn can be attributed to greater Rh release. They also note a mismatch between their estimates and those derived from land surface models. They then provide an explanation whereby temperature lags within the soil can explain a certain fraction of this enhanced autumn respiration. This was a nice paper and could be publishable with some additional analysis and consideration of assumptions.
General Comments:
This paper profits from the high resolution XCO2 measurements which now allow us to estimate net CO2 fluxes at high resolution within specific bioregions and uncover different processes that may be affecting these seasonal fluxes. I found this analysis to be quite thorough and pretty convincing; however, I did have a few general comments. It seems as though the mismatch between observations and models may be dependent on the seasonal estimates of CUE and their assumptions. Perhaps it would be useful to look at total ecosystem respiration (GPP-NEE= TER) initially to see if the same mismatch is evident, this would suggest that the mismatch is not an artifact of the unique CUE applied over this region. Alternatively, one could use an independent estimate of CUE from an independent model (Konings et al. 2019) or use the same seasonal CUE for all regions. Furthermore, see recent analysis on Siberian warming where there is a strong relationship between spring GPP and fall TER (Kwon et al. 2021). Although the timespan for the OCO-2 inversions is too short, this citation on seasonal anomalies may help to put these results in a longer temporal context.
I also had some comments on the soil model comparisons with the observation constrained estimates. The text (line 323) discusses regressions and statistics of those regressions, but the actual figure shows seasonal distributions from models and observations. The figure is pretty clean and easy to interpret, but the paper could benefit from a table in the main text that include your statistics, in addition to standard model performance statistics such as RMSE, MAE, and bias statistics. The model could also be tested against the eddy flux data estimates of Rh and these values could be reported in the table. This would help the reader evaluate which models are indeed superior. Also litterfall estimates seem an order of magnitude too high in Fig. s15 should peak at ~2 TgC day-1 as compared to NPP estimates in Fig. 3. This may just be a units problem but check the model.
See the attached PDF for my specific comments.
References:
Konings, Alexandra G., A. Anthony Bloom, Junjie Liu, Nicholas C. Parazoo, David S. Schimel, and Kevin W. Bowman. 2019. “Global Satellite-Driven Estimates of Heterotrophic Respiration.” Biogeosciences 16 (11): 2269–84.
Kwon, Min Jung, Ashley Ballantyne, Philippe Ciais, Ana Bastos, Frédéric Chevallier, Zhihua Liu, Julia K. Green, Chunjing Qiu, and John S. Kimball. 2021. “Siberian 2020 Heatwave Increased Spring CO2 Uptake but Not Annual CO2 Uptake.” Environmental Research Letters: ERL [Web Site] 16 (12): 124030.
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RC2: 'Comment on bg-2022-40', Anonymous Referee #2, 06 Jun 2022
The manuscript by Byrne et al is an anlysis of seasonal cycles of carbon fluxes over northern ecosystems, with a comparison of inversion results of NEE against DGVM estimates of NEE, and then a comparison of the inversion NEE estimates minus GPP and an estimate of Ra to infer Rh, against DGVM estimates of that as well. The main findings are (a) that NEE late-season positive fluxes are higher in the observations than the models, and (b) that the inferred Rh seasonality indicates that the DGVMs underestimate that late-season Rh.Overall, I think the comparison between inversion results and models is really useful, and the paper should be published. But I find it an interesting but not entirely satisfying analysis. One problem is that the number of different steps from NEE to Rh seems like it introductes the potential for several errors to creep in, particularly as relate to Ra. Second, there are any number of reasons why the DGVMs could show a bias relative to the observations, and it is certainly possible that the lack of deep-soil respiraiton is one reason. But the attempt to provide a mechanistic explanation here using a simple model is not very clear, and subject to somewhat arbitrary choices like how to handle substrate seasonality. I wonder if a slightly different approach of looking at the DGVMs themselves, and asking whether there are structural or parametric charactistics of the models that govern the shapes of their seasonal cycles, and which might provide some clues for identifying whether any of them do a better or worse job than others?
Line 12: please provide uncertainty range for the DGVM estimates, as you do for the data-driven estimates
Line 17: "is not well captured by current DGVMs." Any DGVMs, or just the ensemble mean?
Line 70-72: Could you clarify whether you are using monthly mean CUE values or annual mean values here?
Lines 99-100. How confident are we in the soil temperature predictions of these models? There have been a few analyses of the soil temeprature dynamics and permafrost statistics of climate models at high latitudes. Does this set represent a set of best-performing sopil temperature models?
Fig. 2. I think that the per-area fluxes are more meaningful here, otherwise the reader gets the suggestion that NEE is higher during the summer in the colder than the warmer regions, which is confusing. So I suggest switching fig. S7 and fig. 2, and in general reporting things per unit area.
Figs 2 & S7: I am skeptical about the errors introduced by the GPP -> NPP conversion, I think it would be useful to include a set of GPP panels as well, since, like NEE, that is the most directly observed, with the NPP and RH much less direct.
Figs 2 and S7: A lot of the focus of the discussion is on the autumn differences, but I wonder if the more general problem is that the winter respiration in general is underestimated by the models in the cold region. This would be consistent with the findings of Natali et al., but given the larger-scale datasets used here would still be an important point to emphasize here.
Lne 264: This isn't really a shift, so much as a bias in TRENDY relative to the observations?
Lines 164-270 and fig. S12. I think FLUXNET is actually telling a different story than the larger-scale datasets. The TRENDY models actually have a higher positve NEE anomaly during the shoulder season than FLUXNET, which is the opposite pattern shown in fig. 2c. If this is correct, then I think the discussion of this result needs to be revised accordingly.
Section 3.2, I'm not sure I understand what new information the 14-day-resolved data provides beyond what is in the monthly data. Is this analysis really necessary? If so, could the authors give a bit better motivation and explanation?
Fig.3. I'm very skeptical about how narrow the range of uncertainty in panels a-c are here. What is that a measure of?
Lines 334-348, and figure 4. I don't understand this sensitivity analysis, or why the seasonal cycles in panels g-i are so different from the ones in panels d-f. Could you clarify a bit more what is being shown here? Further, the argument about deep soil playing a greater role should help with the autumn respiration peak, but less so with the bias in respiration in the cold region throughout the winter. What does this analysis have to say about that?
Line 441. I don't understand the line "TRENDY v8 data were downloaded from trendy-v8@trendy.ex.ac.uk.", since that is an email address, not a URL. Please provide a URL or DOI to a FAIR-aligned data archive where the data can be freely downloaded or, if the data is not available, then per this journal's data policy, a detailed explanation of why this is the case is required.
Brendan Byrne et al.
Brendan Byrne et al.
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