the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 07 Dec 2023
Observation-inferred resilience loss of the Amazon rain forest possibly due to internal climate variability
Abstract. Recent observation-based studies suggest that the Amazon rain forest has lost substantial resilience since 1990, indicating that the forest might undergo a critical transition in the near future due to global warming and deforestation. The idea is to use trends in lag-1 auto-correlation of leaf density as an early warning signal of an imminent critical threshold for rain forest dieback. Here we test whether the observed change in auto-correlations could arise from internal variability by using historical and control simulations of nine sixth-generation Earth system model ensembles (Phase 6 of the Coupled Model Intercomparison Project, CMIP6). We quantify trends in leaf area index auto-correlation from both models and satellite observed vegetation optical depth from 1990 to 2017. Four models reproduce the observed trend with at least one historical realization, whereby the observations lie at the upper limit of model variability. Three out of these four models exhibit similar behavior in control runs, suggesting that historical forcing is not necessary for simulating the observed trends. Furthermore, we do not observe a critical transition in any future runs under the strongest greenhouse gas emission scenario (SSP5-8.5) until 2100 in the four models that best reproduce the past observed trends. Hence, the currently observed trends could be caused simply by internal variability, and, unless the data records are extended, have limited applicability as an early warning signal. Our results suggest that the current rapid decline in Amazon rain forest coverage is mainly caused by local actors.
-
Notice on discussion status
The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
-
Preprint
(3904 KB)
-
The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
- Preprint
(3904 KB) - Metadata XML
- BibTeX
- EndNote
- Final revised paper
Journal article(s) based on this preprint
Interactive discussion
Status: closed
-
RC1: 'Comment on egusphere-2023-2734', Anonymous Referee #1, 22 Jan 2024
Please find my comments in the attached pdf.
- AC1: 'Reply on RC1', Raphael Grodofzig, 24 Apr 2024
-
RC2: 'Comment on egusphere-2023-2734', Anonymous Referee #2, 28 Feb 2024
The manuscript is well written, concise and offers a thorough explanation of the objectives, methods and a good overview of the results. The work follows some of the steps taken by Boulton et al (2022), using lag-1 year auto-correlation (AR(1)) of changes in forest vegetation optical depth (VOD) and Leaf Area Index (LAI) as an early warning signal before reaching critical threshold for forest dieback.
In the results, the authors remark that it is impossible, based solely a single data record, to figure out whether observed changes and trends in auto-correlation of VOD are caused by external forcing or internal variability. To address this problem, they mention that common approaches to detect external (forced) changes are the use of multiple climate model runs, based on different codes, or to use models that start from different initial conditions. They then show, as an example, 30 simulations of the historical experiment, comparing it to one CMIP6 model (MPI-ESM1-2-LR). They show that the observed spatially averaged trend of AR(1) falls within the range of trends of the ensemble members for the same period. They also mention the possibility of investigating simulations of equal length as the historical data, but modeled for a pre-industrial context. After mentioning both examples, they state that the forced response of the Amazon rain forest is not needed to generate an AR(1) increase of similar magnitude as the observed one. And just then they mention that not all models are equally fit for the purpose of simulating the dynamics of the forest in accordance with observations. They then apply the KS test to verify if each ensemble member could have been drawn from the same underlying distribution as the observations, and only four of the nine models pass the test. The model used in both examples mentioned above is one that passes the KS test (MPI-ESM1-2-LR), as it should be. But presenting the above-mentioned examples first, with an important argument for the conclusion, and then showing the “screening” made by using the KS test, may cause some confusion. Thus, I suggest the KS test result is presented before the examples are shown, for increased clarity of the text.
Also, after the second example, the authors state (line 125) “The shorter-term deviations appear slightly muted in this case compared to the historical ensemble, and even if encapsulating the longer term trend the shorter variations are clearly less than those observed, therefore possibly suggesting an influence from historical forcing. Overall, however, the displayed model ensemble suggests that the forced response of the Amazon rain forest is not needed to generate an increase in AR(1) of similar magnitude to that observed”. In other words, two arguments that support an influence from historical forcing are shown, and then a generic argument is given to argue that forced response is not important. Since the main conclusion of the manuscript is that external forcing do not generate a significant change in AR(1), I think a more detailed discussion to support this at this point would be interesting.
In the conclusions, the authors state: “Of the four well performing model ensembles, three of them showed trends similar to observations also in their unforced control simulations. These results suggest that the observed trend could simply be an expression of internal variability, and that longer data records would be needed to show that the opposite is the case.” Is it possible to give an aducated guess on how much longer should the data records be?
Boulton et al (2022) argue that the Amazon is showing signs of resilience loss during a period with three “one-in-a-century” droughts, and the higher frequency of extreme droughts leads to ecological changes, but the replacement of drought sensitive tree species by drought resistant ones happens in a slower pace, which may reduce forest resilience even further. If data was available, could the inclusion of the latest extreme drought (2023) to adjust the models significantly change the outcome of the analysis of this manuscript?
The authors also conclude that “This result is further corroborated by the spatial distribution of the increasing trend in AR(1) in the model simulations. Here it is found that ensemble members with substantial positive or negative trends show these in relatively large regions, but not necessarily in those regions with large anthropogenic deforestation. This suggests that such anomalies are associated with large scale weather events.” Boulton et al. (2022) compare AR(1) in pixels that are in 50 km bands of distance to areas with human activities to determine the importance of the internal forcings in the resilience loss. Would it be possible to make a similar approach with the modeled data, comparing AR(1) auto-correlation values on a pixel basis, in fixed distance bands to impacted areas? Another possibility is the approach used by Wang et al. (2023), who used forest degradation and deterioration maps to test the human impact on auto-correlation values.
Below are a few suggestions of corrections:
- Line 58: “…prior critical transitions,…” should read “… prior to critical transitions,…
- Legend Table 2: I suggest the authors include the explanation of “piControl” in the legend of the table
- Correct citation: Boulton et al (2022) is incorrectly cited as Boulton et al. 2020 in line 171.
- In lines 176/177 the phrase “and one model with 33 realisations did clearly under performs.” should read “underperform”.
References
Boulton, C. A., Lenton, T. M., and Boers, N.: Pronounced loss of Amazon rainforest resilience since the early 2000s, Nature Climate Change, 12, 271–278, https://doi.org/10.1038/s41558-022-01287-8, 2022.
WANG, Huan et al. Anthropogenic disturbance exacerbates resilience loss in the Amazon rainforests. Global Change Biology, v. 30, n. 1, p. e17006, https://doi.org/10.1111/gcb.17006, 2023.
Citation: https://doi.org/10.5194/egusphere-2023-2734-RC2 - AC2: 'Reply on RC2', Raphael Grodofzig, 24 Apr 2024
Interactive discussion
Status: closed
-
RC1: 'Comment on egusphere-2023-2734', Anonymous Referee #1, 22 Jan 2024
Please find my comments in the attached pdf.
- AC1: 'Reply on RC1', Raphael Grodofzig, 24 Apr 2024
-
RC2: 'Comment on egusphere-2023-2734', Anonymous Referee #2, 28 Feb 2024
The manuscript is well written, concise and offers a thorough explanation of the objectives, methods and a good overview of the results. The work follows some of the steps taken by Boulton et al (2022), using lag-1 year auto-correlation (AR(1)) of changes in forest vegetation optical depth (VOD) and Leaf Area Index (LAI) as an early warning signal before reaching critical threshold for forest dieback.
In the results, the authors remark that it is impossible, based solely a single data record, to figure out whether observed changes and trends in auto-correlation of VOD are caused by external forcing or internal variability. To address this problem, they mention that common approaches to detect external (forced) changes are the use of multiple climate model runs, based on different codes, or to use models that start from different initial conditions. They then show, as an example, 30 simulations of the historical experiment, comparing it to one CMIP6 model (MPI-ESM1-2-LR). They show that the observed spatially averaged trend of AR(1) falls within the range of trends of the ensemble members for the same period. They also mention the possibility of investigating simulations of equal length as the historical data, but modeled for a pre-industrial context. After mentioning both examples, they state that the forced response of the Amazon rain forest is not needed to generate an AR(1) increase of similar magnitude as the observed one. And just then they mention that not all models are equally fit for the purpose of simulating the dynamics of the forest in accordance with observations. They then apply the KS test to verify if each ensemble member could have been drawn from the same underlying distribution as the observations, and only four of the nine models pass the test. The model used in both examples mentioned above is one that passes the KS test (MPI-ESM1-2-LR), as it should be. But presenting the above-mentioned examples first, with an important argument for the conclusion, and then showing the “screening” made by using the KS test, may cause some confusion. Thus, I suggest the KS test result is presented before the examples are shown, for increased clarity of the text.
Also, after the second example, the authors state (line 125) “The shorter-term deviations appear slightly muted in this case compared to the historical ensemble, and even if encapsulating the longer term trend the shorter variations are clearly less than those observed, therefore possibly suggesting an influence from historical forcing. Overall, however, the displayed model ensemble suggests that the forced response of the Amazon rain forest is not needed to generate an increase in AR(1) of similar magnitude to that observed”. In other words, two arguments that support an influence from historical forcing are shown, and then a generic argument is given to argue that forced response is not important. Since the main conclusion of the manuscript is that external forcing do not generate a significant change in AR(1), I think a more detailed discussion to support this at this point would be interesting.
In the conclusions, the authors state: “Of the four well performing model ensembles, three of them showed trends similar to observations also in their unforced control simulations. These results suggest that the observed trend could simply be an expression of internal variability, and that longer data records would be needed to show that the opposite is the case.” Is it possible to give an aducated guess on how much longer should the data records be?
Boulton et al (2022) argue that the Amazon is showing signs of resilience loss during a period with three “one-in-a-century” droughts, and the higher frequency of extreme droughts leads to ecological changes, but the replacement of drought sensitive tree species by drought resistant ones happens in a slower pace, which may reduce forest resilience even further. If data was available, could the inclusion of the latest extreme drought (2023) to adjust the models significantly change the outcome of the analysis of this manuscript?
The authors also conclude that “This result is further corroborated by the spatial distribution of the increasing trend in AR(1) in the model simulations. Here it is found that ensemble members with substantial positive or negative trends show these in relatively large regions, but not necessarily in those regions with large anthropogenic deforestation. This suggests that such anomalies are associated with large scale weather events.” Boulton et al. (2022) compare AR(1) in pixels that are in 50 km bands of distance to areas with human activities to determine the importance of the internal forcings in the resilience loss. Would it be possible to make a similar approach with the modeled data, comparing AR(1) auto-correlation values on a pixel basis, in fixed distance bands to impacted areas? Another possibility is the approach used by Wang et al. (2023), who used forest degradation and deterioration maps to test the human impact on auto-correlation values.
Below are a few suggestions of corrections:
- Line 58: “…prior critical transitions,…” should read “… prior to critical transitions,…
- Legend Table 2: I suggest the authors include the explanation of “piControl” in the legend of the table
- Correct citation: Boulton et al (2022) is incorrectly cited as Boulton et al. 2020 in line 171.
- In lines 176/177 the phrase “and one model with 33 realisations did clearly under performs.” should read “underperform”.
References
Boulton, C. A., Lenton, T. M., and Boers, N.: Pronounced loss of Amazon rainforest resilience since the early 2000s, Nature Climate Change, 12, 271–278, https://doi.org/10.1038/s41558-022-01287-8, 2022.
WANG, Huan et al. Anthropogenic disturbance exacerbates resilience loss in the Amazon rainforests. Global Change Biology, v. 30, n. 1, p. e17006, https://doi.org/10.1111/gcb.17006, 2023.
Citation: https://doi.org/10.5194/egusphere-2023-2734-RC2 - AC2: 'Reply on RC2', Raphael Grodofzig, 24 Apr 2024
Peer review completion
Journal article(s) based on this preprint
Viewed
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 311 | 125 | 33 | 469 | 20 | 17 |
- HTML: 311
- PDF: 125
- XML: 33
- Total: 469
- BibTeX: 20
- EndNote: 17
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
Martin Renoult
Thorsten Mauritsen
The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
- Preprint
(3904 KB) - Metadata XML