the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Multi-fold increase in rainforests tipping risk beyond 1.5–2 °C warming
Chandrakant Singh
Ruud van der Ent
Ingo Fetzer
Lan Wang-Erlandsson
Abstract. Tropical rainforests invest in their root systems to store moisture in their root zone from water-rich periods for use in water-scarce periods. An inadequate root-zone soil moisture storage predisposes or forces these forest ecosystems to transition to a savanna-like state, devoid of their native structure and functions. Yet changes in soil moisture storage and its influence on the rainforest ecosystems under future climate change remain uncertain. Using the (mass-balance-based) empirical understanding of root zone storage capacity, we assess the future state of the rainforests and the forest-to-savanna transition risk in South America and Africa under four different shared socioeconomic pathway scenarios. We find that under the end-of-the-21st-century climate, nearly one-third of the total forest area will be influenced by climate change. Furthermore, beyond 1.5–2 °C warming, ecosystem recovery reduces gradually, whereas the forest-savanna transition risk increases several folds. For Amazon, this risk can grow by about 1.5–6 times compared to its immediate lower warming scenario, whereas for Congo, this risk growth is not substantial (0.7–1.65 times). The insight from this study underscores the urgent need to limit global surface temperatures below the Paris Agreement.
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Chandrakant Singh et al.
Status: open (until 05 Oct 2023)
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RC1: 'Comment on egusphere-2023-1486', Anonymous Referee #1, 27 Sep 2023
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General comments:
Singh et al. classified the tropical terrestrial ecosystems under current climate and future climate by calculating the hydroclimate-derived root zone storage capacity. Then they assessed the potential rainforests tipping risk with the global warming. They found that the forest-savanna transition risk would largely increase if the climate warming is beyond 1.5-2 degrees. The topic is meaningful and interesting since the land cover change used in current ESMs of CMIP6 is lacked of the consideration of the effects of hydroclimate.
However, readers could be hard to follow and even confused in the main text, because some introduction of method and discussions are not easy to understand. More importantly, the main findings are not clearly shown in the main text. For example, in the Abstract, the “1.5-6 times” growth is the key finding for this study (also corresponding to the title), but how these values are derived is not shown.
In this study, >20% of model convergence are regarded as ‘moderate mode agreement’ or ‘moderate-high model agreement’. Given that the findings with >20% of model convergence are important in this research, I doubt whether the 20% is too low to hardly help obtain the robust results.
It is interesting to compare the prescribed future land-use in IAMs with the projected transitions in this study. But it is not clear for readers which results are more robust. Readers cannot figure it out from the discussions of the authors. For example, on the one hand, the author said the extent of forest-savanna transitions is often underestimated in prescribed land-use compared to those projected in their study. In this case, it seems that results from this study are regarded as more robust. However, on the other hand, the authors said forests that revert to a ‘less water-stressed state’ is overestimated in their analysis. It seems that results from the prescribed future land-use in IAMs are more robust.
Specific comments:
Line 28: which scenario for this growth by about 1.5-6 times.
Lines 98-100: please explain why the hydroclimate and ecosystem can be regarded as in equilibrium. The hydroclimate and ecosystem are projected by ESM in SSP scenario simulations, which are apparently not in equilibrium because of the continued warming.
Lines 130-131: The spatial resolutions of most of ESMs output are close to 0.25 degree? I suppose that the spatial resolutions of most of ESMs are much lower than 0.25 degree.
Line 162: “to reduce loss of root zone moisture storage”?
Line 183: “the actual state of the ecosystems” includes many aspects of ecosystems. “this model can capture the dynamics of actual soil moisture availability for the ecosystems” would be better.
Line 380-381: please add the references of related figure(s).
Lines 590-592: But as shown in Figure 3, even in SSP1-2.6, there are still many regions belonging to “Transition to a more water-stressed state”.
Citation: https://doi.org/10.5194/egusphere-2023-1486-RC1
Chandrakant Singh et al.
Chandrakant Singh et al.
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