A Forested Wetland at the Tipping-Point: 17-Year, Demographic Evidence of Widespread Recruitment Failure Due to Climate Change

2021 ◽  
Author(s):  
Jonathan P. Evans ◽  
Sarah McCarthy-Neumann ◽  
Angus Pritchard ◽  
Jennifer Cartwright ◽  
William Wolfe
2020 ◽  
Vol 12 (17) ◽  
pp. 6992
Author(s):  
Zhuo Wu ◽  
Erfu Dai ◽  
Wenchuan Guan

Subtropical forests face pressure from both rapidly changing climate and increasing harvest activity in southern China. However, the interactive effects of various spatial processes on forests are not well known. The objective of the present study was to answer the question of how forest aboveground biomass (AGB) changes under alternative climate change and harvesting scenarios and to determine whether there will be a tipping point for forest AGB before 2300. Our simulation results show that, although total forest AGB did not reach a tipping point before 2300 under possible climate change and harvesting scenarios, the slope of the total forest AGB showed a decreasing trend around 2100 and 2200. Moderate climate warming was conducive to AGB accumulation, except for in the high emissions Representative Concentration Pathway (RCP8.5) scenario. Our results also indicate that timber harvesting is adaptable to the accumulation of biomass under climate change scenarios. Harvesting intensity was a key variable affecting forest AGB more than harvesting frequency. Our findings will help develop more sustainable forest management strategies that can adapt to potential climate change scenarios, as well as determining the effectiveness of implementing alternative forest harvesting policies.


Subject Prospects for renewable energy in 2017. Significance The United States and China, the world’s two largest economies as well as the largest carbon emitters, announced their ratification of the Paris Agreement in September. Earlier this year, prices for renewable energy in select regions set historic lows below fossil-fired plants. Renewable energy seems to have passed the tipping point towards gradual adoption as the primary source of electric power while also hopefully preventing catastrophic climate change.


2021 ◽  
Author(s):  
Chris Boulton ◽  
Timothy Lenton ◽  
Niklas Boers

<p>The resilience of the Amazon rainforest to both climate and land use change is of critical importance for biodiversity, regional climate, and the global carbon cycle. Some models project future climate-driven Amazon rainforest dieback (Cox et al. 2000) and others argue that land-use and climate change have already pushed the Amazon close to a tipping point of rainforest dieback and transition to savanna (Lovejoy & Nobre 2018, 2019). But competing effects between rising temperatures, changing precipitation patterns, and CO<sub>2</sub> fertilization, make the future of the Amazon uncertain. An alternative approach is to look for direct observational signals of changing rainforest resilience from timeseries analysis - here of remotely-sensed vegetation optical depth (VOD) (Moesinger et al. 2018), which correlates well with changes in broadleaf tree fraction coverage. Our results indicate that the Amazon rainforest has been losing resilience since the early 2000s, with statistical characteristics evolving consistently with critical slowing down on the way to a bifurcation-induced transition. Specifically, changes in lag-1 autocorrelation of VOD show that resilience is lost faster in regions with less mean annual rainfall. Parts of the rainforest that are closer to human activity are also losing resilience more quickly. Given observed increases in dry-season length, and expanding areas of land use change, the loss of Amazon rainforest resilience is likely to continue. Our results provide direct empirical evidence that the Amazon rainforest is losing stability, risking a sudden dieback that would have profound implications for biodiversity, carbon storage and climate change.</p><p> </p><p>References</p><p>Cox, P. M., Betts, R. A., Jones, C. D., Spall, S. A. & Totterdell, I. J. Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model. Nature 408, 184-187, doi:10.1038/35041539 (2000).</p><p>Lovejoy, T. E. & Nobre, C. Amazon Tipping Point. Science Advances 4, eaat2340, doi:10.1126/sciadv.aat2340 (2018).</p><p>Lovejoy, T. E. & Nobre, C. Amazon tipping point: Last chance for action. Science Advances 5, eaba2949, doi:10.1126/sciadv.aba2949 (2019).</p><p>Moesinger, L. et al. The global long-term microwave Vegetation Optical Depth Climate Archive (VODCA). Earth System Science Data 12, 177-196, doi:10.5194/essd-12-177-2020 (2020).</p><p> </p><p>This work was funded by the Volkswagen foundation and the European Union’s Horizon 2020 research and innovation programme under grant agreement No. 820970.</p>


2020 ◽  
Vol 119 (813) ◽  
pp. 34-36
Author(s):  
Pamela McElwee

Political leaders once again failed to commit to adequate action against climate change, but its increasingly visible impacts have galvanized citizen activists.


2014 ◽  
Vol 25 (4) ◽  
pp. 619-628 ◽  
Author(s):  
Patrick Troy

We are now close to reaching what climate scientists advise is a ‘tipping point’ when the injuries we have visited on the planet will become self-reinforcing and produce an ecosystem that is alien to human life. The mal-distribution of consumption within and between nations is a major reason why there is little agreement on appropriate remedial action. Ensuring planetary survival while reducing inequity is made the more difficult, because the richest one-seventh of the world’s population has already reached consumption levels beyond the capacity of the planetary ecosystem to accommodate it.


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