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The changing Amazon forest.

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TLDR
Evidence for concerted changes in the structure, dynamics and composition of old-growth Amazonian forests in the late twentieth century is examined and any switch from carbon sink to source would have profound implications for global climate, biodiversity and human welfare.
Abstract
than 10 cm diameter increased by 0.62G0.23 t C ha K1 yr K1 averaged across the basin. This implies a carbon sink in Neotropical old-growth forest of at least 0.49G0.18 Pg C yr K1 . If other biomass and necromass components are also increased proportionally, then the old-growth forest sink here has been 0.79G0.29 Pg C yr K1 , even before allowing for any gains in soil carbon stocks. This is approximately equal to the carbon emissions to the atmosphere by Amazon deforestation. There is also evidence for recent changes in Amazon biodiversity. In the future, the growth response of remaining old-growth mature Amazon forests will saturate, and these ecosystems may switch from sink to source driven by higher respiration (temperature), higher mortality (as outputs equilibrate to the growth inputs and periodic drought) or compositional change (disturbances). Any switch from carbon sink to source would have profound implications for global climate, biodiversity and human welfare, while the documented acceleration of tree growth and mortality may already be affecting the interactions among millions of species.

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On underestimation of global vulnerability to tree mortality and forest die‐off from hotter drought in the Anthropocene

TL;DR: In this article, the authors identify ten contrasting perspectives that shape the vulnerability debate but have not been discussed collectively and present a set of global vulnerability drivers that are known with high confidence: (1) droughts eventually occur everywhere; (2) warming produces hotter Droughts; (3) atmospheric moisture demand increases nonlinearly with temperature during drought; (4) mortality can occur faster in hotter Drought, consistent with fundamental physiology; (5) shorter Drought can become lethal under warming, increasing the frequency of lethal Drought; and (6) mortality happens rapidly
References
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Climate change 2007: the physical science basis

TL;DR: The first volume of the IPCC's Fourth Assessment Report as mentioned in this paper was published in 2007 and covers several topics including the extensive range of observations now available for the atmosphere and surface, changes in sea level, assesses the paleoclimatic perspective, climate change causes both natural and anthropogenic, and climate models for projections of global climate.
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A globally coherent fingerprint of climate change impacts across natural systems

TL;DR: A diagnostic fingerprint of temporal and spatial ‘sign-switching’ responses uniquely predicted by twentieth century climate trends is defined and generates ‘very high confidence’ (as laid down by the IPCC) that climate change is already affecting living systems.
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Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model

TL;DR: Results from a fully coupled, three-dimensional carbon–climate model are presented, indicating that carbon-cycle feedbacks could significantly accelerate climate change over the twenty-first century.
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Amazon in the mature stage

The mature Amazon forests are currently acting as a carbon sink, absorbing significant amounts of carbon dioxide, but may transition to a carbon source due to environmental stress and compositional changes.