Faculty Opinions recommendation of Mapping carbon accumulation potential from global natural forest regrowth.

Author(s):  
Jianyang Xia
Nature ◽  
2020 ◽  
Vol 585 (7826) ◽  
pp. 545-550 ◽  
Author(s):  
Susan C. Cook-Patton ◽  
Sara M. Leavitt ◽  
David Gibbs ◽  
Nancy L. Harris ◽  
Kristine Lister ◽  
...  

2021 ◽  
Vol 31 (1) ◽  
pp. 182-191
Author(s):  
Borislav Grigorov

Abstract Carbon accumulation in forests is an important step towards achieving better climate mitigation levels. The current research aims at uncovering the link between the NATURA 2000 habitats in Borino Municipality, Southern Bulgaria and the expected carbon sequestration from natural forest regrowth for the period 2020-2050. The case study area currently is of a predominantly mountainous character with a number of forests – a prerequisite for enlargement of the carbon pools. Nevertheless, there are also grassland habitats, which participate in this process as well. The results of the research show that the southern parts of the municipality possess a larger potential for carbon accumulation with levels, reaching 1.10 and 1.28Mg C ha−1 yr−1. The promising outcomes may be used as an example of an investigation of climate mitigation and may serve as a basis for broadening the geographical range in other municipalities in the region.


2021 ◽  
Vol 31 (1) ◽  
pp. 192-199
Author(s):  
Borislav Grigorov

Abstract The present research deals with carbon sequestration, as an important process for mitigating the effects of climate change. The investigation focuses on a 30-year period and it covers only aboveground biomass that builds up from natural forest regrowth, excluding any plantation techniques. Potential carbon sequestration rate from natural forest regrowth in Godech Municipality was measured in Mg C ha−1 yr−1 and the resolution of the map was 1x1 km. The results of the study display that carbon accumulation values in the researched area were consistent with those that were expected in the largest parts of Bulgaria. The biggest share of Godech Municipality falls within the range of 0.82 – 0.96 Mg C ha−1 yr−1 with restricted areas around the villages of Barlya, Smolcha, Gubesh, Murgash and Varbnitsa that may accumulate between 0.96 – 1.11 Mg C ha−1 yr−1. In conclusion, carbon accumulation only from natural forest regrowth provides representative information, however it would have been better if different plantation techniques were regarded as well. The successful results of the investigation should encourage other studies of this type in the neighbouring municipalities.


2021 ◽  
Vol 73 (09) ◽  
pp. 6-6
Author(s):  
Pam Boschee

Purchasing carbon offsets is a widespread means of attempting to meet carbon-reduction and net-zero emissions goals across many industries. Also widespread is the increasing scrutiny of the practice. How “real” are the offsets? How are they quantified and verified, and by whom? Purchasing carbon offsets, or carbon credits, is an option when a company’s efforts to eliminate its carbon emissions through mitigation methods fall short. The offsets are purchased through investments in projects that remove carbon from the atmosphere such as nature-based solutions (e.g., REDD, or reducing emissions from deforestation and forest degradation), negative-emission technologies (including carbon capture and storage [CCS] and bioenergy with CCS), and renewable energy. Here’s where the criticism arises: How is the amount of carbon captured by these projects measured? For example, how much carbon can a tree or forest handle? Are all trees equal in their carbon intake? The uncertainty and variability in carbon-accumulation rates is acknowledged in research studies that are attempting to provide quantification. A study published in Nature compiled more than 13,000 georeferenced measurements to determine the rates for the first 30 years of natural forest regrowth. A map showed more than 100-fold variation in rates across the globe and indicated that default rates from the Intergovernmental Panel on Climate Change may underestimate the rates by 32% on average and do not capture eightfold variation within ecozones. On the other hand, the study concluded that the maximum mitigation potential from natural forest regrowth is 11% lower than previously reported because of the use of overly high rates for locations of potential new forest. While the study was not intended to provide verification to be used in the carbon-offset market, it points to the difficulty in getting the numbers right. Third-party verifiers are casting light on the validity of offsets. Various organizations such as the Climate Registry and the American Carbon Registry (ACR) aim to set standards and best practices. In both the regulated and voluntary carbon markets, ACR says it “oversees the registration and verification of carbon-offset projects following approved carbon accounting methodologies or protocols and issues offsets on a transparent registry system.” In July, CarbonPlan, a nonprofit that analyzes climate solutions based on the best available science and data, rated BCarbon, a standard created by Rice University’s Baker Institute for Public Policy, as one of the best publicly available protocols for soil carbon offsets in the US. BCarbon, a nature-based mitigation system, aims to remove CO2 from the atmosphere and store it in soil as organic carbon. Based on independent verification and certification requirements, the credits under the system are issued for the removal of CO2 by photosynthesis and storage as carbon in soil. Landowners are eligible for storage payments. The Baker Institute said the approach could unlock the potential for removal, storage, and certification of upwards of 1 billion tons of CO2 and lead to the protection and restoration of hundreds of millions of acres of grassland. Scrutiny of carbon offsets is beneficial in this expanding carbon market. Verification and certification will serve to increase the trust of both buyers and sellers—and the public—in what will likely be a bridge toward longer-term solutions to reduce global carbon emissions. And getting the numbers right is essential.


2017 ◽  
Vol 25 (2) ◽  
pp. 199-217 ◽  
Author(s):  
Roland Cochard ◽  
Dung Tri Ngo ◽  
Patrick O. Waeber ◽  
Christian A. Kull

Within a region plagued by deforestation, Vietnam has experienced an exceptional turnaround from net forest loss to forest regrowth. This so-called forest transition, starting in the 1990s, resulted from major changes to environmental and economic policy. Investments in agricultural intensification, reforestation programs, and forestland privatization directly or indirectly promoted natural forest regeneration and the setting-up of plantation forests mainly stocked with exotic species. Forest cover changes, however, varied widely among regions due to specific socio-economic and environmental factors. We studied forest cover changes (including natural and planted forests) and associated drivers in Vietnam’s provinces from 1993–2013. An exhaustive literature review was combined with multivariate statistical analyses of official provincial data. Natural forest regrowth was highest in northern mountain provinces, especially in the period 1993–2003, whereas deforestation continued in the Central Highlands and Southeast Region. Forest plantations increased most in mid-elevation provinces. Statistical results largely confirmed case study-based literature, highlighting the importance of forestland allocation policies and agroforestry extension for promoting small-scale tree plantations and allowing natural forest regeneration in previously degraded areas. Results provide evidence for the abandonment of upland swidden agriculture during 1993–2003, and reveal that spatial competition between expanding natural forests, fixed crop fields, and tree plantations increased during 2003–2013. While we identified a literature gap regarding effects of forest management by para-statal forestry organizations, statistical results showed that natural forests increased in areas managed for protection/regeneration. Cover of other natural forests under the organizations’ management, however, tended to decrease or stagnate, especially more recently when the organizations increasingly turned to multi-purpose plantation forestry. Deforestation processes in the Central Highlands and Southeast Region were mainly driven by cash crop expansion (coffee, rubber) and associated immigration and population growth. Recent data trends indicated limits to further forest expansion, and logging within high-quality natural forests reportedly remained a widespread problem. New schemes for payments for forest environmental services should be strengthened to consolidate the gains from the forest transition, whilst improving forest quality (in terms of biodiversity and environmental services) and allowing local people to actively participate in forest management.


2020 ◽  
Vol 99 ◽  
pp. 105034 ◽  
Author(s):  
Theresa Frei ◽  
Jakob Derks ◽  
Carmen Rodríguez Fernández-Blanco ◽  
Georg Winkel

Geoderma ◽  
2017 ◽  
Vol 297 ◽  
pp. 19-27 ◽  
Author(s):  
Lorenzo Menichetti ◽  
Jens Leifeld ◽  
Lora Kirova ◽  
Sönke Szidat ◽  
Miglena Zhiyanski

2020 ◽  
Author(s):  
Chandra Shekhar Deshmukh ◽  
Dony Julius ◽  
Nardi Nardi ◽  
Ari Putra Susanto ◽  
Nurholis Nurholis

<p>Southeast Asian peatlands, one-third of global tropical peatlands, have sequestered and preserved gigatons of carbon in the past thousands of year. Rainfall fluctuation on yearly and even hourly timescales plays an important role that defines peat carbon accumulation or loss from tropical peatlands. Notably, research related to the ecosystem-scale carbon exchange, including methane (CH<sub>4</sub>), over tropical peatland ecosystems remains limited. Given their significant carbon stocks, the fate of natural tropical peatlands under current and future climate is unknown.</p><p>We performed a study in Kampar Peninsula, a coastal tropical peatland of around 700,000 ha, in Sumatra, Indonesia. This ombrotrophic (acidic and nutrient-poor) peatland largely formed within the past 8000 years. The peninsula is characterized by a large, relatively intact central forest area surrounded by a mosaic of smallholder agricultural land, and industrial fiber wood plantation, smaller secondary forest areas, and undeveloped open and degraded land. We measured the net ecosystem CO<sub>2</sub> and CH<sub>4</sub> exchanges between natural peatland and the atmosphere using the eddy covariance technique over two years (June 2017-May 2019). In addition, peat subsidence rates were measured using polyvinyl chloride poles at every 1 km along 35 km long transect across the natural forest in the peninsula. In the natural forest, groundwater level shows periodic sharp rises and steady decreases corresponding to rain events. The groundwater level can rise up to 20 cm above the peat surface in the wet season, and then in the late dry season can reach -70 cm.</p><p>Our measurements indicate that the natural tropical peatland functioned as a significant source of CO<sub>2</sub> (410±60 g CO<sub>2</sub>-C m<sup>-2</sup> year<sup>-1</sup>) and CH<sub>4</sub> (6.8±0.7 g CH<sub>4</sub>-C m<sup>-2 </sup>year<sup>-1</sup>) to the atmosphere. If we follow IPCC global warming potential (GWP) accounting methodology and apply a 100-year GWP of 34 for CH<sub>4</sub>, this implies that CH<sub>4</sub> emissions contributed ~35% of the 100-year net warming impact. Carbon emissions (due to oxidation of peat, litterfall and coarse wood debris) contributed ~30-35% of the observed subsidence rates. The CO<sub>2</sub> exchanges increased linearly as groundwater level declined. Lower groundwater level enhances peat aeration and potentially increases oxidative peat decomposition, which results in higher CO<sub>2</sub> emissions. The CH<sub>4</sub> exchanges decreased exponentially as groundwater level declined.</p><p>The results indicate that tropical peatland ecosystems are no longer a carbon sink under the current climate. Our results, which are among the first eddy covariance exchange data reported for any tropical peatland, should help to reduce the uncertainty in the estimation of CO<sub>2</sub> and CH<sub>4</sub> emissions from a globally important ecosystem and improve our understanding of the role of natural tropical peatlands under current and future climate.</p>


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