scholarly journals Development of the Forest Carbon Sink Index on Afforestation and Reforestation Activities

2014 ◽  
Vol 103 (1) ◽  
pp. 137-146 ◽  
Author(s):  
Minkyung Song ◽  
Jae Soo Bae ◽  
Mi Hyun Seol
Keyword(s):  
2020 ◽  
Vol 11 (1) ◽  
Author(s):  
R. J. W. Brienen ◽  
L. Caldwell ◽  
L. Duchesne ◽  
S. Voelker ◽  
J. Barichivich ◽  
...  

Abstract Land vegetation is currently taking up large amounts of atmospheric CO2, possibly due to tree growth stimulation. Extant models predict that this growth stimulation will continue to cause a net carbon uptake this century. However, there are indications that increased growth rates may shorten trees′ lifespan and thus recent increases in forest carbon stocks may be transient due to lagged increases in mortality. Here we show that growth-lifespan trade-offs are indeed near universal, occurring across almost all species and climates. This trade-off is directly linked to faster growth reducing tree lifespan, and not due to covariance with climate or environment. Thus, current tree growth stimulation will, inevitably, result in a lagged increase in canopy tree mortality, as is indeed widely observed, and eventually neutralise carbon gains due to growth stimulation. Results from a strongly data-based forest simulator confirm these expectations. Extant Earth system model projections of global forest carbon sink persistence are likely too optimistic, increasing the need to curb greenhouse gas emissions.


2017 ◽  
Author(s):  
Chaocheng Zheng ◽  
Yi Zhang ◽  
Dongxiang Cheng
Keyword(s):  

2020 ◽  
Author(s):  
Wannes Hubau ◽  
Simon L. Lewis ◽  
Oliver L. Phillips ◽  
Hans Beeckman ◽  

<p>Structurally intact tropical forests sequestered ~1 Pg C yr<sup>-1</sup> over the 1990s and early 2000s, equivalent to ~15% of fossil fuel emissions. Climate-driven vegetation models typically predict that this carbon sink will continue for the remainder of the 21<sup>st</sup> century. However, recent plot inventories from Amazonia show a declining rate of carbon sequestration, potentially signaling an imminent end to the sink. Here we assess whether the African tropical forest sink is also declining.</p><p>Records from 244 multi-census plots across 11 countries reveal that the African tropical forest sink in aboveground live biomass has been stable for three decades, at 0.66 Mg C ha<sup>-1</sup> yr<sup>-1</sup>, from 1985-2015 (95% CI, 0.53-0.79). Thus, the carbon sink responses of Earth’s two largest expanses of tropical forest have diverged over recent decades. A statistical model including CO<sub>2</sub>, temperature, drought, and forest dynamics can account for the trends. Despite the past stability of the African carbon sink, our data and model show that very recently the sink has begun decreasing, and that it will continue to decline in the future.  This implies that the intact tropical forest carbon sink on both continents is set to end decades sooner than even the most extreme vegetation model estimates.</p><p>Published independent observations of inter-hemispheric atmospheric CO<sub>2</sub> concentration indicate increasing carbon uptake into the Northern hemisphere landmass, offsetting a weakening of the tropical forest sink, which reinforces our conclusion that the intact tropical forest carbon sink has already saturated. Nevertheless, continued on-the-ground monitoring of the world’s remaining intact tropical forests will be required to test our prediction that the intact tropical forest carbon sink will continue to decline. Our findings were recently published in Nature (March 2020) and have important policy implications: given tropical forests are likely to sequester less carbon in the future than Earth System Models predict, an earlier date to reach net zero anthropogenic greenhouse gas emissions will be required to meet any given commitment to limit the global heating of Earth.</p>


2009 ◽  
Vol 29 (2) ◽  
pp. 161-168 ◽  
Author(s):  
Elena Dalla Valle ◽  
Silvia Lamedica ◽  
Roberto Pilli ◽  
Tommaso Anfodillo

2013 ◽  
Vol 734-737 ◽  
pp. 1848-1851
Author(s):  
Yi Fei Weng

Through forestation and carbon-sink transactions, coal enterprises can not only protect the environment in coal mining areas, but also obtain the financial returns. In this paper, first of all main thought and principles in establishing forest carbon-sink market in coal industry are discussed. Then trading mechanism is designed including CM-CERs and CM-VERs, as well as the operational mechanism with the respects of factors in the market, supply and demand mechanism, price mechanism and risk mechanism. Afterward construction of primary and secondary markets of forest carbon-sink is researched. Finally the conception of integrate with Market in China through Panda Standard and World through CDM of carbon-sink are provided.


2020 ◽  
Author(s):  
Natalia Kowalska ◽  
Georg Jocher ◽  
Ladislav Šigut ◽  
Marian Pavelka

<p>Since the eddy covariance (EC) method became a key method for measurements of the energy and greenhouse gas exchange between ecosystems and the atmosphere, a large number of studies was conducted to understand the mechanisms driving the carbon exchange in forest ecosystems. In recent years, case studies further focused on testing and validating the applicability of the EC technique above forest ecosystems, also assessing the spatial and temporal variability of sub canopy fluxes. These studies led to the conclusion that there is a high probability of overestimating the forest carbon sink strength with EC measurements above the forest canopy only, as these measurements may miss respiration components from within and below the canopy due to insufficient mixing across the canopy. Additional below canopy EC measurements were suggested to tackle this problem and to get information about potential decoupling between below and above forest canopy air masses as well as potentially missing respiration components in the above canopy derived signal.</p><p>The overall goal of the study here is to derive an as detailed as possible understanding of the carbon exchange in Lanžhot floodplain forest with the help of concurrent EC measurements below and above the forest canopy. Lanžhot floodplain forest is situated 6.5 km north of the confluence of the Morava and Thaya rivers in Czech Republic (48.6815483 N, 16.9463317 E). The long-term average annual precipitation at this site is around 517 mm and the mean annual temperature is 9.5 °C. The average groundwater level is -2.7 m. Since a long time flooding occurs here very rarely, the last flooding event was in 2013. In addition, the site is hydrologically managed. Consequently, the water regime of the site changed over the years and represents nowadays relatively dry conditions for such type of ecosystem.</p><p>To reach our research goal we evaluate different single- and two-level filtering strategies of the above canopy derived carbon exchange values and the impact of these filterings on the annual ecosystem carbon exchange rates. Our hypothesis is that conventional single-level EC flux filtering strategies like the u<sub>*</sub>-filtering might not be sufficient to fully capture the carbon exchange of the studied floodplain forest ecosystem. We further hypothesize that additional below canopy EC measurements are mandatory to achieve unbiased forest carbon exchange values with the EC technique.</p>


2014 ◽  
Vol 1010-1012 ◽  
pp. 1903-1906
Author(s):  
Chuang Hong Shang ◽  
Zhi Hong Xu ◽  
Jun Wang

In post-Kyoto Protocol times, forest carbon-sink has become one of the key path choices to realize clean development for coal mining area to govern ecological environmental pollution. In practice, big challenge is to set up effective and systematic government policies for forest carbon-sink in coal mines. For China, it is just at beginning in policies. Currently, China’s forest carbon-sink policies for coal mines ought to be set up in terms of industry, finance and law.


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