Articles tagged with Carbon Sinks
A study tracking 300,000 trees over 30 years reveals that tropical forests' carbon sink is weakening, with a feared switch from absorption to emission imminent. The loss of this critical carbon sink capacity is equivalent to a decade of fossil fuel emissions from major countries.
Researchers at University of Göttingen found mangroves absorb carbon efficiently, prioritizing conservation and restoration. The study analyzed a five-meter-deep core of sediment in Segara Anakan Lagoon, revealing the interaction between climate fluctuations and human activity affected carbon accumulation.
Researchers developed a method to monitor tropical forest carbon emissions at unprecedented detail using satellite imagery and machine learning algorithms. The approach quantified the economic cost of deforestation in Peru, revealing areas with significant net losses of forest carbon due to logging and land conversion.
Scientists at Helmholtz Centre for Environmental Research - UFZ developed an approach using recent satellite data to estimate Amazon forest biomass with greater precision. This enables more accurate assessments of the consequences of droughts and forest fires on the Amazon.
A new roadmap outlines critical actions on forests, farming, and food systems to achieve the land sector's 50% emissions reduction by 2050. The study suggests reducing deforestation, peatland drainage, and burning by 70%, restoring forests and coastal mangroves, and shifting one in five people to primarily plant-based diets.
Scientists have found that rising carbon dioxide concentration in the air enhances land carbon sink, a process known as carbon dioxide fertilization. For every 100-ppm increase in CO2, terrestrial carbon sink increases by 0.64 billion tons of carbon per year globally.
Research finds that older stands of trees protect legacy carbon from burning, while younger stands do not. This shift could change boreal forests from a carbon sink to a source, exacerbating climate change. The study's findings have global implications for future climate scenarios.
A new study found that frequent and large wildfires are releasing stored carbon in boreal forests, transforming them into a source of carbon instead of a sink. This shift has significant implications for global climate change and greenhouse gas levels.
Researchers discovered that glacial meltwaters in Canada are a net carbon dioxide sink due to consumption of CO2 in mineral weathering. This finding suggests that glacial meltwaters globally may also act as unrecognized sinks of atmospheric carbon dioxide.
Studies suggest that harvested wood products can store up to 441 megatons of CO2 per year by 2030. However, their net carbon sink value is threatened by global emissions and economic fluctuations that can turn them into a source of emissions.
A study examines ocean carbon sinks over two decades, finding they may account for 10-40% of atmospheric CO2 buildup. Current carbon cycle models underestimate sensitivity to climate variability, suggesting inaccurate global carbon budget predictions.
Researchers found positive correlations between biodiversity conservation and carbon sequestration in ten of twelve landscapes, indicating a shared benefit. The study suggests that increasing biodiversity can also increase carbon storage, highlighting the interconnectedness of these two goals.
Scientists estimated that 1.177 megatonnes of carbon would be lost if all predicted habitat were colonized by beavers, impacting large terrestrial carbon sinks. Invasive mammals like North American beavers pose a significant threat to carbon sequestration in riparian forests.
Young, regrowing forests in middle and high latitudes and areas with reforestation programs take up large amounts of CO2. This age effect accounts for about 25% of forests' CO2 uptake.
Scientists at the University of Sydney have modelled how marine snow absorbs carbon dioxide over millennia, keeping the planet cool. The study found that carbonate accumulation in deep-sea sediments has increased significantly over time, with a net increase in total volume of carbonate sediments in the oceans.
Research at the University of Birmingham reveals that young forests are a substantial contributor to the world's carbon sink, accounting for around 25% of total carbon dioxide absorption. These forests, typically in temperate zones, have been re-growing on land with previously experienced human activities.
Climate researchers warn that peatlands in the Peruvian Amazon may lose up to 500 million tons of carbon by the end of the century due to warmer temperatures and increased precipitation. This loss could lead to a significant increase in global carbon emissions, exacerbating climate change.
A study simulating Amazonian peatland dynamics from 2100 AD to 12,000 years ago finds that peatlands may become a net source of carbon under changing climate conditions. Basin peatland and non-peatland soils are predicted to release up to 0.4 petagrams of carbon by 2100.
Peatlands, which store up to 530 billion tons of global carbon, are vulnerable to climate change due to changing temperature and precipitation patterns. The study found that temperate regions in warmer periods can accumulate more carbon than tropical regions, but ultimately release it as warming intensifies.
New research suggests global warming will cause peatlands to absorb more carbon initially, but the effect will weaken as warming increases. The study highlights the importance of protecting intact peatlands and restoring drained peatlands to prevent rapid rates of peat decomposition.
Beaver dams raise water levels, releasing organic carbon to the atmosphere. Research indicates beavers can act as both carbon sinks and sources, with some ponds fixing up to 470,000 tons of carbon per year or releasing 820,000 tons annually.
A new study of lake sediments reveals that increased westerly winds are likely to reduce the Southern Ocean's ability to absorb carbon dioxide from the atmosphere. This could accelerate climate change as the Southern Ocean currently absorbs over 40% of human-produced carbon dioxide.
A University of California, Davis study found that grasslands are more resilient carbon sinks than forests in 21st century California, especially when considering the impacts of droughts and wildfires. Grasslands store most of their carbon underground, making them a viable option for carbon offset efforts.
Researchers reexamined ocean circulations and river carbon transport, finding the Southern Ocean is a smaller carbon sink than thought. Land in the northern hemisphere absorbs less carbon, but rivers send it to the ocean with increased strength, challenging current estimates.
Peatland initiation coincided with warming and increased precipitation, forming globally important carbon sinks. The study's findings have implications for future changes in peatland distribution.
A new study reveals that tropical forests act as a net source of carbon dioxide, with most releases caused by deforestation and degradation. The majority of land areas in the tropics showed no significant change in carbon over the 12-year period, but those that did experienced losses mainly due to deforestation.
Climate change threatens tropical peat swamps, which once removed carbon dioxide from the atmosphere. Peatland forests in Southeast Asia have been disappearing due to clear-cutting and drainage projects, now potentially destroying forested peatlands.
New research shows that forests 'held their breath' during the recent global warming slowdown, releasing less carbon back into the atmosphere. During this period of slower warming, worldwide forests took up more carbon dioxide through photosynthesis and stored it in the natural environment.
A recent study by University of Exeter researchers found that temperature fluctuations drive the year-to-year variability of global land-based carbon sinks. Locally, however, water availability is the dominant factor in determining the success of carbon sinks.
A study by the University of Southern Denmark reveals that Thurøbund's protected and productive bay stores a record amount of carbon, with an average of 27,000 grams per square meter. This exceeds global estimates of seagrass meadow storage, highlighting the importance of preserving these ecosystems.
A recent study found that fragmented forest edges in New England absorb more carbon than expected due to increased growth rates, but also experience more heat stress. This mixed outcome suggests that while forests may be valuable carbon sinks, they are also sensitive to climate change.
Researchers estimate that seaweed globally sequesters 173 trillion grams of carbon per year, with 90% of this being due to transport into deep-sea sediments. This highlights the significance of seaweed as a major carbon sink, surpassing Amazonian forests.
A recent study published in Global Biogeochemical Cycles reveals that the Amazon Basin's carbon sink was completely shut down by a severe drought. Meanwhile, an international team is working to provide an up-to-date assessment of polar ice mass losses and their contributions to global sea level rise.
A new study found that major green donors allocate most of their climate mitigation funding to developing countries with large carbon sinks and good governance. This funding often overlooks least-developed countries, diverting public finance from poor nations and exacerbating global inequality.
A recent study by researchers at the Universities of Exeter and Leeds found that a drought completely shut down the Amazon Basin's carbon sink, killing trees and slowing their growth. The study used long-term measurements from the RAINFOR network to examine tree responses during two large-scale droughts occurring in 2005 and 2010.
Researchers at the University of Exeter found that peatland ecosystems' ability to absorb and store carbon is threatened by rising sea levels due to increased salt concentrations. The study highlights the vulnerability of blanket bogs in Northwest Scotland to sea-level rise, which could lead to a sharp decline in carbon storage.
A University of Minnesota study found that plants can acclimate to warmer temperatures, releasing significantly less additional carbon dioxide than previously believed. The 'B4Warmed' project simulated the effects of climate change on 10 tree species, revealing a 5% increase in leaf respiration compared to ambient temperatures.
A University of Queensland-led study assesses the amount of carbon stored in tropical forests recovering after land-clearing practices in the Philippines. Regenerating secondary forests are substantial carbon sinks, increasing their capacity to store carbon with abandonment age.
A study has uncovered a complex planktonic network influencing the ocean's biological carbon pump, which removes carbon from the atmosphere. The research found that certain bacterial and viral genes predict variations in carbon export, enabling better predictions of climate change effects.
Researchers found that tropical secondary forests exhibit a high level of resilience and can sequester large amounts of carbon. These new-growth forests have accumulated enough biomass to uptake 3.05 tons of carbon per hectare per year, 11 times the rate of old-growth forests.
A recent study discovered that West Antarctic seabed life is a significant carbon sink, removing excess CO2 from the atmosphere. This finding suggests that maximizing natural carbon capture by seabed life could help reduce global CO2 levels.
A study by the USDA Forest Service found that landscapes with 50-60% forest land use had statistically the same sink strength as those with 90-100% forest. This suggests that land use change is a substantial component of the forest carbon sink in the Eastern United States, and new approaches like establishing new forests may help seque...
New studies reveal that the Southern Ocean has increasingly removed more carbon dioxide from the atmosphere since 2002. The research, compiled from millions of ship-based observations, suggests that the Southern Ocean's carbon sink is strengthening, contrary to previous findings.
The Southern Ocean's carbon sink has revived after 'saturating' since 2005 due to changes in weather patterns. The reinvigoration is attributed to variations in wind and temperature, enabling the ocean to absorb more CO2 from the atmosphere.
The Southern Ocean's carbon sink has renewed its strength, absorbing more atmospheric carbon dioxide over the past decade. This improvement is attributed to changes in sea surface temperature and dissolved inorganic carbon levels.
Research from the University of East Anglia reveals that the Southern Ocean's carbon sink has reinvigorated after a decade of stagnant absorption. The team attributes this change to shifts in wind patterns and temperature, which have led to increased upwelling of deep waters containing higher concentrations of dissolved CO2.
Researchers will investigate how disturbances like fire and insect infestation are changing the Earth's carbon absorption, and use models to optimize observation networks for detecting impact on ecosystem carbon balance. The project aims to understand how terrestrial landscapes are shifting from being a net carbon sink to a source.
A new study found that climate models significantly disagree on the amount of atmospheric carbon dioxide sequestered in Northern Eurasian tundra and boreal ecosystems. The region's land carbon sink has been strengthening in recent decades, but some models now show signs of weakening.
A new study suggests that the world's deserts may be storing significant amounts of climate-changing carbon dioxide, with estimates suggesting up to 20 billion metric tons stored in underground aquifers. This discovery could improve models used to predict future climate change and enhance calculations of the Earth's carbon budget.
Researchers estimate that fjords bury about 18 million tonnes of organic carbon annually, equivalent to 11% of global marine carbon burial. Fjords are 'hotspots' for carbon burial due to their deep and stable environments.
Recent research showed that replacing chemical fertilizer with organic manure significantly decreased greenhouse gas emissions. Organic farming improved crop yields while reversing the agriculture ecosystem's role as a carbon source, becoming a carbon sink.
Researchers at Woods Hole Oceanographic Institution discovered that stressed and dying phytoplankton release chemicals that stimulate marine bacteria to quickly convert organic carbon back into CO2. This process reduces the amount of sinking detritus, releasing more CO2 into the shallow ocean and atmosphere.
A recent paper by University of South Carolina paleoceanographer Kelly Gibson shows that rapid climate change affected marine ecosystems in the Cariaco Basin, a body of water off Venezuela's coast. The study used nitrogen isotope ratios to estimate changes in primary productivity and carbon sequestration in the ocean.
The loss of underwater posidonia meadows reduces their ability to capture and store atmospheric CO2, and can also lead to the release of stored carbon into the atmosphere. Seagrass meadows, like those studied, play a crucial role in mitigating anthropogenic emissions by capturing carbon.
A recent study from the University of British Columbia found that high seas fish and aquatic life remove 1.5 billion tonnes of carbon dioxide annually, valued at $148 billion US. This compares to the $16 billion paid for 10 million tonnes of caught fish, highlighting their importance as a natural carbon sink.
New research reveals dryland ecosystems have emerged as a significant driver of the global carbon cycle, contributing to a four-fold increase in net carbon uptake. The study highlights the impact of climate extremes and desert greening on ecosystem processes, with surprising interactions discovered between natural events and biomes.
A study by two students at Linköping University found that aquatic environments in India emit 42% of expected natural carbon dioxide equivalents, highlighting the importance of reducing fossil carbon emissions. Methane accounts for 71% of these emissions, providing a potential pathway to reduction through water pollution mitigation.
New research suggests that global warming of four degrees or more will lead to a saturation point for vegetation's ability to absorb CO2, resulting in a decrease in the 'carbon sink' effect. This shift in focus could change how scientists approach understanding and mitigating climate change.
A new analysis published in Nature suggests that the coastal ocean now takes in more carbon dioxide than it releases, potentially impacting global predictions related to climate change. Researchers propose a mechanism for the shift, which could make the coastal ocean a more important carbon sink in the future.
Researchers at MIT found that the Arctic Ocean is becoming a more efficient carbon sink due to increased biological growth in summer months. However, some regions, such as the Barents Sea, become carbon sources, emitting carbon dioxide into the atmosphere.