Adaptation
Storm Surge Reduction by MangrovesBackgroundFlooding and wave energy from storm surges can damage infrastructure and harm inhabitants of coastal communities. Climate change and sea level rise have the potential to increase or intensify storm surges, which necessitate investment in coastal defenses and disaster risk reduction. Mangroves can reduce the effects of storm surges through attenuating waves and wind, making mangroves an important form of nature-based protection for coastal communities. Open access copy available |
Reduction of Wind and Swell Waves by MangrovesBackgroundCoastal ecosystems can mitigate the damage from extreme weather events like tropical storms and hurricanes. With human populations increasing in coastal areas, policymakers and stakeholders are interested in coastal ecosystems, like mangrove forests, as a nature-based form of coastal defense and resilience. This report aims to examine the potential for mangroves to reduce wind and swell waves in order to inform decision makers about the potential for mangroves to decrease the risks faced by coastal communities. Open access copy available |
Forest carbon in Amazonia: the unrecognized contribution of indigenous territories and protected natural areasBackgroundAmazonia stores an estimated 80–120 Pg of aboveground carbon, and changes in this stock have global climate implications. Indigenous territories (ITs) and protected natural areas (PNAs) together cover roughly one-third to one-half of the Amazon region, yet their specific contribution to maintaining forest carbon has often been overlooked in regional mitigation discussions. Quantifying their role is important for designing REDD+, climate finance, and land rights policies that reflect on-the-ground conservation performance. Open access copy available |
Overestimated natural biological nitrogen fixation translates to an exaggerated CO2 fertilization effectBackgroundBiological nitrogen fixation (BNF) supplies a substantial fraction of reactive nitrogen of ecosystems, typically estimated in the tens to over 100 Tg N yr⁻¹ globally, thus constraining how strongly plants can respond to rising CO2. Many Earth system models (ESMs) parameterize BNF such that nitrogen does not strongly limit CO2 fertilization, potentially inflating modelled land carbon sinks and underestimating future atmospheric CO2 concentrations. Quantifying this bias is important for realistic carbon budget and mitigation assessments. Open access copy available |
Global Carbon Budget 2025Background“Global Carbon Budget 2025” extends the living dataset on anthropogenic carbon dioxide (CO2) emissions and their redistribution among atmosphere, ocean, and land, updating trends through 2024, and providing preliminary 2025 estimates. Atmospheric CO2 has risen from about 278 ppm in 1750 to 422.8 ± 0.1 ppm in 2024, with recent growth amplified by the 2023–2024 El Niño event. This paper highlights the continued dominance of fossil fuel emissions, persistent sources of land-use change, and climate-driven modulation of land and ocean sinks within the broader carbon-climate system. Open access copy available |
Global Carbon Budget 2024Background“Global Carbon Budget 2024” assesses how anthropogenic carbon dioxide (CO2) emissions disrupt the global carbon cycle relative to pre-industrial conditions, when atmospheric CO2 was about 278 ppm in 1750. The study focuses on emissions from fossil fuels and land-use change and how these are partitioned between the atmosphere, ocean, and terrestrial biosphere. Recent changes, in the context of long-term trends since 1958, emphasize the role of deforestation, fossil fuel combustion, and climate variability, such as El Niño, in shaping CO2 fluxes. Open access copy available |
Decreasing landscape carbon storage in western US forests with 2 °C of warmingBackgroundThis study investigates how a 2°C increase in global mean temperature above pre-industrial levels could alter above-ground carbon storage in forests across the western United States, a region already experiencing climate-driven tree mortality, reduced regeneration, and more frequent fire and insect outbreaks. Forest carbon density is treated as a “carbon carrying capacity” controlled by climate and disturbance regimes, and there is concern that warming and drying will shift many areas towards lower carbon forest or non-forest states, with implications for climate mitigation and carbon offset projects. Open access copy available |
Elevation, aspect, and climate shape blue pine (Pinus wallichiana) biomass and carbon dynamics in the Bhutanese HimalayasBackgroundForests cover over two-thirds of Bhutan and are constitutionally protected, enabling national carbon neutrality. Yet, climate change, increasing temperatures, variable precipitation, and heightened wildfire risk threaten carbon storage capacity and species distributions. Blue pine is a fast-growing, socio-economically important species dominating inner dry valleys between roughly 2200–3000 m, making it an ideal model to understand how elevation and slope aspect regulate biomass accumulation and carbon sequestration under changing climate conditions. Open access copy available |
Bridging conservation and policy: evaluating national targets to reduce mangrove loss under the Kunming–Montreal biodiversity frameworkBackgroundThis research examines the alignment between the Kunming–Montreal Global Biodiversity Framework (GBF) targets and national efforts to halt mangrove loss. Under the Convention on Biological Diversity, GBF’s Targets 1 and 3 aim to reduce habitat loss and expand protected areas to conserve 30% of critical ecosystems by 2030. Mangroves, vital for biodiversity, carbon storage, and coastal protection, continue to experience degradation due to both human and natural drivers. Despite partial success in global mangrove protection, national policies often fail to address underlying drivers of degradation or incorporate specific, measurable conservation actions. Open access copy available |
Warming induces unexpectedly high soil respiration in a wet tropical forestBackgroundTropical forests play a key role in regulating the global carbon cycle, exchanging more carbon dioxide with the atmosphere than any other terrestrial biome. However, limited in situ experiments constrain understanding of their response to climate warming. Understanding these responses is crucial, as even small changes in soil respiration in tropical regions can substantially influence global carbon dynamics and climate feedbacks. Open access copy available |
