Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain
the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in
Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles
and JavaScript.
Drought-induced forest dieback has emerged as a global concern and is expected to increase worldwide under projected future climate change. A study using long-term forest plots now provides a quantitative estimate of drought-induced increase in tree mortality across Canada's boreal forests—one of the most important terrestrial carbon sinks.
A significant proportion of the US public believe that climate scientists widely disagree about climate change. Now a survey-based study investigates whether this misperception is important and finds that individuals who believe there is broad scientific disagreement tend to feel less certain that global warming is occurring and show less support for climate policy.
Decisions about how soon, how quickly and by how much carbon dioxide emissions are reduced will determine whether the climate target of limiting warming to 2 °C can be met. Research reveals that it will probably only be possible if ambitious reductions are implemented within the next two decades and emissions eventually fall to zero.
Both greenhouse gas emissions and changes in land use and cover have modified the Earth’s climate since preindustrial times. A modelling study now shows that the impact of land-cover change on regional climate depends critically on how snow cover and rainfall change under increased greenhouse gases.
Global climate models have a well-known bias in the position and strength of the Southern Hemisphere westerly winds. Research reveals that this bias increases carbon uptake by the ocean, reducing atmospheric carbon dioxide concentrations, in climate model simulations—a result that should help constrain uncertainties in climate model projections.
The ‘pathway’ the world needs to follow to limit global temperature rise to 2 °C remains uncertain. Analysis that takes technical and economic constraints on reducing emissions into account indicates that emissions need to peak in the next decade and then fall rapidly to have a good chance of achieving this goal.
Substituting fossil fuels with bioenergy from forests, as well as thinning forests to reduce wildfire emissions, has been proposed as a means of cutting carbon dioxide emissions. A study based on inventory data for US West Coast forests now challenges this proposal, and finds that it could lead to 2–14% higher emissions than current management practices over the next 20 years.
The West Antarctic Peninsula has experienced rapid warming in recent decades. One of the effects has been a loss of the ‘fast-ice’ skin, or frozen layer, that forms on the sea surface each winter and reduces seabed scouring. A study now links increased seabed scouring over the past 25 years to higher benthic mortality, with implications for the region’s biodiversity.
Little information exists to guide conservation planning under climate change uncertainty. Now a study combines ecological predictions with an economic decision framework to investigate strategies to minimize extinction risk in one of the world’s most threatened ecosystems—the South African fynbos. The research finds that the best conservation options vary nonlinearly with available budget.
In some decades, such as 2000–2009, the observed globally averaged surface-temperature time series has shown a flat or slightly negative trend. A modelling study provides evidence that heat uptake by the deep ocean may cause these hiatus periods and may be linked to La Niña-like conditions.
Climate impacts on biodiversity are usually assessed at the morphospecies level. An analysis of the distribution and mitochondrial DNA variability of nine montane aquatic insect species in Europe suggests range contractions will be accompanied by severe loss of genetic diversity. These results imply that morphospecies-scale assessments may greatly underestimate potential biodiversity losses from climate change.
Ocean acidification poses a threat to marine calcifiers, but their response varies widely. An analysis of Mediterranean corals and molluscs now shows that the ability to continue shell and skeleton growth in corrosive seawater is determined in part by the existence of outer organic protective layers. High temperatures, however, modify resistance to acidification.
Enhanced tropical forest productivity, facilitated by increasing carbon dioxide concentrations, could act as a substantial carbon sink. However, a long-term field experiment shows that increased leaf-litter inputs to the soil as productivity rises could stimulate the release of significant amounts of soil carbon, partially offsetting predicted gains in carbon storage.
Managed relocation, whereby species are moved to a more suitable habitat, has been proposed as a means of combating negative climate-change impacts on biodiversity. A quantitative decision framework to evaluate the optimal timing of relocation shows that in some cases, such as when population size is small, haste is ill advised.
The abundance of persistent organic pollutants (POPs) in the Arctic atmosphere has decreased over recent decades owing to international restrictions and regulations. However, an analysis confirms that warming is remobilizing POPs into the atmosphere from sinks such as snow and ice, a process that will increase the risk of exposure to these toxic chemicals.
The hydrological cycle is ultimately driven by solar energy, so it is not surprising that energy constraints affect the response of rainfall to climate change at a global level. Now analysis shows that the regional response of rainfall to greenhouse-gas-driven warming can also be understood from an energetic perspective.
The importance of disease in modulating ecosystem responses to climate change remains poorly understood. A seven-year study of the effects of increased snow cover on tundra plant communities in Sweden found that, although plant growth was favoured by increased snow, biomass and carbon-balance trends were reversed by a pathogen outbreak.
Preventing deforestation—a key goal of international climate policy—can incur an opportunity cost for local communities who depend on forest resources for their livelihoods. A study compares the cost of carbon conservation through forest protection with that of a scheme that directly alleviates the demand for forest conversion.
Subzero temperatures at high latitudes typically restrict shipping but facilitate ground transportation. A study quantifies the impacts of climate change on Arctic transportation by mid-century and finds that all eight Arctic states will probably suffer steep declines in inland transport, but will reap the benefits of faster sea travel.
Ocean acidification due to anthropogenic carbon dioxide emissions has negative effects on many marine organisms, but the long-term impacts are less well known. A study into the effects of natural carbon dioxide seeps on coral reefs and seagrasses confirms model predictions that acidification may contribute to reduced diversity and resilience.