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Crabeater seals feed predominantly on Antarctic krill. Combining seal tracks and diving behaviour with environmental variables allows the future foraging habitat, and therefore krill distribution, to be predicted, suggesting a shift offshore and south along the western Antarctic Peninsula.
The Galapagos Islands inspired the theory of evolution by means of natural selection; now in the Anthropocene, the Galapagos represent an important natural laboratory to understand ecosystem resilience in the face of climate extremes and enable effective socio-ecological co-evolution under climate change.
Antarctic krill play a key role in Southern Ocean food webs but are vulnerable to climate change, with habitat shifts predicted in response. Now, a study of climate change impacts on a krill-specialist predator — the crabeater seal — suggests that this abundant marine mammal may be forced southwards with its prey.
Under rising CO2, most plants constrict their stomata, lose less water via transpiration and photosynthesize more efficiently. A global dataset of tree-ring isotope measurements reveals a slowdown in water-use efficiency gains over the twentieth century, with marked spatiotemporal variability.
Despite strict controls on precursor emissions, ozone air pollution has not decreased over Europe in recent decades. This is largely attributed to water-stressed vegetation; during heatwaves and drought, plants are less effective at ozone removal via stomata, worsening peak ozone pollution episodes.
Snow in the mountains provides a natural reservoir, storing water in the cold season for use later in the year. Now research demonstrates that reduced mountain snowpack due to rising temperatures makes drought harder to predict and jeopardizes irrigated agriculture throughout the world.
Policy makers debate whether responding to climate change can be complementary to economic growth. New research tracking competing economic ideas across the environmental debate shows that climate change is increasingly seen as an opportunity; however, many still argue that growth and climate action are in conflict.
This Perspective maps the history of climate targets and shows how the international goal of avoiding dangerous climate change has been reinterpreted in the light of new modelling methods and technological promises, ultimately enabling policy prevarication and limiting mitigation.
Since 1980, European nations have made a tremendous effort to mitigate ozone pollution by reducing emissions, only to achieve limited success. Research now shows that vegetation stressed by heat and drought conditions has partly thwarted these actions.
Natural decadal variability has a role in global mean surface temperature trends. Observational data and modelling show that since the mid-1980s, the tropical eastern Pacific variability and the cold ocean–warm land pattern have covaried to enhance acceleration and deceleration in warming trends.
Climate warming causes less mountain precipitation to fall as snow. Hydrologic simulations predict that in a high-end emissions scenario, this decreases the predictability of seasonal water resources across the western United States, with low-elevation coastal areas impacted most strongly.
Arctic lakes and their resident fish species are warming rapidly. Geospatial analysis of Canadian Arctic lakes predicts a 20% increase in lake trout productivity by 2050 and a 29% increase in harvestable biomass across an expanded range.
This analysis of global climate policy reports shows how economic ideas have shaped climate policy. The authors find a shift from neoclassical dominance to a more diversified discourse, which has expanded policy choices beyond market-based policies to include green innovation and industrial policy.
Snowmelt runoff is an important source of water for irrigating agricultural crops in high-mountain Asia, Central Asia, western Russia, western US and the southern Andes. Climate change places water resources in these basins at risk, indicating the need to adapt water management.
Climate change will increase the intensity and frequency of a range of natural hazards, from floods to wildfires, which impact the built environment. More research is needed on buildings and infrastructure performance under different climate-driven events to support recovery predictions and effective mitigation policies.
Characterizing infrastructure vulnerability to climate change is essential given the long asset lives, criticality of services delivered and high costs of upgrading and maintaining these systems. Reconciling uncertainty from past infrastructure design decisions with future uncertainty of climate change will help prioritize limited resources to high risk assets.