Research articles

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.

Models overestimate Arctic methane emissions compared to observations. Incorporating microbial dynamics into biogeochemistry models helps reconcile this discrepancy; high-affinity methanotrophs are an important part of the Arctic methane budget and double previous estimates of methane sinks.

Costs of achieving climate targets are uncertain. A metamodel estimates the median costs of limiting warming to 2 °C and 1.5 °C to be US$15 trillion and US$30 trillion. Uncertainty in emissions reductions costs dominates at these levels; climate system uncertainty dominates at higher warming levels.

Nitrogen removal occurs primarily through microbially mediated denitrification, which produces the GHG N₂O, and anaerobic ammonium oxidation (anammox), which does not. Warming stimulates denitrification relative to annamox in subtropical sediments, indicating that warming could lead to greater N₂O production.

Coal use is responsible for a large proportion of climate damages. This study shows that phasing out coal yields substantial near-term, local environmental and health benefits that outweigh direct policy costs, providing incentives for immediate climate action.

Concrete production emits high levels of GHGs. It also causes air pollution, with emissions of particulate matter as well as nitrogen and sulfur oxides, which together with GHG emissions cause climate and health damages nearing 75% of the industry value.

Over 60 years of hydrographic data from southeast of Bermuda show the temporal variability of North Atlantic subtropical mode water. Between 2010 and 2018, there was an 86–93% loss of thickness, suggesting weaker production of mode water that is expected to continue with warming.

Changes in the leaf area index alter the distribution of heat and moisture. The change in energy partitioning related to leaf area, increasing latent and decreasing sensible fluxes over the observational period 1982–2016, is moderated by plant functional type and background climate.

Northern peatlands are a significant carbon sink but are vulnerable to decomposition during drought and low water tables. Woody litter added to these ecosystems during high water table conditions leaches polyphenolics that protect carbon stores against decomposition, even during subsequent drought.

Climate change beliefs in the US are politically polarized. Using longitudinal survey data, this study finds that climate change beliefs are less stable over time for Republicans compared with Democrats, suggesting that public beliefs may eventually shift towards broader acceptance.

Erosion is a major problem facing sandy beaches that will probably worsen with climate change and sea-level rise. Half the world’s beaches, many of which are in densely populated areas, could disappear by the end of the century under current trends; mitigation could lessen retreat by 40%.

Exceptionally warm years in 2017–2019 have caused changes in the physical and biological characteristics of the Pacific Arctic Ocean. What these changes mean for the ecosystem and societal consequences will depend on if they are evidence of a transformation or anomalies in the system.

Climate change has led to earlier spring leaf-out in northern temperate and boreal regions. This advanced leaf-out causes warming in the Northern Hemisphere due to the combined effects of water vapour, cloud and snow-albedo feedbacks on the surface energy budget.

Global warming will affect food-web structure and species persistence, and real world data is needed for better prediction. Combining species counts and temperature data from rock pools with dynamic modelling predicts biodiversity increases in arctic to temperate regions and declines in the tropics.

Anthropogenic aerosols mask some greenhouse warming via radiation scattering and cloud interactions. Research suggests the economic impact of this aerosol-induced cooling was small globally, although it benefitted developing countries in warm climates and harmed high-latitude developed countries.

North Pacific mode water controls extratropical-to-tropical heat and mass exchange. Analysis and model simulations show that decadal temperature variations in this subtropical North West Pacific water mass are forced remotely by Atlantic Multidecadal Variability.

Earth’s energy imbalance from human and natural drivers—effective radiative forcing—is difficult to constrain, contributing to uncertainty in long-term climate change. A top-down observational constraint reduces IPCC AR5 assessed uncertainty by nearly 40% and suggests models are biased low.

Intergenerational inheritance of traits in corals can help species survive environmental change. Examination of intergenerational DNA methylation profiles in a reef-building coral shows there to be genome-wide inheritance, with the potential for adaptive capacity to environmental stressors.

Warming in the Arctic has been thought to cause mid-latitude weather and climate changes. Simulations show Arctic changes have small influence outside of high latitudes, with background global warming exerting more influence over mid-latitude winter precipitation and wind changes.