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Climate models predict that by 2020, 20–55% of the three key ocean basins express an anthropogenic fingerprint of change. The well-ventilated Southern Ocean water masses are particularly sensitive, emerging as early as the 1980–1990s, consistent with observations of change over the past 30 years.
Wide-ranging estimates of the social cost of carbon limit its usefulness in setting carbon prices. Near-term to net zero is an alternative modelling approach that focuses on the prices, combined with other policies, needed to set an economy on a pathway consistent with a net-zero emissions target.
Sea-level rise raises water tables, causing flooding from below and saltwater intrusion. A modelling study predicts that coastal California groundwater flooding will expand 50–130 m inland with 1 m of sea-level rise, with areal flooding extent strongly dependent on topography and drainage capacity.
More intense precipitation is an expected consequence of anthropogenic climate change. Now research quantifies the effect of more concentrated rainfall on American agriculture.
Arctic climate in the Last Interglacial (LIG)—a warm period 130,000–116,000 years ago—is poorly simulated by modern climate models. A model with improved sea-ice melt-pond physics reproduces LIG Arctic temperatures, suggests an ice-free Arctic during this period and predicts the same by 2035.
Multilevel network modelling shows that social network exposure promotes both adaptive and transformative responses to climate change among Papua New Guinean islanders. Different social–ecological network structures are associated with adaptation versus transformation.
Short-term extreme weather events such as hourly heat can negatively impact crop yields. US maize and soy yields are damaged by rare extreme hourly downpours, but benefit from more common heavy rainfall, indicating yields may benefit from increasing precipitation intensity under climate change.
Reduced GHG and air pollutant emissions during the COVID-19 lockdowns resulted in declines in NOx emissions of up to 30%, causing short-term cooling, while ~20% SO2 emissions decline countered this for overall minimal temperature effect.
Detecting a human role in a given year of extreme glacier mass loss is difficult at regional scales. Event attribution methods estimate that two extreme mass-loss years in the New Zealand Southern Alps, 2011 and 2018, were at least six and ten times more likely with anthropogenic climate warming.
Warming harms public health in Chinese cities directly via heat and indirectly by worsening air quality. Climate and epidemiological models estimate that reducing aerosols in a warmer climate can enhance atmospheric ventilation, reduce particulate matter exposure and offset warming-driven deaths.
Climate warming over Canada drives glacier retreat and threatens water resources in regions that rely on downstream meltwater. Streamflow and climate data are combined with a municipal water source database to identify Alberta communities whose water supply would be most impacted by glacier retreat.