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Synergistic Interactions Between Warming and Elevated Atmospheric CO 2 Increase Soil Organic Carbon SequestrationNARA Subscribed
Warming and elevated CO 2 (eCO 2 ) are two potentially opposing climate‐carbon (C) feedback mechanisms that modulate the magnitude of the land C sink, with warming decreasing and eCO 2 increasing C sequestration. However, their net effect on soil organic C (SOC)—the largest terrestrial C stock—remains uncertain. Here, we quantify how warming, eCO 2 , and their interactions influence SOC by using 5558 paired observations from 1...
What Do Latest CMIP6 Global Climate Models Say About Future Arctic Sea Ice Coverage Changes?NARA Subscribed
Observational evidence of rapid Arctic sea ice decline motivates the need for reliable projections of first ice‐free Arctic summer year (FIASY). Remotely sensed observations, combined with outcomes from global climate models, provide a foundation to characterise the future state of the Arctic. Modelling of sea ice dynamics has significantly improved between CMIP5 and CMIP6, with nearly three times as many models capturing real...
Precision measurement of the Ds*+-Ds+ meson mass differenceNARA Subscribed
Soil organic carbon (SOC) sequestration is vital for food security and climate mitigation. However, its long‐term response to fertilisation remains unclear. Using the 180‐year Broadbalk Experiment (the world's longest‐running fertilisation trial; Rothamsted, UK), combined with 14 C labelling and metagenomics, we identified fundamentally distinct mechanisms of SOC accumulation: a microbially mediated dual pathway under organic...