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Link to original content: https://www.nature.com/ngeo.rss
Nature Geoscience Nature Geoscience is a monthly journal dedicated to publishing high-quality original research papers across all areas of the geosciences. The journal’s content reflects all the disciplines within the geosciences, including studies of the Earth’s climate system, the solid Earth and the planets. Nature Geoscience covers studies based on all the methods used by geoscientists, ranging from field work and numerical modelling on regional and global scales to theoretical studies and remote sensing. Physical, chemical and biological investigations that contribute to our understanding of the Earth system or the planets are all represented. http://feeds.nature.com/ngeo/rss/current Nature Publishing Group en © 2024 Macmillan Publishers Limited, part of Springer Nature. All rights reserved. Nature Geoscience © 2024 Macmillan Publishers Limited, part of Springer Nature. All rights reserved. permissions@nature.com Nature Geoscience https://www.nature.com/uploads/product/ngeo/rss.gif http://feeds.nature.com/ngeo/rss/current <![CDATA[Author Correction: Oxygen priming induced by elevated CO<sub>2</sub> reduces carbon accumulation and methane emissions in coastal wetlands]]> https://www.nature.com/articles/s41561-024-01611-1 Nature Geoscience, Published online: 22 November 2024; doi:10.1038/s41561-024-01611-1

Author Correction: Oxygen priming induced by elevated CO2 reduces carbon accumulation and methane emissions in coastal wetlands]]> 2 reduces carbon accumulation and methane emissions in coastal wetlands]]> Genevieve L. NoyceAlexander J. SmithMatthew L. KirwanRoy L. RichJ. Patrick Megonigal doi:10.1038/s41561-024-01611-1 Nature Geoscience, Published online: 2024-11-22; | doi:10.1038/s41561-024-01611-1 2024-11-22 Nature Geoscience 10.1038/s41561-024-01611-1 https://www.nature.com/articles/s41561-024-01611-1 <![CDATA[Multi-month forecasts of marine heatwaves and ocean acidification extremes]]> https://www.nature.com/articles/s41561-024-01593-0 Nature Geoscience, Published online: 21 November 2024; doi:10.1038/s41561-024-01593-0

One type of ocean acidification extreme event, as well as marine heatwaves, can be confidently predicted up to 1 year in advance, according to forecasts stemming from an Earth system model ensemble.]]> Samuel C. MogenNicole S. LovenduskiStephen G. YeagerAntonietta CapotondiMichael G. JacoxStephen BogradEmanuele Di LorenzoElliot L. HazenMercedes Pozo BuilWho KimNan Rosenbloom doi:10.1038/s41561-024-01593-0 Nature Geoscience, Published online: 2024-11-21; | doi:10.1038/s41561-024-01593-0 2024-11-21 Nature Geoscience 10.1038/s41561-024-01593-0 https://www.nature.com/articles/s41561-024-01593-0 <![CDATA[Arctic freshwater anomaly transiting to the North Atlantic delayed within a buffer zone]]> https://www.nature.com/articles/s41561-024-01592-1 Nature Geoscience, Published online: 20 November 2024; doi:10.1038/s41561-024-01592-1

Freshwater being released from the Beaufort Gyre is accumulating in an Arctic Ocean buffer zone before it can reach the North Atlantic, according to an analysis of satellite observation and modelling.]]> Qiang WangSergey DanilovThomas Jung doi:10.1038/s41561-024-01592-1 Nature Geoscience, Published online: 2024-11-20; | doi:10.1038/s41561-024-01592-1 2024-11-20 Nature Geoscience 10.1038/s41561-024-01592-1 https://www.nature.com/articles/s41561-024-01592-1 <![CDATA[Low-elevation forest extent in the western United States constrained by soil surface temperatures]]> https://www.nature.com/articles/s41561-024-01577-0 Nature Geoscience, Published online: 19 November 2024; doi:10.1038/s41561-024-01577-0

Soil surface temperatures constrain the low-elevation extent of forests in the western United States through their direct effects on seedling mortality, according to analyses of the relationship between post-fire tree recruitment and soil surface temperature across this region.]]> Zachary A. HoldenSolomon Z. DobrowskiAlan SwansonZachary HoylmanDrew LyonsAllen WarrenMarco Maneta doi:10.1038/s41561-024-01577-0 Nature Geoscience, Published online: 2024-11-19; | doi:10.1038/s41561-024-01577-0 2024-11-19 Nature Geoscience 10.1038/s41561-024-01577-0 https://www.nature.com/articles/s41561-024-01577-0 <![CDATA[Weakening of the Atlantic Meridional Overturning Circulation driven by subarctic freshening since the mid-twentieth century]]> https://www.nature.com/articles/s41561-024-01568-1 Nature Geoscience, Published online: 18 November 2024; doi:10.1038/s41561-024-01568-1

Fresh meltwater entering the Labrador and Irminger seas has resulted in a slowing of the Atlantic Meridional Overturning Circulation since the 1950s, according to a combination of modelling approaches.]]> Gabriel M. PontesLaurie Menviel doi:10.1038/s41561-024-01568-1 Nature Geoscience, Published online: 2024-11-18; | doi:10.1038/s41561-024-01568-1 2024-11-18 Nature Geoscience 10.1038/s41561-024-01568-1 https://www.nature.com/articles/s41561-024-01568-1 <![CDATA[Recovery of ecosystem productivity in China due to the Clean Air Action plan]]> https://www.nature.com/articles/s41561-024-01586-z Nature Geoscience, Published online: 15 November 2024; doi:10.1038/s41561-024-01586-z

A quantitative assessment suggests that the reductions in aerosol and ozone levels from 2014 to 2020 due to the clean air action in China led to a substantial increase in the national net primary productivity due to the weakened aerosol climatic effects, alleviated ozone vegetation damage and enhanced light availability.]]> Hao ZhouXu YueHuibin DaiGuannan GengWenping YuanJiquan ChenGuofeng ShenTianyi ZhangJun ZhuHong Liao doi:10.1038/s41561-024-01586-z Nature Geoscience, Published online: 2024-11-15; | doi:10.1038/s41561-024-01586-z 2024-11-15 Nature Geoscience 10.1038/s41561-024-01586-z https://www.nature.com/articles/s41561-024-01586-z <![CDATA[Coupled decline in ocean pH and carbonate saturation during the Palaeocene–Eocene Thermal Maximum]]> https://www.nature.com/articles/s41561-024-01579-y Nature Geoscience, Published online: 12 November 2024; doi:10.1038/s41561-024-01579-y

Elevated atmospheric CO2 during the Palaeocene–Eocene Thermal Maximum coincided with substantial declines in the pH and carbonate saturation state of the ocean.]]> Mingsong LiLee R. KumpAndy RidgwellJessica E. TierneyGregory J. HakimSteven B. MalevichChristopher J. PoulsenRobert TardifHaoxun ZhangJiang Zhu doi:10.1038/s41561-024-01579-y Nature Geoscience, Published online: 2024-11-12; | doi:10.1038/s41561-024-01579-y 2024-11-12 Nature Geoscience 10.1038/s41561-024-01579-y https://www.nature.com/articles/s41561-024-01579-y <![CDATA[Estimated human-induced warming from a linear temperature and atmospheric CO<sub>2</sub> relationship]]> https://www.nature.com/articles/s41561-024-01580-5 Nature Geoscience, Published online: 11 November 2024; doi:10.1038/s41561-024-01580-5

Humans have caused 1.49 °C of warming compared with a pre-1700 baseline, a global estimate based on the linear relationship between atmospheric CO2 and temperature.]]> 2 relationship]]> Andrew JarvisPiers M. Forster doi:10.1038/s41561-024-01580-5 Nature Geoscience, Published online: 2024-11-11; | doi:10.1038/s41561-024-01580-5 2024-11-11 Nature Geoscience 10.1038/s41561-024-01580-5 https://www.nature.com/articles/s41561-024-01580-5