Opposing wet and dry conditions in Central and mainland Southeast Asia over the past millennium were controlled by climate variability over the Pacific and Indian oceans, a pattern likely to become more severe due to ongoing warming, according to an analysis of palaeoclimate records…
Source: Nature Geoscience | Springer Nature Limited
Nature Geoscience | Springer Nature Limited
- Contrasting drivers of South Asian summer and winter monsoon evolution during the last deglaciation
- Opposing hydroclimate extremes in Central and mainland Southeast Asia over past millennium
- Negative core–mantle boundary heat flux beneath low-shear-wave-velocity provinces
- Enhanced marine burial of terrestrial organic carbon through the Palaeocene–Eocene Thermal Maximum
- Vigorous mantle convection triggered the Cretaceous Pacific large igneous provinces
- Observed stratospheric mean age decrease consistent with circulation acceleration
- The pace of stratospheric circulation
- Tracking hydrogen migration in iron under Earth’s core conditions
Nature PodcastThe Nature Podcast brings you the best stories from the world of science each week. We cover everything from astronomy to zoology, highlighting the most exciting research from each issue of the Nature journal. We meet the scientists behind the results and provide in-depth analysis from Nature’s journalists and editors…
