Scientists led by Prof. YANG Yuanhe from the Institute of Botany have found that soil carbon dioxide emissions are more sensitive to climate warming in permafrost-collapsed areas than in non-collapsed areas.
Researchers from China, South Korea, France, the United Kingdom, and the United States have reconstructed the weathering history of the Western Pacific island arc over the past 140,000 years, combined with the simulation results from transient climate models, and revealed the temporal and spatial distribution characteristics of deep convection-precipitation evolution in the warm pool.
Researchers led by Prof. WANG Kelin from the Institute of Subtropical Agriculture conducted a seven-year observation and control experiment in a karst region in southern China. To reduce random error, they used new methods to study how synchronized land-use change (starting at the same time and place) affects soil ecological processes and functions were used.
Researchers have documented that persistent millennial-scale Asian winter monsoon intensity fluctuations were superimposed on 41-kyr and ~100-kyr orbital variability during both the warmer late Pliocene and colder early Pleistocene, in response to both external astronomical forcing and internal climate dynamics.
Researchers from the Institute of Applied Ecology have unveiled new advances in the carbon capture capabilities of China's cement industry and its potential contribution to carbon neutrality.
Researchers from the Institute of Applied Ecology have been delving into the mysteries of how different soil types affect these microbial communities and their impact on underground processes.
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