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The dominant external forces influencing the rate of change of the Earth System have been astronomical and geophysical during the planet’s 4.5-billion-year existence. In the last six decades, anthropogenic forcings have driven exceptionally rapid rates of change in the Earth System. This new regime can be represented by an ‘Anthropocene equation’, where other forcings tend to zero, and the rate of change under human influence can be estimated. Reducing the risk of leaving the glacial–interglacial limit cycle of the late Quaternary for an uncertain future will require, in the first instance, the rate of change of the Earth System to become approximately zero.
Research news | 2020-02-21
Despite rapid urban growth, agriculture in a wetland area in the south of Mexico City soldiers on, more than a millennium after its birth
Research news | 2020-02-19
Malin Falkenmark calls for a shift towards a water based biosphere stewardship. The alternative, she warns, could be catastrophic
Research news | 2020-02-17
Trying to reach the goals under current business-as-usual will come at a heavy price on the planetary boundaries
Research news | 2020-02-14
The new "Our Future On Earth" report provides risks analysis based on survey of 222 global sustainability experts, including centre researchers
Research news | 2020-02-13
New assessment aims to fill critical gaps in understanding the growing role aquatic foods play in the global food system
Research news | 2020-02-09
A new study harmonizes the water planetary boundary with local boundaries for the La Cienega wetlands in Colombia