
In the 7500 kilometers from its center to the fringes of its upper atmosphere, the Earth plays host to an array of dynamic processes, operating on a range of length and time scales. Those processes include the convective swirls and eddies of the liquid outer core, which give rise to the planet's magnetic field; the far slower churning of the mantle, which moves whole continents; the intricately coupled interplay of two vast heat reservoirs, the ocean and the atmosphere, which manifests its complexity in climatic oscillations such as El Niño; and the sometimes violent interactions of the outer atmosphere, the magnetosphere, and the solar wind, which create extraterrestrial storm systems that can perturb "space weather" for tens of Earth radii.
The 16 June 2000 Special Issue of Science looks at the state of the art in Earth systems research -- and, in particular, at how the combination of geophysical and geochemical approaches, as well as the application of sophisticated 3D numerical modeling, is allowing new insights on how the planet works. To point you toward some additional online resources, and to add historical perspective to the discussions in the Special Issue, we've prepared this Science Online supplement.