| http://www.w3.org/ns/prov#value | - But the physics is such that, rather than a horizontally-diffuse vertical overturning that varies smoothly over time according to the radiative forcing and feedbacks, the overturning tends to occur in localized updrafts that vary signicantly over periods of time far shorter than the diurnal heating cycle or, for that matter, larger-scale weather processes such as the development of a synoptic-scal
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