Spatiotemporal relationships in the structure of the 80-year time series of observations of local surface air temperatures
Journal: Bulletin of the Crimean Astrophysical Observatory
Year: 2012

A semipermanent solar flux arrives to Earth and ensures the observable level of illumination and the average surface temperature. Solar energy incoming to the Earth’s surface is uneven and depends primarily on the Earth’s position in orbit, the speed of its rotation, and local and regional conditions. The sharp increase in the global surface temperature over the past 30 years has been accompanied by corresponding changes in local climate characteristics that significantly affected the state of t