Mechanism of Formation of Long-Term Directional Climate Changes in the Past and Current Centuries

A. V. Dzyuba and G. N. Panin

Climatic changes of the past century are diagnosed based on the generalized empirical data. Considered is a forcing impact of interannual inhomogeneity of the angular velocity of the Earth on the pressure field, atmospheric circulation, and radiation balance of the climate system. A physical mechanism of formation of global climate change tendencies as a response to the composition of greenhouse and rotational effects is described. Possible climate changes in the current century are assessed.