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Przyczyny i mechanizmy zmian klimatu w plejstocenie : state of art

Hrynowiecka A.

Przegląd Geologiczny

2016

Vol. 64, nr 1

26--34

The reason of cyclic climate change during the Pleistocene is probably so-called Milankovitch cycles, consisting of three main orbital parameters of the Earth: the shape of Earth’s orbit eccentricity, axial tilt of Earth and precession – change in the direction of the Earth’s axis. They also impact on the insolation, which significantly contributes to the formation of ice sheets. The climate is conditioned largely by energy derived from the sun, dependent on the current solar activity. Specific configurations of these factors have contributed to the formation of glacial-interglacial cycles in the past; they have today and will have an impact on the climate of our planet in the future.