Earth’s Cryosphere, 2019, Vol. XXIII, № 4, p. 31-36
COMMENTARIES ON THE ARTICLE “IMPACTS OF CLIMATE CHANGE ON LONG-TERM DYNAMICS OF SEASONAL FREEZING IN MOSCOW REGION: RETROSPECTIVE ANALYSIS AND UNCERTAINTIES IN FORECASTING FOR THE SECOND HALF OF THE 21ST CENTURY”
BY S.P. POZDNYAKOV, S.O. GRINEVSKYI, E.A. DEDIULINA
V.М. Fedorov
Lomonosov Moscow State University, 1, Leninskie Gory, Moscow, 119991, Russia; fedorov.msu@mail.ru
The use of physical and mathematical models for forecasting the dynamics of seasonal freezing in Moscow region and the results’ uncertainty have prompted the analysis of general and specific problems of physical and mathematical modeling of climate, as well as the climate system components and characteristics. The solution of these problems can contribute to the improvement of physical and mathematical models and long-term forecasting of climate change processes in the Earth’s cryosphere.
Cryosphere, seasonally frozen layer, dynamics, prediction, simulation, solar radiation, variation of insolation, meridional gradient in insolation, climate change factors