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ROLE OF THE RADIATION FACTOR IN GLOBAL CLIMATIC EVENTS OF THE LATE HOLOCENE
1 Lomonosov Moscow State University
2 Instituto de Geofisica, Universidad Nacional Autonoma de México
3 Harvard & Smithsonian Center for Astrophysics
4 Institute of Earth Physics and Space Science
5 Universidad Tecnológica Nacional, Grupo de Estudios Ambientales
2 Instituto de Geofisica, Universidad Nacional Autonoma de México
3 Harvard & Smithsonian Center for Astrophysics
4 Institute of Earth Physics and Space Science
5 Universidad Tecnológica Nacional, Grupo de Estudios Ambientales
Journal: Geophysical processes and biosphere
Tome: 20
Number: 3
Year: 2021
Pages: 5-19
UDK: 551.551.1+551.581
DOI: 10.21455/GPB2021.3-1
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FEDOROV V.M., FROLOV D.M., VELASCO H.V.M.N., SOON W.W., CIONCO R.G. ROLE OF THE RADIATION FACTOR IN GLOBAL CLIMATIC EVENTS OF THE LATE HOLOCENE // . 2021. Т. 20. № 3. С. 5-19. DOI: 10.21455/GPB2021.3-1
@article{FEDOROVROLE2021,
author = "FEDOROV, V. M. and FROLOV, D. M. and VELASCO, H. V. M. N. and SOON, W. W. and CIONCO, R. G.",
title = "ROLE OF THE RADIATION FACTOR IN GLOBAL CLIMATIC EVENTS OF THE LATE HOLOCENE",
journal = "Geophysical processes and biosphere",
year = 2021,
volume = "20",
number = "3",
pages = "5-19",
doi = "10.21455/GPB2021.3-1",
language = "English"
}
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Keywords: insolation, insolation characteristics, heat exchange, solar activity, late Holocene, Little Ice Age, medieval climatic optimum
Аnnotation: On the basis of the performed calculations of insolation and insolation characteristics, taking into account changes in solar activity, the causes of global climatic events in the late Holocene were determined. The main reasons for the Little Ice Age are the long and deep minimum of summer insolation and insolation seasonality in the northern hemisphere. The values of the minimums are fixed in the range of approximately 1400-1750. The depth of the minimum over the past 5000 years, taking into account the change in solar activity, is about 8.0 W/m
