Climate Variations and Solar Activity in the Holocene

被引：0

作者：

Kudryavtsev, I. V. ^{[1
,2
]}

Dergachev, V. A. ^{[1
]}

Nagovitsyn, Yu. A. ^{[2
,3
]}

机构：

[1] Ioffe Inst, St Petersburg, Russia

[2] Russian Acad Sci, Main Pulkovo Astron Observ, St Petersburg, Russia

[3] State Univ Aerosp Instrumentat, St Petersburg, Russia

来源：

GEOMAGNETISM AND AERONOMY | 2024年 / 64卷 / 08期

关键词：

NORTHERN-HEMISPHERE TEMPERATURES; COSMIC-RAYS; RADIOCARBON DATA; ICE-SHEET; RECONSTRUCTION; C-14; CO2; IRRADIANCE; ISOTOPE; CARBON;

D O I：

10.1134/S0016793224700476

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

The causes of climate change on Earth represent one of the main questions in modern science. As is known, solar radiation is one of the main factors that determines the physical characteristics of Earth's atmosphere. Therefore, changes in solar activity cannot but lead to changes in Earth's climate. It is well known that the Little Ice Age took place on Earth during the Sporer, Maunder, and Dalton deep solar minima. The article analyzes changes in solar activity and Earth's climate since the beginning of the end of the last global glaciation (approximately 20 000-19 000 years ago). In particular, it is shown that the Mayendorff warming, Dryas coolings, and the Iron Age cooling (in the first millennium BCE) could be associated with changes in solar activity, just like the Little Ice Age.

引用

页码：1342 / 1347

页数：6

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