全新世气候变化与太阳活动

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
I. V. Kudryavtsev, V. A. Dergachev, Yu. A. Nagovitsyn
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引用次数: 0

摘要

地球上气候变化的原因是现代科学的主要问题之一。众所周知,太阳辐射是决定地球大气层物理特性的主要因素之一。因此,太阳活动的变化不能不引起地球气候的变化。众所周知,小冰河期发生在地球上的Spörer、蒙德和道尔顿深太阳极小期。这篇文章分析了自最后一次全球冰期结束以来(大约20 000 - 19 000年前)太阳活动和地球气候的变化。特别是,研究表明,马恩多夫变暖、仙女木变冷和铁器时代变冷(公元前一千年)可能与太阳活动的变化有关,就像小冰期一样。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Climate Variations and Solar Activity in the Holocene

Climate Variations and Solar Activity in the Holocene

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 Spörer, 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.

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来源期刊
Geomagnetism and Aeronomy
Geomagnetism and Aeronomy Earth and Planetary Sciences-Space and Planetary Science
CiteScore
1.30
自引率
33.30%
发文量
65
审稿时长
4-8 weeks
期刊介绍: Geomagnetism and Aeronomy is a bimonthly periodical that covers the fields of interplanetary space; geoeffective solar events; the magnetosphere; the ionosphere; the upper and middle atmosphere; the action of solar variability and activity on atmospheric parameters and climate; the main magnetic field and its secular variations, excursion, and inversion; and other related topics.
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