I. V. Kudryavtsev, V. A. Dergachev, Yu. A. Nagovitsyn
{"title":"Climate Variations and Solar Activity in the Holocene","authors":"I. V. Kudryavtsev, V. A. Dergachev, Yu. A. Nagovitsyn","doi":"10.1134/S0016793224700476","DOIUrl":null,"url":null,"abstract":"<p>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.</p>","PeriodicalId":55597,"journal":{"name":"Geomagnetism and Aeronomy","volume":"64 8","pages":"1342 - 1347"},"PeriodicalIF":0.7000,"publicationDate":"2025-02-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geomagnetism and Aeronomy","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1134/S0016793224700476","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
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.
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.
京公网安备 11010802042870号
京ICP备2023020795号-1
分享
求助内容：
应助结果提醒方式：
扫码关注我们
