4.7 Article

Holocene climate variations in the Altai Mountains and the surrounding areas: A synthesis of pollen records

期刊

EARTH-SCIENCE REVIEWS
卷 185, 期 -, 页码 847-869

出版社

ELSEVIER SCIENCE BV
DOI: 10.1016/j.earscirev.2018.08.007

关键词

Altai Mountains; Holocene climate change; Pollen; Atlantic Multidecadal Oscillation

资金

  1. Chinese Natural Science Grants [41771234, 41361140361]
  2. Chinese Academy Sciences International Cooperation Program [GJHZ201315]

向作者/读者索取更多资源

Based on pollen data from 30 sequences reviewed here, we reconstruct the spatial and temporal variations in temperature and in aridity that occurred during the Holocene in the Altai Mountains and the surrounding areas (i.e., the examined area). The synthesized regionally-averaged temperature-index curves from low-elevation regions show that the climate was consistently warming from similar to 12,000 to similar to 9000 cal. yr BP and has experienced a gradual cooling trend since similar to 9000 cal. yr BP. It means that the Holocene temperature trend in low-elevation regions of the examined area has sensitively responded to variations in the total solar irradiance. The synthesized regionally-averaged aridity-index curve exhibits a persistent wetting trend during the Holocene in low-elevation regions. The deduced Holocene precipitation-index variations suggest that the Holocene wetting trend resulted from a combined effect of temperature decreasing and precipitation increasing. The Holocene precipitation increase seems to be associated with the Holocene AMO-like (i.e., Atlantic centennial oscillations) events in the North Atlantic Ocean. However, the early-Holocene variations of temperature and aridity in high-elevation regions were significantly deviated from the variations in low-elevation regions and this deviation was probably a result of permafrost thawing at higher elevations.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据