HOLOCENE CLIMATE OPTIMUM AS A MODEL OF THE GLOBAL CLIMATE OF THE BEGINNING OF THE 21ST CENTURY.

被引：0

作者：

Borzenkova, I.I.

Zubakov, V.A.

机构：

来源：

Soviet meteorology and hydrology | 1984年 / 08期

关键词：

ATMOSPHERIC TEMPERATURE - GEOLOGY - GLACIERS - OXYGEN - Isotopes - RAIN AND RAINFALL;

D O I：

暂无

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学科分类号：

摘要：

The global climate events of the last 16,000 years are discussed, based on various indirect data (paleontological, oxygen isotope, glaciological, etc. ) using the radiocarbon method. Noted is the complexity of climate fluctuations in the late glacial period, the Holocene. Two climatic optimums are identified most clearly: Early Boreal (8. 9-8. 8 thousand years ago) and Late Atlantic (6. 2-5. 5 thousand years ago). This work presents schematic maps of the difference in summer air temperature and mean global precipitation totals between the time of the climatic optimum (6. 2-5. 5 thousand years ago) and the modern epoch.

引用

页码：52 / 58

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