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DOI | 10.1360/02yd0219 |
Climatic significance of delta O-18 records from an 80.36 m ice core in the East Rongbuk Glacier, Mount Qomolangma (Everest) | |
Zhang, DQ; Qin, DH; Hou, SG; Kang, SC; Ren, JW; Mayewski, PA | |
发表日期 | 2005 |
ISSN | 1006-9313 |
起始页码 | 266 |
结束页码 | 272 |
卷号 | 48期号:2 |
英文摘要 | The delta O-18 variations in an 80-36 m ice core retrieved in the accumulation zone of the East Rongbuk Glacier, Mount Qomolangma (Everest), is not consistent with changes of air temperature from both southern and northern slopes of Himalayas, as well as these of the temperature. anomalies over the Northern Hemisphere. The negative relationship between the 5180 and the net accumulation records of the ice core suggests the amount effect of summer precipitation on the delta O-18 values in the region. Therefore, the delta O-18 records of the East Rongbuk ice core should be a proxy of Indian Summer Monsoon intensity, which shows lower delta O-18 values during strong monsoon phases and higher values during weak phases. |
关键词 | PRECIPITATIONTEMPERATUREO-18 |
英文关键词 | East Rongbuk ice core; delta O-18 values; air temperature; Indian Summer Monsoon |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000228190600014 |
来源期刊 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/158707 |
推荐引用方式 GB/T 7714 | Zhang, DQ,Qin, DH,Hou, SG,et al. Climatic significance of delta O-18 records from an 80.36 m ice core in the East Rongbuk Glacier, Mount Qomolangma (Everest)[J]. 中国科学院青藏高原研究所,2005,48(2). |
APA | Zhang, DQ,Qin, DH,Hou, SG,Kang, SC,Ren, JW,&Mayewski, PA.(2005).Climatic significance of delta O-18 records from an 80.36 m ice core in the East Rongbuk Glacier, Mount Qomolangma (Everest).SCIENCE IN CHINA SERIES D-EARTH SCIENCES,48(2). |
MLA | Zhang, DQ,et al."Climatic significance of delta O-18 records from an 80.36 m ice core in the East Rongbuk Glacier, Mount Qomolangma (Everest)".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 48.2(2005). |
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