摘要
Based on the analysis of carbonate content and loss on ignition for a long sediment core (737 m in length) drilled in Heqing, the orbital scale evolution of the Southwest Monsoon is revealed, by using overlapped spectral analysis and filter methods. It is shown that the obliquity cycle and precession cycle are the key factors for the Southwest Monsoon evolution and that the change of the global ice volume and the uplift of the Qinghai-Tibetan Plateau also impose great influences on it.
| 源语言 | 英语 |
|---|---|
| 页(从-至) | 1813-1819 |
| 页数 | 7 |
| 期刊 | Chinese Science Bulletin |
| 卷 | 52 |
| 期 | 13 |
| DOI | |
| 出版状态 | 已出版 - 7月 2007 |
| 已对外发布 | 是 |
联合国可持续发展目标
此成果有助于实现下列可持续发展目标:
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可持续发展目标 13 气候行动
学术指纹
探究 'The orbital scale evolution of regional climate recorded in a long sediment core from Heqing, China' 的科研主题。它们共同构成独一无二的指纹。引用此
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