Climatic variations since the Little Ice Age recorded in the Guliya Ice Core
Climatic variations since the Little Ice Age recorded in the Guliya Ice Core
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DOI：
10.1360/yd1996-39-6-587
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发表时间：
1996-11
影响因子：
5.7
通讯作者：
Y. Tandong;Jiao Ke-qin;Tian Lide;Y. Zhihong;Shi Wei-lin;L. Thompson
中科院分区：
文献类型：
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作者：
Y. Tandong;Jiao Ke-qin;Tian Lide;Y. Zhihong;Shi Wei-lin;L. Thompson
根据古里雅冰芯的δ18O记录和古里雅冰芯的积累记录，讨论了古里雅冰芯小冰期以来的气候变化。根据记录，可以观测到1570年以来的几次明显的气候波动事件。在过去的400年中，17世纪和19世纪是降水量较少的相对凉爽时期，18世纪和20世纪是降水量较高的相对温暖时期。研究还揭示了高原气温与降水的密切关系。暖化对应降水偏多，冷化对应降水偏少，这与季风对该地区的影响有关。
The climatic variations since the Little Ice Age recorded in the Guliya Ice Core are discussed based on glacial δ18O and accumulation records in the Guliya Ice Core. Several obvious climate fluctuation events since 1570 can be observed according to the records. In the past 400 years, the 17th and 19th centuries are relatively cool periods with less precipitation, and the 18th and 20th centuries are relatively warm periods with high precipitation. The study has also revealed the close relationship between temperature and precipitation on the plateau. Warming corresponds to high precipitation and cooling corresponds to less precipitation, which is related with the influence of monsoon on this region.