...录研究_stmopen 关键词】: 渭河 末次间冰期 黄土 粒度 碳酸钙 气候演化 [gap=852]Keywords】: Weihe River,Last Interglacial,loess,grain size,calcium carbonate,climate evolution ..
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the last interglacial age 末次间冰期
the last interglacial 末次间冰期以来
since last interglacial 末次间冰期以来
the last interglacial period 末次间冰期
last interglacial-glacial cycle 末次间冰期
last glacial-interglacial cycle 末次间冰期冰期旋回
In the last interglacial, the upper reaches of Wei River were mainly controlled by the summer monsoon, so it presented much wetter as compared with the northwest of the loess plateau.
末次间冰期,渭河上游受夏季风影响较大,气候相对暖湿,其间的气候较黄土高原西北部湿润,但比黄土高原东南部的要干燥一些。
参考来源 - 末次间冰期以来渭河上游的气候变化·2,447,543篇论文数据，部分数据来源于NoteExpress
The wild climate swings shown by GRIP in the last interglacial are not seen in the GISP2 core.
最后一次间冰期的抓地力所显示的剧烈气候波动在 GISP2 地核中没有出现。
Kopp's team reconstructed the sea levels in the last interglacial period, around 125, 000 years ago.
科普的研究小组重构了约12.5万年以前，最后一次间冰期时期的海平面。
His results, published in the journal Nature, showed that sea levels around the world during the last interglacial were between 6.6m and 9m higher than today.
他的研究结果发表在《自然》杂志上，显示全球海平面在最后一次间冰期时期，比现在高6.6米~ 9米。
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