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在过去的55万年里,中度半球间的水文波动波动在过去的55万年里发生了
Kyoung-nam Jo1, Kyung Sik Woo2, Sangheon Yi1
1Korea Institute of Geoscience and Mineral Resources, Daejeon 305-350, South Korea.
Nature
|April 4, 2014
概括
一项研究显示,由热带融合区 (ITCZ) 的变化驱动的半球间水文波动波动延伸到中度地区. 这种在韩国洞穴中观察到的现象影响了温带气候系统和全球冰河时代周期.
科学领域:
- 古气候学 古气候学
- 气候动力学 气候动力学
- 地质化学 地质化学
背景情况:
- 热带融合区 (ITCZ) 通过度变化影响区域降水.
- 一个半球间的水文波动描述了半球之间反相降水趋势.
- 以前的研究表明,这种摇摆在热带和亚热带地区运作.
研究的目的:
- 研究半球间水文波动对高度地区和全球气候系统的影响.
- 为了确定在热带地区观察到的水文反相延伸到中度.
主要方法:
- 来自朝鲜半岛的55万年长的洞穴生长频率记录的分析.
- 将韩国洞穴数据与南半球洞穴记录进行比较,以确定半球反相.
主要成果:
- 半球降水反相,表明水文波动,在西太平洋中度地区被确定,延伸到东北亚.
- 在过去的55万年里,半球间水文波动的影响至少达到中度.
结论:
- 轨道时间尺度ITCZ转移显著影响温带气候系统.
- 半球间的水文波动可能会影响北半球中度地区的水蒸气和植被反,并可能调节四分期冰期周期.
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