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来自印度太平洋热水池的2000年的温度和水文重建
Delia W Oppo1, Yair Rosenthal, Braddock K Linsley
1Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA. doppo@whoi.edu
Nature
|August 29, 2009
概括
来自热带印度-太平洋热池的新海面温度重建揭示了过去的气候变化. 这份记录显示,20世纪末期的气候变暖比以往更高,与北半球的气候趋势一致.
科学领域:
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
背景情况:
- 北半球温度重建表明最近的变暖.
- 热带地区,特别是印太热带 (IPWP),对全球气候至关重要.
- 现有的重建依赖于陆地数据,忽视了海洋的影响.
研究的目的:
- 在IPWP中重建过去两千年的海面温度 (SST).
- 将基于代理的SST数据与仪器记录和北半球趋势进行比较.
- 了解IPWP水文学对东亚季风系统的影响.
主要方法:
- 从马卡萨海峡,印度尼西亚,十年来解决了连续SST重建.
- 利用代理数据重叠仪器记录进行直接比较.
- 伴随海水三角洲的重建(18) O作为盐度和水文学指标.
主要成果:
- IPWP SST重建显示了与北半球温度重建类似的趋势.
- 重建的SSTs可以与中世纪温暖时期 (1000-1250年) 的现代价值相比较.
- 小冰河时代的海面温度低于现代值,具有显著的变化.
结论:
- IPWP SST记录提供了关于热带气候变化的宝贵长期观点.
- IPWP水文学与东亚季风系统在百年至千年的时间尺度上紧密相结合.
- 过去的IPWP温度变化为了解当前和未来的气候变化提供了背景.
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