亚极链接到现代赤道太平洋冷舌的出现
Alfredo Martínez-Garcia1, Antoni Rosell-Melé, Erin L McClymont
1Geological Institute, ETH Zürich, 8092 Zürich, Switzerland. alfredo.martinez-garcia@erdw.ethz.ch
概括
由于南极和北极地区的降温,太平洋冷舌形成了. 这种冷却也改变了气候模式,支持了在世-普世过渡期间海洋学变化的假设.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 海洋学 海洋学 海洋学
背景情况:
- 东方赤道太平洋的冷舌是影响全球气候的关键海洋特征.
- 它的普略纪-普列斯托纪发展与热带热带冷却所驱动的热带热带排放有关.
研究的目的:
- 研究南极和南极地区的同步冷却与冷舌发展.
- 为了检查亚南极洲气候对轨道变化的反应变化的变化.
主要方法:
- 从亚南极和亚北极地区的古气候代理数据的分析.
- 区域冷却的时间与冷舌的出现相比较.
- 评估气候对地球轨道周期的反应的变化.
主要成果:
- 亚南极和亚北极地区发生了相当大的冷却,与冷舌发展相吻合.
- 亚南极气候从亚热带气候转变为亚极气候,以应对轨道强迫.
- 有证据支持这样的假设:海洋冷却导致热线积聚和旋转缩.
结论:
- 热带外的冷却在平世-普世时期的太平洋冷舌的发展中发挥了重要作用.
- 观察到的气候变化表明海洋的温水球和亚热带旋转的收缩.
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