在冰河时代的厄尔尼诺样式热带太平洋海面温度温度
Athanasios Koutavas1, Jean Lynch-Stieglitz, Thomas M Marchitto
1Lamont-Doherty Earth Observatory and Department of Earth and Environmental Sciences, Columbia University, Palisades, NY 10964, USA. athan@ldeo.columbia.edu
概括
太平洋的海面温度影响了全球气候超过3万年. 这些温度的变化,特别是在最后的冰川最大期,揭示了大气模式和海洋条件的变化.
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:
- 东赤道太平洋的冷舌区的海面温度 (SST) 显著影响全球大气循环.
- 了解该地区过去的气候变化对于预测未来气候动态至关重要.
研究的目的:
- 重建和分析从最后的冰川最大期 (LGM) 到现在的赤道太平洋东部冷舌气候变化.
- 研究SST变化与全球大气循环模式之间的关系.
主要方法:
- 从加拉帕戈斯群岛附近的海底沉积物中重建SST记录,使用foraminifera中的/比.
- 对过去3万年气候变化的分析,将SST数据与前cession诱导的季节性相关联.
主要成果:
- 在过去的3万年里,冷舌的SST表现出连贯的变化,与前cession诱导的季节性.
- 最后的冰川最大降温 (1.2°C) 表示热带温度梯度放松,大气循环减弱 (哈德利和沃克),热带融合区向南移动,以及类似厄尔尼诺的模式.
- 中期Holocene冷却表明类似于拉尼娜的模式,具有增强的SST梯度和增强的贸易风.
结论:
- 热带太平洋的SST梯度在全球气候变化中发挥着重要作用.
- 过去的气候重建提供了关于大气循环对热带太平洋SST变化的敏感性的见解.
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