小冰河时代和20世纪太平洋的深度降温
1Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. ggebbie@whoi.edu.
概括
海洋深度仍在从小冰河时代开始降温, 表面水则变暖. 这种深海热量损失抵消了近期上海热量增长的四分之一,
科学领域:
- 古代海洋学
- 海洋学
- 气候科学
背景情况:
- 从中世纪温暖时期到现代变暖之前的小冰河时代,全球变冷发生了.
- 海洋的长期记忆意味着历史上的表面异常与深海温度调整有关.
研究的目的:
- 调查正在进行的深海温度调整与历史气候变化.
- 为了比较太平洋深度和大西洋温度趋势与海洋表面的变化.
主要方法:
- 使用海洋模型与古海洋学和现代水文学数据相结合.
- 从HMS挑战者探险 (1870年代) 的温度数据与当代测量数据进行比较.
主要成果:
- 太平洋的深度显示了对小冰河时代降温的持续调整.
- 海洋表面和大西洋深度的温度反映了当前的人为变暖.
- 自公元1750年以来,深海的热量损失约占上海热量的25%.
结论:
- 深海循环模式继续反映过去的气候状态,特别是太平洋的小冰河时代.
- 观察到的温度趋势凸显了海洋层对气候变化的复杂和滞后反应.
- 了解这些深海调整对于准确的气候变化预测至关重要.
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