甲时期Tethys的数值模拟环球电流环球电流
Bush1
1Atmospheric and Oceanic Sciences Program, Princeton University, Post Office Box CN710, Sayre Hall, Princeton, NJ 08544-0710, USA.
概括
一个强大的向西环球热带电流存在于白时期. 这一发现得到了先进的气候建模的支持,澄清了从1.44亿年前到6.5亿年前的海洋循环模式.
科学领域:
- 古代海洋学 古代海洋学 古代海洋学
- 气候建模气候模型
- 地质历史地质历史
背景情况:
- 纪时期的海洋流是了解过去气候的关键.
- 以前的气候模型很难准确地模拟白时期的海洋循环.
研究的目的:
- 调查白时期环球热带气流的存在和特征.
- 通过先进的建模技术来完善古海洋学重建.
主要方法:
- 使用了一种合大气-海洋气候模型.
- 采用高空间分辨率的网格.
- 纳入了白纪晚期的大陆分布.
主要成果:
- 成功模拟了一个强大的西向环球热带电流.
- 在季风期间观察到当地泰西斯海道表面电流的逆转.
- 证实了环球电流的稳定性,尽管存在区域差异.
结论:
- 在白纪,出现了重要的向西环球热带气流.
- 先进的气候模型可以准确地描绘古代海洋学条件.
- 区域性季风影响了更广泛的环球流中的地方流.
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