在地势坐标中没有水平的重力
1Department of Atmopsheric and Oceanic Sciences, University of California, Los Angeles, CA 90095.
概括
这项研究表明,在地球物理模型中,使用地势坐标可以消除地球重力旋转力的水平组成部分. 这为完善大气和海洋循环模型提供了一个框架.
科学领域:
- 地质物理学 地质物理学
- 大气科学 大气科学
- 海洋学 海洋学 海洋学
背景情况:
- 对于大规模循环的传统地质物理模型往往忽略了地球重力旋转力的水平组成部分.
- 这种做法最近面临挑战,需要重新评估基础假设.
研究的目的:
- 研究在地物理模型中忽视地球重力旋转力的水平组成部分的后果.
- 为了证明坐标转换为地势坐标对这种力的影响.
主要方法:
- 将坐标转换为地势坐标应用于地球物理建模框架.
- 分析的重点是地球的重力旋转力在这个新的坐标系内的行为.
主要成果:
- 坐标转换为地势坐标有效地消除了地球重力旋转力的水平组成部分.
- 这一发现验证了在历史上遗漏了这种力成分的模型的使用.
结论:
- 地势坐标框架为当前的建模实践提供了理论上的理由.
- 这一框架可以作为未来更精细的大气和海洋循环的地球物理模型的基础.
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