对异质半层生物地质化学的物理控制
Mara A Freilich1,2, Lilian A Dove1,3, Katarina Merk1
1Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, RI USA.
概括
海洋流连接表面和深水,影响海洋生物和化学物质. 了解这些动态是改善海洋通风和生物地球化学模型的关键.
科学领域:
- 海洋学 海洋学 海洋学
- 海洋生物地质化学海洋生物地质化学
- 物理海洋学 物理海洋学
背景情况:
- 海洋的表面和内部是通过在次季节时间尺度上运行的三维物理过程相互连接的.
- 埃迪动力学显著地影响了上半半层海洋中的生物化学和生物变异性,正如模型和观测所示.
研究的目的:
- 突出物理过程在塑造地下生物地化学和生物变异性的重要性.
- 强调地下标志差异对海洋通风,生物地球化学功能和微生物群落的影响.
主要方法:
- 利用数值模型和观测数据来研究海洋动态.
- 应用水质框架来描述地下的不一致性和标记物运输.
主要成果:
- 厄迪动力学在上层中层海洋的生物地质化学和生物学中起着至关重要的作用.
- 地下探测器差异影响海洋通风时间表和微生物生态系统.
结论:
- 考虑动态运输过程的水质框架对于理解地下不齐是必不可少的.
- 未来投资于共同的物理和生物测量对于推进半层生物化学研究至关重要.
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