在海洋中输入和损失的空间合
Curtis Deutsch1, Jorge L Sarmiento, Daniel M Sigman
1Program on Climate Change, School of Oceanography, University of Washington, Seattle, Washington 98195, USA. cdeutsch@ocean.washington.edu
Nature
|January 12, 2007
概括
海洋固对于海洋生产力至关重要,它可以取代丢失的. 这项研究显示,固定率在太平洋是最高的,与缺乏的水域有关.
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
- 循环动力学 循环动力学
背景情况:
- 固定对于海洋生物的生产力至关重要,它补充了通过脱而失去的.
- 由于具有很高的时间和空间可变性,对海洋固的直接测量具有挑战性.
- 了解影响固定的因素 (如铁,N:P比率,温度) 受到测量不确定性的限制.
研究的目的:
- 通过分析它们对表面酸盐和酸盐度的间接影响,确定全球海洋固率.
- 研究全球海洋中固化,脱化和营养物质固化学之间的关系.
- 阐明海洋固的驱动因素,特别是在营养有限的地区.
主要方法:
- 利用海洋循环模型从观察到的酸盐和酸盐度推断固率.
- 分析了不同海洋区域中固速率的空间分布.
- 与脱率和大气铁沉积等因素相关的固速率.
主要成果:
- 固定率在太平洋是最高的.
- 在水柱脱率高的地区观察到高的固定率.
- 大气中铁沉积量较低的地区显示固率较高.
结论:
- 海洋固与脱区中缺水的形成密切相关.
- 固化在稳定海洋中固定的数量方面起着至关重要的作用.
- 这些发现支持了固化作为海洋营养平衡的关键调节器的假设.
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