概括
在赤道太平洋.
科学领域:
- 海洋学 海洋学 海洋学
- 海洋化学 海洋化学
- 生物海洋学 生物海洋学
背景情况:
- 赤道太平洋是大气中二氧化碳的重要来源.
- 它也被认为是将有机碳出口到深海的关键地区.
研究的目的:
- 为了研究赤道太平洋的化学和生物变异性.
- 确定这种变化的主要驱动因素及其对碳循环的影响.
主要方法:
- 从赤道太平洋 (170°W至95°W) 的化学和生物数据分析.
- 评估偏远风和热带波浪的作用.
主要成果:
- 遥远的风和热带不稳定的波浪是化学和生物变异的主要驱动因素.
- 大多数生物生产依赖于回收的营养素;上游营养素的吸收最小.
- 优光区的高效生物循环导致光合作用过程中的碳出口量很小.
- 每年的排放量:大约0.3千兆的二氧化碳进入大气层,有机颗粒碳进入深海.
- 溶解有机碳的产量大约是颗粒流量的三倍.
结论:
- 厄尔尼诺现象是这个系统年间变化的主要原因.
- 赤道太平洋在全球碳循环中的作用是复杂的,受到物理和生物过程的影响.
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