对台风的海洋生物地质化学反应的审查
Fajin Chen1, Qibin Lao2, Xuan Lu2
1College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China; School of Chemistry and Environment, Guangdong Ocean University, Zhanjiang 524088, China; Key Laboratory for Coastal Ocean Variation and Disaster Prediction, Guangdong Ocean University, Zhanjiang 524088, China; Key Laboratory of Climate, Resources and Environment in Continental Shelf Sea and Deep Sea of Department of Education of Guangdong Province, Guangdong Ocean University, Zhanjiang 524088, China.
Marine pollution bulletin
|August 16, 2023
概括
台风显著改变了海洋的生物地质化学和动态. 虽然它们可以通过营养上游增加生产力,但有机物分解占主导地位,消耗氧气.
科学领域:
- 海洋科学 海洋科学
- 海洋学 海洋学 海洋学
- 生物地质化学生物地质化学
背景情况:
- 台风是极端天气事件,对海洋生态系统产生深远影响.
- 它们影响海洋动力学,生物地球化学和气候调节.
- 台风导致营养物质上升,可能导致浮游植物的繁荣,增加海洋的碳吸收.
研究的目的:
- 提供台风对海洋动态和生物地球化学的影响的系统概述.
- 详细阐述台风引起的有机物分解的特征和机制.
- 突出研究台风后的合海洋学和生物地球化学过程的重要性.
主要方法:
- 审查现有文献和综合发现.
- 对海洋学变化的卫星遥感数据的分析.
- 关于海洋生物地球化学过程的实地观测的汇编.
主要成果:
- 台风导致海洋物理和化学性质发生重大变化.
- 植物浮游生物的开花可能是由于营养丰富而发生的,作为碳汇.
- 有机物分解是一个主要的过程,导致水柱中的氧气耗尽,充当碳源.
结论:
- 了解台风驱动的海洋学和生物地球化学合是至关重要的.
- 有机物分解在台风后的碳循环中起着关键作用.
- 需要进一步的研究才能充分阐明这些复杂的相互作用及其对气候的影响.
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