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Oceanic Forcing of Coral Reefs

机译:珊瑚礁的海洋强迫

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摘要

Although the oceans play a fundamental role in shaping the distribution and function of coral reefs worldwide, a modern understanding of the complex interactions between ocean and reef processes is still only emerging. These dynamics are especially challenging owing to both the broad range of spatial scales (less than a meter to hundreds of kilometers) and the complex physical and biological feedbacks involved. Here, we review recent advances in our understanding of these processes, ranging from the small-scale mechanics of flow around coral communities and their influence on nutrient exchange to larger, reef-scale patterns of wave-and tide-driven circulation and their effects on reef water quality and perceived rates of metabolism. We also examine regional-scale drivers of reefs such as coastal upwelling, internal waves, and extreme disturbances such as cyclones. Our goal is to show how a wide range of ocean-driven processes ultimately shape the growth and metabolism of
机译:尽管海洋在塑造全世界珊瑚礁的分布和功能方面起着根本性的作用,但对海洋与礁石过程之间复杂的相互作用的现代理解仍在不断出现。由于空间尺度的范围很广(不到一米到几百公里),而且涉及到复杂的物理和生物反馈,因此这些动力尤其具有挑战性。在这里,我们回顾了对这些过程的理解的最新进展,从珊瑚群落周围的小规模流动机制及其对养分交换的影响到更大的,礁石规模的波浪和潮汐驱动的环流模式及其对海洋的影响。珊瑚礁水质和新陈代谢速率。我们还研究了珊瑚礁的区域尺度驱动因素,例如沿海上升流,内部波浪和飓风等极端干扰。我们的目标是展示各种各样的海洋驱动过程最终如何塑造海藻的生长和新陈代谢。

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