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Simulating transport pathways of pelagic Sargassum from the Equatorial Atlantic into the Caribbean Sea

机译:模拟中上纲海藻从赤道大西洋到加勒比海的运输途径

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Since 2011, beach inundation of massive amounts of pelagic Sargassum algae has occurred around the Caribbean nations and islands. Previous studies have applied satellite ocean color to determine the origins of this phenomenon. These techniques, combined with complementary approaches, suggest that, rather than blooms originating in the Caribbean, they arrive from the Equatorial Atlantic. However, oceanographic context for these occurrences remains limited. Here, we present results from synthetic particle tracking experiments that characterize the interannual and seasonal dynamics of ocean currents and winds likely to influence the transport of Sargassum from the Equatorial Atlantic into the Caribbean Sea. Our findings suggest that Sargassum present in the western Equatorial Atlantic (west of longitude 50 degrees W) has a high probability of entering the Caribbean Sea within a year's time. Transport routes include the Guiana Current, North Brazil Current Rings, and the North Equatorial Current north of the North Brazil Current Retroflection. The amount of Sargassum following each route varies seasonally. This has important implications for the amount of time it takes Sargassum to reach the Caribbean Sea. By weighting particle transport predictions with Sargassum concentrations at release sites in the western Equatorial Atlantic, our simulations explain close to 90% of the annual variation in observed Sargassum abundance entering the Caribbean Sea. Additionally, results from our numerical experiments are in good agreement with observations of variability in the timing of Sargassum movement from the Equatorial Atlantic to the Caribbean, and observations of the spatial extent of Sargassum occurrence throughout the Caribbean. However, this work also highlights some areas of uncertainty that should be examined, in particular the effect of "windage" and other surface transport processes on the movement of Sargassum. Our results provide a useful launching point to predict Sargassum beaching events along the Caribbean islands well in advance of their occurrence and, more generally, to understand the movement ecology of a floating ecosystem that is essential habitat to numerous marine species.
机译:自2011年以来,在加勒比海国家和岛屿周围发生了大量的浮游性浮游藻海滩的淹没。先前的研究已经应用卫星海洋颜色来确定这种现象的起源。这些技术与互补方法相结合,表明它们来自赤道大西洋,而不是起源于加勒比海的花朵。但是,这些事件的海洋背景仍然有限。在这里,我们介绍了合成粒子跟踪实验的结果,这些实验表征了可能影响Sargassum从赤道大西洋到加勒比海的运输的洋流和风的年际和季节动态。我们的发现表明,存在于赤道西大西洋(西经50度以西)的Sargassum在一年时间内极有可能进入加勒比海。运输路线包括圭亚那洋流,北巴西洋流环和北巴西洋流逆转以北的北赤道洋流。沿着每条路线的Sargassum的数量随季节变化。这对于Sargassum到达加勒比海所需的时间量具有重要意义。通过用赤道西大西洋释放点的Sargassum浓度对颗粒运输预测进行加权,我们的模拟解释了观测到的进入加勒比海的Sargassum丰度每年变化的近90%。此外,我们的数值实验结果与从赤道大西洋到加勒比海的马尾藻运动时间变化的观察结果以及整个加勒比海中马尾藻发生的空间范围的观察结果非常吻合。但是,这项工作还强调了应检查的某些不确定性领域,特别是“风阻”和其他表面运输过程对Sargussum运动的影响。我们的结果提供了一个有用的出发点,可以在加勒比岛屿上发生Sar​​gassum海滩事件之前就对其进行预测,并且更广泛地了解一个漂浮生态系统的运动生态系统,该生态系统是众多海洋物种的重要栖息地。

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