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Unusual phytoplankton blooms in the southwestern Bay of Bengal: a comparative study

机译:孟加拉湾西南湾的不寻常的Phytoplankton绽放:比较研究

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Two unusual phytoplankton bloom events were identified in the southwestern Bay of Bengal from MODIS-derived chlorophyll-a concentration data collected between 2003 and 2015. The occurrence of the unusual phytoplankton bloom in December 2005 (called Bloom 1 in this study) has been reported in the literature to be triggered by multiple forcings, including strong cyclonic eddy, frequent typhoons, and strong wind-induced mixing. Interestingly, the other unusual phytoplankton bloom (called Bloom 2 in this study) was identified in almost the same location in December 2013. Further, it is the strongest bloom during our study period with large area of high Chl-a > 1.0 mg/m~3 and shared some similar features with Bloom 1, such as wide coverage and long duration. At the same time, there were also frequent typhoons and a cyclonic eddy. The possible causes of Bloom 2 were examined using time series of multi-satellite datasets, including sea surface height anomalies (SSHA), sea surface temperature (SST), together with Argo profile data. We found that the cyclonic eddy might be not yet the dominant factor for Bloom 2 as the eddy was much weaker than that of Bloom 1. Specially, SST in December 2013 was lowest among all the December from 2003 to 2015. That is, the stratification is weakest. Therefore, the weak stratification can be broken easily by mixing induced by typhoons and cyclonic eddies and finally result in the strong bloom. This comparative studies could provide us some insight in understanding the role of eddies and tropical cyclones in phytoplankton dynamics in the Bay of Bengal.
机译:从2003年至2015年间收集的Modis衍生的叶绿素 - 植物的植物西南湾的两个不寻常的浮游植物绽放事件均鉴定在2003年至2015年间收集的浓度数据。在2005年12月(本研究中称为Bloom 1)的异常浮游植物盛开的发生由多种强制引发的文献,包括强潮流,频繁的台风和强风诱导的混合。有趣的是,其他不寻常的Phytoplankton Bloom(这项研究中称为Bloom 2)在2013年12月几乎相同的位置确定了。此外,在我们的研究期间,它是大面积的高CHL-A> 1.0mg / m的研究期间最强壮的绽放〜3并与盛开1共享一些类似的功能,如覆盖范围宽,持续时间很长。与此同时,还有频繁的台风和旋风涡流。使用时间序列进行多卫星数据集,包括海面高度异常(SSHA),海面温度(SST),与ARGO简介数据一起检查绽放2的可能原因。我们发现,随着涡流比布鲁姆1.特别弱得多的气旋涡流可能尚未布卢姆2的主导因素,SST在2013年12月是在所有的最低月从2003年到2015年。也就是说,分层是最弱的。因此,通过由台风和旋风漩涡诱导的混合可以容易地破裂弱分层,最后导致强烈绽放。这种比较研究可以为我们提供一些洞察力,了解埃迪迪斯和热带气旋在孟加拉湾的浮游植物动力学中的作用。

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