首页> 外文期刊>Fresenius environmental bulletin >TRANSPORT OF THE NEMOPILEMA NOMURAI IN THE YELLOW SEA AND EAST CHINA SEA REVEALED BY FIELD OBSERVATION, SATELLITE DATA, AND PARTICLE-TRACKING EXPERIMENTS
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TRANSPORT OF THE NEMOPILEMA NOMURAI IN THE YELLOW SEA AND EAST CHINA SEA REVEALED BY FIELD OBSERVATION, SATELLITE DATA, AND PARTICLE-TRACKING EXPERIMENTS

机译:野外观测,卫星数据和颗粒追踪实验揭示了新海藻在黄海和华东海域的运输

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The spatial distribution of the giant jellyfish Nemopilema nomurai and its relation to water masses and circulation in the Yellow Sea and East China Sea were investigated by ship observations, satellite sea surface temperature (SST), and particletracking experiments. Temperature and salinity were examined by hierarchical clustering, and eight main water masses were identified. High abundances of giant jellyfish were observed in Southern Yellow Sea Water and in mixed waters, but few jellyfish were observed in other water masses. Variation in satellite SST was used to characterize the seasonal variation in the water masses. The results indicated that as the winter monsoon weakened, a water mass with SST (>15qC) at the Jiangsu coast in May extended northeastward and eastward until July. Southerly wind was probably an important factor inducing this northeastward circulation. Moreover, transport of jellyfish was verified by backward, forward particle-tracking experiments based on the flow field from a numerical model and an independent ferry data. The water masses with jellyfish traced back to the Jiangsu coast in the month of May. Furthermore, water masses without jellyfish traced back to the mouth of the Changjiang River, and the Taiwan Strait. These results indicate that the high abundance of giant jellyfish observed in July came from the northern East China Sea or southern Yellow Sea coast in May when ephyrae were liberated from polyps there as SST increased from below 15qC to higher values.
机译:通过船舶观测,卫星海面温度(SST)和粒子追踪实验研究了黄海和东海巨型海lyNemopilema nomurai的空间分布及其与水量和环流的关系。通过分层聚类检查温度和盐度,并确定了八个主要水团。在南部黄海水和混合水域中观察到大量的大型水母,而在其他水团中则观察到很少的水母。卫星海表温度的变化用来表征水团的季节性变化。结果表明,随着冬季季风减弱,江苏沿海5月SST(> 15qC)的水团向东北和向东延伸至7月。南风可能是引起这种东北向循环的重要因素。此外,基于数值模型和独立轮渡数据的流场,通过向后,向前的粒子跟踪实验验证了水母的运输。五月的水母水团可追溯到江苏沿海。此外,没有水母的水团可以追溯到长江流域和台湾海峡。这些结果表明,七月份观测到的大量海j来自五月份的东中国海北部或黄海南部沿海地区,当时随着SST从低于15qC升高到更高的值,那里的息肉释放出了e。

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