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导致东海/日本海异常大的聚球藻(Cochlodinium polykrikoides)水华形成的物理过程。

Physical processes leading to the development of an anomalously large Cochlodinium polykrikoides bloom in the East sea/Japan sea.

机构信息

Department of Oceanography, Pusan National University, Busan 609-735, Republic of Korea.

Department of Oceanography, Pusan National University, Busan 609-735, Republic of Korea.

出版信息

Harmful Algae. 2016 May;55:250-258. doi: 10.1016/j.hal.2016.03.019. Epub 2016 Apr 15.

Abstract

An anomalously large Harmful Algal Bloom (HAB) was observed in the southwest coast of the East/Japan Sea (hereafter the East Sea) during the summer of 2013. During this time period, the presence of Cochlodinium polykrikoides (C. polykrikoides) was detected by the Geostationary Ocean Color Imager (GOCI) and validated by in-situ observations. GOCI observations have been available since 2011, thus allowingto examine various stages of the physical condition of the developing C. polykrikoides bloom, thereby other multi-satellite and buoy measurements obtained between 2011 and 2013. Research results indicate that this HAB is related to four processes: the transport of C. polykrikoides from the south coast of Korea to the HAB area; a relatively high insolation; continuous coastal upwelling; and a favorable Sea Surface Temperature (SST) for C.polykrikoide growth. In examination of the main transport mechanisms, geostrophic current measurements were used to estimate the flow trajectories, showing water from the south coast to the HAB area off the southeast coast of Korea. Result shows that ninety percent of the water from the south coast reached the HAB area in 2013. Furthermore, to examine the insolation mechanism, the Photosynthetically available radiation (PAR) value was derived from the Moderate Resolution Imaging Spectoradiometer (MODIS), showing that PAR values were relatively high in the HAB area during HAB period (47Einmday). Moreover, Upwelling age (UA) was calculated in order to investigate the strength of coastal upwelling events, which were found to support relatively high UA values during the HAB period. The mean UA value during the HAB period was 1.01, higher than those in 2011 and 2012 which were 0.61 and 0.76, respectively. Finally, SST in the HAB area was also analyzed to examine which conditions were most favorable for HAB growth. Therefore, the results of this study suggest that the four mechanisms can explain the relative contributions of the anomalously HAB development observed off the southeast coast of Korea.

摘要

2013 年夏季,在日本海(东海)西南海岸观测到一次异常规模的有害藻华(HAB)。在此期间,通过地球静止轨道海洋成像仪(GOCI)检测到聚生角毛藻(C. polykrikoides)的存在,并通过现场观测得到验证。GOCI 观测自 2011 年开始提供,因此可以检查发展中的聚生角毛藻藻华的各个阶段的物理状况,从而获得 2011 年至 2013 年之间的其他多卫星和浮标测量数据。研究结果表明,此次 HAB 与四个过程有关:聚生角毛藻从韩国南部海岸向 HAB 区域的输送;相对较高的太阳辐射;连续的沿海上升流;以及适合 C.polykrikoide 生长的海面温度(SST)。在检查主要的输送机制时,使用地转流测量来估计流轨迹,显示来自南部海岸的水流向韩国东南海岸外的 HAB 区域。结果表明,2013 年,90%的南部海岸的水到达了 HAB 区域。此外,为了检查太阳辐射机制,从中分辨率成像光谱仪(MODIS)中得出了光合有效辐射(PAR)值,结果表明在 HAB 期间 HAB 区域的 PAR 值相对较高(47Einmday)。此外,为了调查沿海上升流事件的强度,计算了上升流年龄(UA),结果发现上升流年龄在 HAB 期间相对较高。HAB 期间的平均 UA 值为 1.01,高于 2011 年和 2012 年的 0.61 和 0.76。最后,还分析了 HAB 区域的 SST,以检查最有利于 HAB 生长的条件。因此,本研究的结果表明,这四个机制可以解释韩国东南海岸观测到的异常 HAB 发展的相对贡献。

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