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Real-Time Observations of the February 2010 Chile and March 2011 Japan Tsunamis: Recorded in Honolulu by the Pacific Islands Ocean Observing System

机译:2010年2月智利和2011年3月日本海啸的实时观测:太平洋岛屿海洋观测系统在火奴鲁鲁记录

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摘要

Continuous monitoring by the Pacific Islands Ocean Observing System (PacIOOS) provided a unique opportunity to study the effects of two tsunamis on the coastal and estuarine waters of Hawai'i. By the time the 2010 Chile and 2011 Japan tsunamis reached the waters of southern O'ahu, they had lost much of their power (both were < 1 m high in Honolulu Harbor). Nevertheless, their effects on the surrounding waters were profound, with increases observed in near-bed current velocities, mixing in estuarine waters, salinity, turbidity, chlorophyll, and pathogenic bacteria such as Vibrio spp. In addition to these increases, we observed small decreases in nitrate and dissolved oxygen concentrations offshore, including a dampening of the normal diel cycle in dissolved oxygen. Some of the effects penetrated canals as far as 1 km inshore and could be observed up to 0.5 km offshore. Data from the PacIOOS sensors and our sampling show that altered and potentially degraded water quality can persist longer than the physical threat from surge. Shortly after both tsunamis, the "all clear" signal was given and people resumed recreational activities in coastal waters before our data indicated recovery of healthy water quality conditions. Following such events, monitoring should be expanded and continued in order to accurately characterize water quality and evaluate potential public health risks.
机译:太平洋岛屿海洋观测系统(PacIOOS)的持续监测为研究两个海啸对夏威夷沿海和河口水域的影响提供了独特的机会。到2010年智利和2011年日本海啸到达瓦胡岛南部的水域时,它们已经失去了很多动力(在檀香山港口,两者的高度都<1 m)。然而,它们对周围水域的影响是深远的,在近海床流速,河口水域混合,盐度,浊度,叶绿素和病原菌(如弧菌)中观察到的增加。除了这些增加之外,我们还观察到了海上硝酸盐和溶解氧浓度的小幅下降,包括正常溶解氧中Diel循环的减弱。一些影响渗透到了近岸1公里处的运河中,并且可以观察到近岸0.5公里处的情况。来自PacIOOS传感器和我们采样的数据表明,改变的水质和潜在的退化水质比浪涌造成的物理威胁持续时间更长。两次海啸发生后不久,在我们的数据表明健康水质状况恢复之前,人们发出了“全部清除”信号,人们在沿海水域恢复了娱乐活动。发生此类事件后,应扩大并继续进行监测,以准确表征水质特征并评估潜在的公共健康风险。

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  • 来源
    《Oceanography》 |2014年第2期|186-200|共15页
  • 作者单位

    Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, USA;

    Department of Oceanography, University of Hawai'i at Manoa, Honolulu, HI, USA;

    Department of Oceanoeraphv, University of Hawai'i at Manoa, Honolulu, HI, USA;

    Department of Oceanography, University of Hawai'i at Manoa, Honolulu, HI,USA;

    Mechanical and Aerospace Engineering, University of California, San Diego, La Jolla, CA, USA;

    Department of Oceanography, University of Hawai'i at Manoa, Honolulu, HI,USA;

    Department of Oceanography, University of Hawai'i at Manoa, Honolulu, HI, USA;

    Department of Environmental Sciences, University of Virginia, Charlottesville, VA, USA;

    Department of Oceanography, University of Hawai'i at Manoa, Honolulu, HI, USA;

    Department of Oceanography, University of Hawai'i at Manoa, Honolulu, HI, USA;

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