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Uplift of a coral island in the andaman sea due to the 2004 sumatra earthquake measured using remote sensing reflectance of water

机译:由于2004年苏门答腊地震,在Andaman海上隆起的隆起,使用遥感反射水测量

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摘要

The 2004 Sumatra earthquake, together with the tsunami that followed, caused massive destruction in many coastal areas of the Indian Ocean. Uplift and subsidence of land near to the epicenter of the earthquake in the Andaman Sea have been reported. In this paper, we report observations of the uplift in high resolution SPOT-5 satellite images in a coral island near to the Andaman Islands. The depth of the submerged reefs can be measured using water reflectance models commonly employed in the ocean color research community. The uplift magnitude is estimated by the difference in water depth measured in the pre- and post-earthquake images, taking into account the difference in tide levels. The uplift is found to be 1.6 m with an uncertainty of about 0.3 m.
机译:2004年苏门答腊地震,以及随后的海啸,在印度洋的许多沿海地区引起了大规模的破坏。据报道,Andaman海域地震震中的隆起和土地附近的沉降和沉降。在本文中,我们在靠近安达曼岛附近的珊瑚岛的高分辨率点卫星图像中报告了对高分辨率的隆起的观察。浸没珊瑚礁的深度可以使用海洋颜色研究界通常使用的水反射模型来测量。考虑到潮汐水平的差异,升高幅度估计升高幅度估计。发现隆起是1.6米,不确定度约为0.3米。

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