Spatio-temporal distribution of internal waves in the Andaman Sea based on satellite remote sensing

Liying Zhou, Jingsong Yang, Juan Wang, Shuangyan He, Zhiguo He, Antony K. Liu, M. Hsu
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引用次数: 9

Abstract

In this paper, More than 1000 satellite images including Terra/Aqua MODIS, Sentinel-1A SAR images from 2013 to 2015 were analyzed to obtain spatio-temporal distribution of internal waves in the Andaman Sea. The statistical results demonstrate that the internal wave have been observed mostly in four areas by the remote sensing: northern Sumatra Island, western Malay Peninsula, northeast of the Nicole Islands and eastern Andaman Islands in Andaman Sea. Internal waves in the middle and the gradually changing bathymetric gradients areas of the Andaman Sea have been unobserved by the remote sensing. Internal waves can be observed in Andaman Sea all through the year, most in hot season (February to April), next rainy season( May to October). And a minimum number of internal waves are observed in rainy(June to August), however, this may be caused by the small amount of clear MODIS images in rainy in the Andaman Sea, it need to further proof by using more remote sensing images.
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基于卫星遥感的安达曼海内波时空分布
本文利用2013 - 2015年Terra/Aqua MODIS、Sentinel-1A SAR等1000多幅卫星影像进行分析,获得安达曼海内波的时空分布特征。统计结果表明,遥感观测到的内波主要集中在四个区域:苏门答腊岛北部、马来半岛西部、尼科尔群岛东北部和安达曼海安达曼群岛东部。安达曼海中部和逐渐变化的水深梯度区域的内波一直是遥感观测不到的。安达曼海全年都可以观察到内波,大多数在炎热季节(2月至4月),其次是雨季(5月至10月)。而在多雨期(6 - 8月)观测到的内波数最少,但这可能是由于安达曼海多雨期MODIS清晰影像较少造成的,需要使用更多的遥感影像进一步证明。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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