葛瑞克摄制区大湾水域盐度值及海温分布分析

CI-TECH Pub Date : 2021-11-20 DOI:10.33005/ci-tech.v2i2.47
M. Yusuf, Hendrata Wibisana, Siti Zainab
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引用次数: 0

摘要

拔uk Lamong的水域位于泗水的北海海岸,直接毗邻Gresik摄政。拉朗湾作为一个国际战略港口而闻名。在打陆拉密的沿海水域,一些河流流入拉密湾。这些活动会导致淡水和海水之间的相互作用。这种相互作用影响了直流直下水域的盐度扩散模式和海面温度。盐度和海水表面温度是造成海洋腐蚀的最大因素之一,这将破坏海洋周围建筑物的结构。预计在本研究中,有关Teluk Lamong水域的信息将用于土木工程领域的数据信息或数据库利用,其中包括港口维护和沿海建筑规划。在此背景下,有必要利用Landsat 8卫星图像监测2016年和2020年Lamong湾盐度值和海面温度的变化。对该算法进行建模得到的结果是,该算法用于处理图像盐度的模型为公式Power中的波段Band_4,模型算法为y = 25.437x-0.046,决定度值R²= 0.5825。而采用算法模型的功率方程中的海面温度y = 302.14x0.0029,确定值R²= 0.4182。t检验和验证检验的分析结果都是合格的。图像数据分析结果显示,盐度分布范围为27.33 (ppm) ~ 29.9 (ppm),海面温度范围为303.95 ~ 304.39开尔文。
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ANALYSIS OF THE DISTRIBUTION OF SALINITY VALUE AND SEA SURFACE TEMPERATURE IN LAMONG BAY WATERS, GRESIK REGENCY
The waters of Teluk Lamong are located on the north sea coast of Surabaya, which is directly adjacent to the Gresik Regency. Lamong Bay is famous as a strategic port place on an International scale. Along the coastal waters of Teluk Lamong, some rivers flow in Lamong Bay. These activities can lead to interaction between fresh water and seawater. This interaction affects the pattern of salinity spread and sea surface temperature in the waters of Teluk Lamong. Salinity and Sea Surface Temperature is one of the biggest factors causing corrosion in the sea that will damage the structure of buildings around the sea. It is expected that in this research as information about the waters of Teluk Lamong for data information or database utilization in the field of civil engineering, among others, port maintenance and coastal building planning. Based on this background, research is needed to monitor the spread of salinity values and sea surface temperatures in Lamong Bay using Landsat 8 satellite imagery for the years 2016 and 2020. The result of modeling the algorithm obtained, the model of the algorithm used to process the salinity of the image is the wavelength Band_4 in the Equation Power with the model algorithm y = 25.437x-0.046, and the degree of determination value R² = 0.5825. While sea surface temperature in power equation with algorithm model y = 302.14x0.0029 and determination value R² = 0.4182. The results of an analysis of the T-test and validation test can be qualified. The results of the analysis of imagery data showed salinity distribution ranged from 27.33 (ppm) to 29.9 (ppm), while sea surface temperatures ranged from 303.95 Kelvin to 304.39 Kelvin.
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