哨兵2A经验测深法在马尼若湖水深测量中的应用

Wendi Arifin, Febriandi Febriandi, M. Hanif, Triyatno Triyatno, E. S. Mokhtar, E. Mutia
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引用次数: 0

摘要

Maninjau湖是由火山活动形成的湖泊。许多人类活动发生在集水区,但也发生在已开发的水域。本研究旨在绘制Maninjau湖的水深图,并评估野外样本分布对图像转换质量结果的影响。使用的数据是Sentinel 2A卫星图像,点测结果。分析方法采用归一化差分水指数算法、太阳闪烁法、经验测深法和线性回归。研究结果发现,以单元格为代表的物体深度的记录过程中,分布的变化转化为离散。由此变换所得的水的深度是指在野外调查中测量的样品。水域的最大深度在107米范围内。浅水区主要分布在马尼若湖的北部,是马尼若湖的外缘。南部地区形成一个深盆地。该样本以经验水深图的形式分布,实测结果与转换之间的关系回归值为0.769,说明考虑了调查样本的总量和分布对转换结果质量的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Application of Empirical Bathymetry Method on Sentinel 2A for Measuring Water Depth of Maninjau Lake
Lake Maninjau is a lake formed by volcanic activity. Many human activities occur on the catchment area, but also in exploited waters. This study aims to mapping the depth of the waters in the Lake Maninjau and assess the effect of field sample distribution on the quality results of the image transformation. The data used are satellite imagery Sentinel 2A, results of point survey. The analysis technique uses the normalized difference water index algorithm, sun glint, empirical bathymetry method and linear regression. The result of the research which is has found that variations of distribution into the dispersion of the recording process of the depth of the object represented by cell. The depth of the water from the results of this transformation refers to the measurement sample in the field survey. The maximum depth of the waters is in the range of 107m. Shallow waters are predominantly distributed in the northern region which is the out late of Lake Maninjau. The southern area forms a deep basin. The distribution of this sample is in the form of an empirical bathymetry map and the relationship between the results of field measurements and the transformation with a regression value of 0.769, this indicates the consideration of total and distribution of survey sample is influence on quality of the results of the transformation.
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