Estimation of Sea Surface Salinity Concentration from Landsat 8 OLI Data in The Strait of Madura, Indonesia

Muhsi Muhsi, B. M. Sukojo, M. Taufik, P. Aji, Lalu Muhamad Jaelani
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引用次数: 1

Abstract

Remote sensing technique to estimate the sea surface salinity has been widely implemented in the seas of various regions. The interface between them was developed using a regression equation like the algorithm in previous research. However, the use of this algorithm for waters in Indonesia, especially in Madura Strait, still requires some adjustment since it is related to the characteristics of different areas in which the algorithm was developed. The development of an applicable local algorithm was performed by finding the best coefficient value in estimating sea surface salinity by considering the value of its lowest NMAE (Normalized Mean Absolute Error). By using salinity and in-situ Rrs(l) (Reflectance of remote sensing) data, we found that the coefficient for the slope was -0.0092, and the intercept was 1.4903. The developed algorithm produces higher accuracy than the existing algorithm, with an NMAE of 0.51%. This NMAE value is smaller than previous research, so this new model can be used to estimate sea surface salinity, particularly in Indonesian sea waters.
利用Landsat 8 OLI资料估算印尼马杜拉海峡海面盐度浓度
海表盐度遥感估算技术已广泛应用于各区域海域。它们之间的接口是使用与之前研究中的算法类似的回归方程来开发的。然而,该算法在印度尼西亚水域,特别是马杜拉海峡的使用,仍然需要一些调整,因为这与算法开发的不同地区的特点有关。通过考虑海水表面盐度的最低NMAE(归一化平均绝对误差)值,找到估算海水表面盐度的最佳系数值,开发了一种适用的局部算法。利用盐度和原位遥感反射率(Rrs(l))数据,我们发现坡度系数为-0.0092,截距为1.4903。该算法比现有算法具有更高的准确率,NMAE为0.51%。这个NMAE值比以前的研究要小,所以这个新模型可以用来估计海面盐度,特别是在印度尼西亚的海水中。
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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来源期刊
CiteScore
0.10
自引率
0.00%
发文量
11
审稿时长
15 weeks
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