应用惩罚三维(3D)混合技术估算海洋叶绿素

M. Onabid, S. Wood
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引用次数: 0

摘要

薄板回归样条(TPRS)被引入,作为在二维(2D)混合过程中消除卫星和现场观测之间差异的一种方法,试图校准海洋叶绿素。这一结果显著提高了利用卫星观测的惩罚模型的预测能力。此外,由于人们认为大多数物理系统都存在于三维(3D)中,因此混合过程已扩展到三维。在本文中,试图通过将惩罚过程扩展到三维(3D)混合来获得更可靠和准确的海洋叶绿素预测。使用积分最小二乘法(ILS)和积分平方导数法(ISD)计算惩罚矩阵。使用积分最小二乘法获得的结果并不令人鼓舞,但使用积分平方导数获得的结果表明,在预测海洋叶绿素方面有了合理的改进,尤其是在验证数据被卫星数据集的可用数据包围的情况下,该过程在计算上显得昂贵,并且结果在一般规模上与其他方法相匹配。在这两种情况下,当使用这两种技术计算惩罚矩阵时,在三维混合中执行惩罚过程的程序已经建立好,并且在必要时可以用于任何类似的三维问题。
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Estimating Ocean Chlorophyll Using the Penalized Three Dimensional (3D) Blending Technique
The Thin Plate Regression Spline (TPRS) was introduced as a means of smoothing off the differences between the satellite and in-situ observations during the two dimensional (2D) blending process in an attempt to calibrate ocean chlorophyll. The result was a remarkable improvement on the predictive capabilities of the penalized model making use of the satellite observation. In addition, the blending process has been extended to three dimensions (3D) since it is believed that most physical systems exist in the three dimensions (3D). In this article, an attempt to obtain more reliable and accurate predictions of ocean chlorophyll by extending the penalization process to three dimensional (3D) blending is presented. Penalty matrices were computed using the integrated least squares (ILS) and integrated squared derivative (ISD). Results obtained using the integrated least squares were not encouraging, but those obtained using the integrated squared derivative showed a reasonable improvement in predicting ocean chlorophyll especially where the validation datum was surrounded by available data from the satellite data set, however, the process appeared computationally expensive and the results matched the other methods on a general scale. In both case, the procedure for implementing the penalization process in three dimensional blending when penalty matrices were calculated using the two techniques has been well established and can be used in any similar three dimensional problem when it becomes necessary.
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