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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >A machine learning approach to estimate surface ocean pCO(2) from satellite measurements
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A machine learning approach to estimate surface ocean pCO(2) from satellite measurements

机译:从卫星测量估算表面海洋PCO(2)的机器学习方法

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Surface seawater partial pressure of CO2 (pCO(2)) is a critical parameter in the quantification of air-sea CO2 flux, which further plays an important role in quantifying the global carbon budget and understanding ocean acidification. Yet, the remote estimation of pCO(2) in coastal waters (under influences of multiple processes) has been difficult due to complex relationships between environmental variables and surface pCO(2). To date there is no unified model to remotely estimate surface pCO(2) in oceanic regions that are dominated by different oceanic processes. In our study area, the Gulf of Mexico (GOM), this challenge is addressed through the evaluation of different approaches, including multi-linear regression (MLR), multi-nonlinear regression (MNR), principle component regression (PCR), decision tree, supporting vector machines (SVMs), multilayer perceptron neural network (MPNN), and random forest based regression ensemble (RFRE). After modeling, validation, and extensive tests using independent cruise datasets, the RFRE model proved to be the best approach. The RFRE model was trained using data comprised of extensive pCO(2) datasets (collected over 16 years by many groups) and MODIS (Moderate Resolution Imaging Spectroradiometer) estimated sea surface temperature (SST), sea surface salinity (SSS), surface chlorophyll concentration (Chl), and diffuse attenuation of downwelling irradiance (Kd). This RFRE-basedpCO(2) model allows for the estimation of surface pCO(2) from satellites with a spatial resolution of 1 km. It showed an overall performance of a root mean square difference (RMSD) of 9.1 mu atm, with a coefficient of determination (R-2) of 0.95, a mean bias (MB) of - 0.03 mu atm, a mean ratio (MR) of 1.00, an unbiased percentage difference (UPD) of 0.07%, and a mean ratio difference (MRD) of 0.12% for pCO(2) ranging between 145 and 550 mu atm. The model, with its original parameterization, has been tested with independent datasets collected over the entir
机译:CO2的表面海水部分压力(PCO(2))是航空海洋二氧化碳通量量化的关键参数,这进一步在量化全球碳预算和了解海洋酸化方面发挥着重要作用。然而,由于环境变量和表面PCO(2)之间的复杂关系,PCO(2)在沿海水域(在多个过程的影响下)难以估计。迄今为止,没有统一的模型在以不同的海洋过程中主导的海洋区域中远程估计表面PCO(2)。在我们的研究领域,墨西哥湾(GOM),通过评估不同方法,包括多线性回归(MLR),多非线性回归(MNR),原理成分回归(PCR),决策树,解决方案,支持向量机(SVM),多层Perceptron神经网络(MPNN)和随机林基数的回归合奏(RFRE)。使用独立巡航数据集建模,验证和广泛的测试后,RFRE模型被证明是最好的方法。 RFRE模型使用广泛的PCO(2)数据集(由多个组收集超过16年)和MODIS(适度分辨率成像光谱仪),估计海表面温度(SST),海表面盐度(SSS),表面叶绿素浓度(CHL),并扩散贫困辐照度(KD)。该RFRE-PSPCO(2)模型允许使用1公里的空间分辨率估计来自卫星的表面PCO(2)。它显示出9.1μmat的根均值(RMSD)的整体性能,测定系数(R-2)为0.95,平均偏差(MB)为-0.03μmat,平均值(MR) 1.00,无偏见的百分比差(UPD)为0.07%,平均比率差(MRD)为145至550亩的PCO(2)之间的0.12%。具有原始参数化的模型已通过在Otil上收集的独立数据集进行测试

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