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A new method for deriving ocean surface specific humidity and air temperature: an artificial neural network approach

机译:一种推导海洋表面比湿度和气温的新方法:人工神经网络方法

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A new methodology for deriving monthly averages of surface specific humidity (Q_a) and air temperature (T_a) is described. Two main aspects characterize the new approach. First, remotely sensed parameters, total precipitable water (W), and sea surface temperature (SST) are used to derive Q_a and T_a. Second. artificial neural networks (ANN) are employed to find transfer functions relating the input (W, SST) and output (Q_a and T_a) parameters. Input data consist of nearly six years (January 1988-November 1993) of monthly averages of total precipitable water from Special Sensor Microwave/lmager data and sea surface temperature analysis from the National Centers for Environmental Prediction. Surface marine observations of Q_a and T_a are used to develop and evaluate the new methodology. The performance of the algorithm is measured with surface marine observations not used in the development phase. Higher seasonally dependent discrepancies between Q_a and T_a derived from the new method and in sim data are observed in regions such as the Kuroshio and Gulf Stream currents. After removal of systematic biases. the new method indicates that the combination of W and SST as input parameters and the ANN algorithm provides an interesting alternative for deriving monthly averaged surface parameters. The global mean bias in Q_a is 0.010 +- 0.23 g kg~(-1) over most oceanic areas, whereas root-mean-square (rms) differences are 0.77+- 0.39 g kg~(-1). Likewise. the global mean bias and rms in T_a are on the order of -7.3 X 10~(-5) +- 0.27 deg C and 0.72 +- 0.38 deg C, respectively.
机译:描述了一种用于得出月表平均湿度(Q_a)和气温(T_a)的月平均值的新方法。新方法具有两个主要方面。首先,使用遥感参数,总可沉淀水(W)和海面温度(SST)来得出Q_a和T_a。第二。人工神经网络(ANN)用于查找与输入(W,SST)和输出(Q_a和T_a)参数有关的传递函数。输入数据包含来自特殊传感器微波/成像仪数据的近六年(1988年1月至1993年11月)的月平均总降水量以及来自国家环境预测中心的海面温度分析。使用Q_a和T_a的表面海洋观测资料来开发和评估新方法。该算法的性能是用开发阶段未使用的水面海洋观测值来衡量的。从新方法得出的Q_a和T_a之间的季节性相关差异较大,并且在sim数据中,在黑潮和墨西哥湾流等地区也观察到了这种差异。消除系统偏差之后。新方法表明,将W和SST作为输入参数以及ANN算法的组合为导出月平均表面参数提供了有趣的替代方法。在大多数海洋地区,Q_a的总体平均偏差为0.010±0.23 g kg〜(-1),而均方根差(rms)差异为0.77±0.39 g kg〜(-1)。同样。 T_a中的整体平均偏差和均方根分别为-7.3 X 10〜(-5)+-0.27摄氏度和0.72 +-0.38摄氏度。

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