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Reconstructing the Past Wind Stresses over the Tropical Pacific Ocean from 1875 to 1947

机译:重建1875至1947年热带太平洋上的过去风应力

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An important step in understanding the climate system is simulating and studying the past climate variability, using oceanic models, atmospheric models, or both. Toward this goal, long-term wind stress data, as the forcing of oceanic or climate models, are often required. In this study, the possibility of reconstructing the past winds of the tropical Pacific Ocean using historical sea surface temperature (SST) and sea level pressure (SLP) datasets was explored. Four statistical models, based on principal component (PC) regression and singular vector decomposition (SVD), were developed for reconstructing monthly pseudo wind stress over the tropical Pacific for the period 1875-1947. The high-frequency noise was removed from the raw data prior to the reconstruction. These models are SST-based PC regression (model 1), SLP-based PC regression (model 2), SST-based SVD (model 3), and SLP-based SVD (model 4). The results show that reconstructed wind stresses from all models can account for more than one-half of the total variances. In general, the SLP is better than SST as a predictor and the SVD method is superior to the PC regression. Forced by these reconstructed wind stresses, an oceanic general circulation model can simulate realistic interannual variability of the tropical Pacific SST. However, the wind stress reconstructed by SST-based models leads to better simulation skill in comparison with that from SLP-based models. Last, a long-term wind stress dataset was constructed for the period from 1875 to 1947 by the SST-based SVD model, which provides a useful tool for studying the past climate variability over the tropical Pacific, especially for El Nino-Southern Oscillation.
机译:理解气候系统的重要一步是使用海洋模型和/或大气模型来模拟和研究过去的气候变异性。为了实现这一目标,通常需要长期的风应力数据,作为强迫海洋或气候模式的数据。在这项研究中,探索了使用历史海面温度(SST)和海平面压力(SLP)数据集重建热带太平洋过去风的可能性。建立了四个基于主成分(PC)回归和奇异矢量分解(SVD)的统计模型,用于重建1875年至1947年期间热带太平洋的月度伪风应力。在重建之前,已从原始数据中去除了高频噪声。这些模型是基于SST的PC回归(模型1),基于SLP的PC回归(模型2),基于SST的SVD(模型3)和基于SLP的SVD(模型4)。结果表明,来自所有模型的重构风应力可以占总方差的一半以上。通常,SLP优于SST作为预测因子,而SVD方法优于PC回归。在这些重构的风应力的作用下,海洋总环流模型可以模拟热带太平洋海表温度的现实年际变化。然而,与基于SLP的模型相比,基于SST的模型重建的风应力导致更好的仿真技巧。最后,通过基于SST的SVD模型构建了1875年至1947年的长期风应力数据集,该数据集为研究热带太平洋过去的气候变化,特别是厄尔尼诺-南方涛动提供了有用的工具。

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