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A sampling technique to compare climate simulations with sparse satellite observations: Performance evaluation of a CMIP5 EC-Earth forced dynamical wave climate ensemble with altimeter observations

机译:一种采样技术,与稀疏卫星观测的气候仿真比较:CMIP5 EC地球强制动态波气候合奏性能评价,高度计观测

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Global climate simulations do not capture the exact time history, making it difficult to directly compare them with observations. In this study we simulate the sampling of altimeter observations from a seven-member wind and wave climate ensemble. This allows us to assess the skill of the climate simulations, relative to satellite observations instead of the typical approach which uses reanalysis or hindcast datasets as reference. Out of the sampling methods tested, we find that a systematic sampling technique performs the best. We then apply systematic sampling to wind fields from EC-Earth and wave fields generated using the wave model (WAM) to replicate the changing sampling of the satellite observations. Next we then quantitatively assess the climate simulations and find that the probability density functions (PDFs) computed from the EC-Earth wind speed samples match the shape of the PDFs obtained from the altimeter observations. EC-Earth consistently under-estimates the wind speed with respect to the altimeter observations. Contrary to the wind speed under-estimation, the wave simulations overestimate wave heights especially in the extra-tropics. The wind speed seasonality in EC-Earth is larger than the seasonality evaluated from altimeter wind observations while the opposite is true for the wave height seasonality; suggesting the wave physical parameterizations can be improved. We find that the wave height inter-annual variability of the modeled data is considerably less than the inter-annual variability evaluated from the altimeter observations; suggesting long-term climate variability is not well captured. Overall the wave ensemble captures the important features of the global wave climate. The methodology can be adapted to other climate simulations and observational datasets.
机译:全球气候模拟不会捕获确切的时间历史,使得难以将它们与观察结果进行比较。在这项研究中,我们模拟了来自七个成员风和波浪气候合奏的高度计观测的采样。这使我们可以评估气候模拟的技能,相对于卫星观察而不是使用再分析或HindCast数据集作为参考的典型方法。在测试的采样方法中,我们发现系统采样技术表现最佳。然后,我们将系统采样从使用波模型(WAM)生成的EC-BARM和WAVE字段应用到风场以复制卫星观测的改变采样。接下来,我们可以定量地评估气候仿真,并发现从EC地球风速样本计算的概率密度函数(PDF)与从高度计观察中获得的PDF的形状匹配。 EC地球一致地估计到高度计观察的风速。与风速估计相反,波模拟尤其是额外热带的波浪高度。 EC-NARG的风速季节性大于从高度计风测量评估的季节性,而相反的波浪高度季节性是正确的;建议可以提高波物理参数化。我们发现建模数据的波浪高度年度可变性相当小于从高度计观察中评估的年间变异性;建议长期气候变异性并不充分捕获。总体而言,波乐队捕获了全球波浪气候的重要特征。该方法可以适应其他气候模拟和观察数据集。

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