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Performance of downscaled regional climate simulations using a variable-resolution regional climate model : Tasmania as a test case

机译:使用可变分辨率区域气候模型进行的按比例缩小的区域气候模拟的性能:塔斯马尼亚岛作为测试案例

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摘要

In this study we develop methods for dynamically downscaling output from six general circulation models (GCMs) for two emissions scenarios using a variable-resolution atmospheric climate model. The use of multiple GCMs and emissions scenarios gives an estimate of model range in projected changes to the mean climate across the region. By modeling the atmosphere at a very fine scale, the simulations capture processes that are important to regional weather and climate at length scales that are subgrid scale for the host GCM. We find that with a multistaged process of increased resolution and the application of bias adjustment methods, the ability of the simulation to reproduce observed conditions improves, with greater than 95% of the spatial variance explained for temperature and about 90% for rainfall. Furthermore, downscaling leads to a significant improvement for the temporal distribution of variables commonly used in applied analyses, reproducing seasonal variability in line with observations. This seasonal signal is not evident in the GCMs. This multistaged approach allows progressive improvement in the skill of the simulations in order to resolve key processes over the region with quantifiable improvements in the correlations with observations.
机译:在这项研究中,我们开发了使用可变分辨率大气气候模型动态缩小两种排放情景下六个通用循环模型(GCM)的输出的方法。使用多个GCM和排放情景可以估算该区域平均气候预计变化的模型范围。通过以非常精细的比例对大气建模,模拟可以捕获对于区域气候和气候非常重要的过程,该过程对于宿主GCM而言是亚网格尺度。我们发现,随着分辨率提高的多阶段过程以及偏差调整方法的应用,模拟重现观察到的条件的能力得到了改善,其中超过95%的空间变化被解释为温度,而大约90%的降水被解释为空间。此外,缩小比例还可以显着改善应用分析中常用变量的时间分布,从而再现与观测一致的季节性变化。在GCM中,这种季节性信号并不明显。这种多阶段的方法可以逐步提高模拟技巧,以便解决该地区的关键过程,并提高与观测值的相关性。

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