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首页> 外文期刊>Journal of Hydrology >Comparing statistically downscaled simulations of Indian monsoon at different spatial resolutions
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Comparing statistically downscaled simulations of Indian monsoon at different spatial resolutions

机译:比较不同空间分辨率下印度季风的统计缩减模拟

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Impacts of climate change are typically assessed with fairly coarse resolution General Circulation Models (GCMs), which are unable to resolve local scale features that are critical to precipitation variability. GCM simulations must be downscaled to finer resolutions, through statistical or dynamic modelling for further use in hydrologic analysis. In this study, we use a linear regression based statistical downscaling method for obtaining monthly Indian Summer Monsoon Rainfall (ISMR) projections at multiple spatial resolutions, viz., 0.05 degrees, 0.25 degrees and 0.50 degrees, and compare them. We use 19 GCMs of Coupled Model Intercomparison Project Phase 5 (CMIP5) suite and combine them with multi model averaging and Bayesian model averaging. We find spatially non-uniform changes in projections at all resolutions for both combinations of projections. Our results show that the changes in the mean for future time periods (2020s, 2050s, and 2080s) at different resolutions, viz., 0.05, 0.25 and 0.5, obtained with both Multi-Model Average (MMA) and Bayesian Multi-Model Average (BMA) are comparable. We also find that the model uncertainty decreases with projection times into the future for all resolutions. We compute Signal to Noise Ratio (SNR), which represents the climate change signal in simulations with respect to the noise arising from multi-model uncertainty. This appears to be almost similar at different resolutions. The present study highlight that, a mere increase in resolution by a way of computationally more expensive statistical downscaling does not necessarily contribute towards improving the signal strength. Denser data networks and finer resolution GCMs may be essential for producing usable rainfall and hydrologic information at finer resolutions in the context of statistical downscaling. (C) 2014 Elsevier B.V. All rights reserved.
机译:通常使用相当粗略的分辨率通用循环模型(GCM)评估气候变化的影响,该模型无法解析对降水变化至关重要的局部尺度特征。必须通过统计或动态建模将GCM模拟缩减为更高分辨率,以进一步用于水文分析。在这项研究中,我们使用基于线性回归的统计缩减方法来获取多个空间分辨率(即0.05度,0.25度和0.50度)的月度印度夏季风降雨(ISMR)投影,并进行比较。我们使用19个GCM耦合模型比较项目阶段5(CMIP5)套件,并将它们与多模型平均和贝叶斯模型平均相结合。我们发现两种投影组合在所有分辨率下投影的空间不均匀变化。我们的结果表明,使用多模型平均值(MMA)和贝叶斯多模型平均值获得的未来时间段(2020s,2050s和2080s)在不同分辨率下的平均值变化(即0.05、0.25和0.5) (BMA)是可比的。我们还发现,对于所有分辨率,模型的不确定性都会随着未来的投影时间而降低。我们计算信噪比(SNR),该信噪比表示针对多模型不确定性产生的噪声的模拟气候变化信号。在不同的分辨率下,这似乎几乎是相似的。本研究强调,通过计算上更昂贵的统计缩减规模而仅增加分辨率并不一定有助于提高信号强度。在统计规模缩小的背景下,Denser数据网络和更高分辨率的GCM可能对于以更高分辨率生成可用的降雨和水文信息至关重要。 (C)2014 Elsevier B.V.保留所有权利。

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