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Drought frequency projection using regional climate scenarios reconstructed by seasonal artificial neural network model

机译:季节性人工神经网络模型重构的区域气候情景干旱频率预测

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The climate change impacts on drought in the Korean peninsula were projected using Global Climate Model (GCM) output reconstructed regionally by an artificial neural network (ANN) model. The reconstructed model outputs were subsequently used as an input to project drought severity evaluated by Standard Precipitation Index (SPI). The original GCM output corresponds to the CGCM3.1/T63 under the 20C3M reference scenario and the IPCC A1B, A2 and B1 projection scenarios. Because in general GCM shows limitation in capturing typhoon generation occurred at sub-grid scale, the training and validation of the ANN model utilized a precipitation data set with typhoon-generated rainfall eliminated for enhancing the ANN's computational performance. The non-stationarity characteristics of SPI was examined using the Mann-Kendall test. The projection was implemented for the near future period (2011-2040), mid-term (2041-2070) and long-term (2071-2100) future periods. The results indicated mitigated drought severity under all scenarios in terms of frequency, magnitude and drought spells even for the mildest B1 scenario. The SDF (severity-duration-frequency) curves illustrate the common patterns of alleviated drought severity for most future scenarios and elongated drought duration. The reconstructed GCM projection recovers the underestimated precipitation and provided more realistic drought projection even though there would be still uncertainties of spatial and temporal variability.
机译:使用人工神经网络(ANN)模型对全球气候模型(GCM)产出进行了区域重构,从而预测了朝鲜半岛的气候变化影响。随后将重建的模型输出用作通过标准降水指数(SPI)评估的项目干旱严重程度的输入。在20C3M参考方案和IPCC A1B,A2和B1投影方案下,原始GCM输出对应于CGCM3.1 / T63。因为一般而言,GCM显示捕获在台风规模下发生的台风的局限性,所以ANN模型的训练和验证使用了降水数据集,其中消除了台风产生的降雨,从而增强了ANN的计算性能。使用Mann-Kendall检验检查了SPI的非平稳性。该预测是针对不久的将来时期(2011-2040),中期(2041-2070)和长期(2071-2100)时期执行的。结果表明,即使在最温和的B1情景下,在频率,强度和干旱情况下,所有情景下的干旱严重程度均得到缓解。 SDF(严重性-持续时间-频率)曲线说明了在大多数未来情况下和延长的干旱持续时间下减轻干旱严重程度的常见模式。重建的GCM预测可以恢复被低估的降水量,并提供更现实的干旱预测,即使时空变化仍存在不确定性。

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