利用代用模型预测气候变化下不断变化的地貌上的风暴潮

Mohammad Ahmadi Gharehtoragh, David R. Johnson
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引用次数: 0

摘要

在计算预算有限的情况下,管理沿岸洪水风险的规划人员需要权衡利弊。模拟多个时段或场景会限制在每个地貌上运行多少次风暴模拟。在本分析中,我们提出了一种深度学习模型,用于预测风暴潮,它不仅是风暴参数的函数,也是地貌特征和边界条件(如海平面)的函数。该模型是根据高级环流(ADCIRC)对路易斯安那州沿海 2020 年基线和 2030 年至 2070 年十年期两种形态和气候情景下的水动力模拟得出的浪涌峰值进行训练的。在每个地貌 90 次风暴和 94,013 个地理空间位置上,对一个地貌进行交叉验证,得出的均方根误差为 0.086 米,最大均方根误差为 0.050 米。对模型预测和 ADCIRC 模拟的年超标概率(AEP)估计值进行了双侧 Kolmogorov-Smirnov 检验,仅有 1.1% 的时间拒绝了预测值和 ADCIRC AEP 值来自同一分布的零假设。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Using surrogate modeling to predict storm surge on evolving landscapes under climate change

Using surrogate modeling to predict storm surge on evolving landscapes under climate change
Planners managing coastal flood risk under a constrained computational budget face a tradeoff. Simulating many time periods or scenarios limits how many storm simulations can be run on each landscape. In this analysis, we present a deep learning model to predict storm surge as a function of storm parameters but also landscape features and boundary conditions (e.g., sea level). It is trained on peak surge elevations from Advanced Circulation (ADCIRC) hydrodynamic simulations of coastal Louisiana in a 2020 baseline and decadal periods from 2030 to 2070 under two morphological and climate scenarios. Leave-one-landscape-out cross-validation yielded a 0.086-m RMSE and 0.050-m MAE over 90 storms per landscape and 94,013 geospatial locations. A two-sided Kolmogorov-Smirnov test comparing annual exceedance probability (AEP) estimates from the model predictions to ADCIRC simulations rejected the null hypothesis that the predicted and ADCIRC AEP values were drawn from the same distribution only 1.1% of the time.
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