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Verification of mesoscale numerical weather forecasts in mountainous terrain for application to avalanche prediction

机译:验证山区中尺度数值天气预报在雪崩预报中的应用

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Two high-resolution, real-time, numerical weather prediction (NWP) models are verified against case study observations to quantify their accuracy and skill in the mountainous terrain of western Canada. These models, run daily at the University of British Columbia (UBC), are the Mesoscale Compressible Community (MC2) Model and the University of Wisconsin Nonhydrostatic Modeling System (NMS). The main motivations of this work are: 1) to extend the lead time of avalanche forecasts by using NWP-projected meteorological variables as input to statistical avalanche threat models; and 2) to create another tool to help avalanche forecasters in their daily decision-making process. Observation data from the Whistler/Blackcomb ski area in the British Columbia ( BC) Coast Mountains and from Kootenay Pass in the Columbia Mountains of southeast BC are used to verify the forecasts. The two models are run with grid spacings of 3.3 km ( MC2) and 10 km ( NMS) over Whistler/Blackcomb, and with 2, 10 ( MC2), and 30 km ( NMS) over Kootenay Pass. The quality of the forecasts is measured using standard statistical methods for those variables that are important for avalanche forecasting. It is found that the raw model output has biases that can be easily removed using Kalman filter predictor postprocessing. The resulting automatically corrected forecasts have quite small absolute errors in temperature (0.7degreesC). It is also found that the coarser-resolution NMS model produces comparable results to the finer-resolution MC2 model for precipitation at Kootenay Pass. These objective forecast errors are of the same order of magnitude as the meteorological observation (sampling/representativeness) errors in the snowy, windy mountainous terrain, resulting in forecasts that have value in extending the range of avalanche forecasts for locations such as Kootenay Pass, as discussed in a recent study by Roeger et al. [References: 20]
机译:针对案例研究观察,验证了两个高分辨率的实时数字天气预报(NWP)模型,以量化其在加拿大西部山区的准确性和技能。这些模型每天在不列颠哥伦比亚大学(UBC)运行,分别是中尺度可压缩社区(MC2)模型和威斯康星大学非静液压模型系统(NMS)。这项工作的主要动机是:1)通过使用NWP预测的气象变量作为统计雪崩威胁模型的输入来延长雪崩预报的提前期。 2)创建另一个工具来帮助雪崩预报员进行日常决策。来自不列颠哥伦比亚省(BC)海岸山脉的惠斯勒/黑梳山滑雪场和不列颠哥伦比亚省东南部的哥伦比亚山脉的Kootenay Pass的观测数据被用于验证预测。这两个模型在惠斯勒/黑梳上方的网格间距分别为3.3 km(MC2)和10 km(NMS),在Kootenay Pass上方的网格间距为2,10(MC2)和30 km(NMS)。对于那些对于雪崩预测很重要的变量,使用标准统计方法来测量预测的质量。发现原始模型输出具有偏差,可以使用卡尔曼滤波器预测变量后处理轻松消除偏差。结果自动校正后的预报的温度绝对误差很小(0.7摄氏度)。还发现,对于Kootenay Pass降水,较粗分辨率的NMS模型产生的结果与较细分辨率的MC2模型相当。这些客观的预测误差与在多雪,多风的山区地形上的气象观测(采样/代表性)误差具有相同的数量级,从而导致预测具有扩大Kootenay Pass等地点雪崩预测范围的价值。在Roeger等人的最新研究中讨论过。 [参考:20]

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