用等高线模拟进行北极海冰边缘的概率预报

Hannah M. Director, A. Raftery, C. Bitz
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引用次数: 7

摘要

在北极,海冰或冰冻的海水每年都会结冰和融化。由于气候变化导致海冰数量减少,因此需要提前数周到数月准确预测海冰的位置。典型的海冰预报是用集合模式,即基于物理的海冰及其周围海洋和大气的确定性模式来进行的。混合轮廓线预测是一种预测海冰的方法,它对集合的输出进行后处理,并将其与近年来观测到的海冰模式加权。与未经调整的动态集合预报和其他统计参考预报相比,这些预报的校准效果更好。为了产生这些预测,引入了一种新的统计技术,直接模拟海冰边缘轮廓,即海冰覆盖区域周围的边界。因此,后处理中的大部分计算工作都可以放在海冰边缘轮廓上,由于海冰边缘轮廓在海洋规划中的作用,这一点尤为重要。使用欧洲中期天气预报中心集合,评估了混合等高线预报和参考方法对2008-2016年每月海冰预报的预估时间从0.5-6.5个月不等。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Probabilistic forecasting of the Arctic sea ice edge with contour modeling
Sea ice, or frozen ocean water, annually freezes and melts in the Arctic. The need for accurate forecasts of where sea ice will be located weeks to months in advance has increased as the amount of sea ice reduces due to climate change. Typical sea ice forecasts are made with ensemble models, physics-based deterministic models of sea ice and the surrounding ocean and atmosphere. This paper introduces Mixture Contour Forecasting, a method to forecast sea ice that post-processes output from ensembles and weights them with observed sea ice patterns in recent years. These forecasts are better calibrated than unadjusted dynamic ensemble forecasts and other statistical reference forecasts. To produce these forecasts, a novel statistical technique is introduced that directly models the sea ice edge contour, the boundary around the region that is ice-covered. Most of the computational effort in post-processing can therefore be placed on the sea ice edge contour, which is of particular importance due to its role in maritime planning. Mixture Contour Forecasting and reference methods are evaluated for monthly sea ice forecasts for 2008-2016 at lead times ranging from 0.5-6.5 months using the European Centre for Medium-Range Weather Forecasts ensemble.
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