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Multi-model seasonal forecast of Arctic sea-ice: forecast uncertainty at pan-Arctic and regional scales

机译:北极海冰的多模式季节性预报:整个北极和区域尺度的预报不确定性

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摘要

Dynamical model forecasts in the Sea Ice Outlook (SIO) of September Arctic sea-ice extent over the last decade have shown lower skill than that found in both idealized model experiments and hindcasts of previous decades. Additionally, it is unclear how different model physics, initial conditions or forecast post-processing (bias correction) techniques contribute to SIO forecast uncertainty. In this work, we have produced a seasonal forecast of 2015 Arctic summer sea ice using SIO dynamical models initialized with identical sea-ice thickness in the central Arctic. Our goals are to calculate the relative contribution of model uncertainty and irreducible error growth to forecast uncertainty and assess the importance of post-processing, and to contrast pan-Arctic forecast uncertainty with regional forecast uncertainty. We find that prior to forecast post-processing, model uncertainty is the main contributor to forecast uncertainty, whereas after forecast post-processing forecast uncertainty is reduced overall, model uncertainty is reduced by an order of magnitude, and irreducible error growth becomes the main contributor to forecast uncertainty. While all models generally agree in their post-processed forecasts of September sea-ice volume and extent, this is not the case for sea-ice concentration. Additionally, forecast uncertainty of sea-ice thickness grows at a much higher rate along Arctic coastlines relative to the central Arctic ocean. Potential ways of offering spatial forecast information based on the timescale over which the forecast signal beats the noise are also explored.
机译:过去十年来,九月北极海冰范围的海冰展望(SIO)中的动力学模型预测显示,其技巧比理想化模型实验和后几十年的后兆预报中的技巧要低。另外,还不清楚不同的模型物理,初始条件或预测后处理(偏差校正)技术如何导致SIO预测不确定性。在这项工作中,我们使用初始化为北极中部相同海冰厚度的SIO动力学模型,得出了2015年北极夏季海冰的季节预报。我们的目标是计算模型不确定性和不可减少的误差增长对预测不确定性和评估后处理的重要性的相对贡献,并将泛北极预测不确定性与区域预测不确定性进行对比。我们发现,在进行预测后处理之前,模型不确定性是导致预测不确定性的主要因素,而在进行预测后处理后,预测不确定性总体上降低了,模型的不确定性减少了一个数量级,不可减少的误差增长成为了主要因素。预测不确定性。尽管所有模型在其对9月海冰数量和范围的后处理预测中普遍表示同意,但海冰浓度并非如此。此外,相对于北冰洋中部,沿北极海岸线海冰厚度的预测不确定性将以更高的速率增长。还探讨了基于预测信号击败噪声的时间尺度提供空间预测信息的潜在方法。

著录项

  • 来源
    《Climate dynamics》 |2017年第4期|1399-1410|共12页
  • 作者单位

    Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA;

    Catholic Univ Louvain, Georges Lemaitre Ctr Earth & Climate Res, Louvain La Neuve, Belgium;

    Meteo France, UMR 3589, Ctr Natl Rech Meteorol, Toulouse, France;

    NASA, Goddard Space Flight Ctr, Global Modeling & Assimilat Off, Greenbelt, MD USA;

    Barcelona Supercomp Ctr, Barcelona, Spain;

    Catholic Univ Louvain, Georges Lemaitre Ctr Earth & Climate Res, Louvain La Neuve, Belgium|Barcelona Supercomp Ctr, Barcelona, Spain;

    Naval Res Lab, Hancock Cty, MS USA;

    NOAA NWS NCEP Climate Predict Ctr, College Pk, MD USA;

    Univ Washington, Appl Phys Lab, Polar Sci Ctr, Seattle, WA 98105 USA;

    Meteo France, UMR 3589, Ctr Natl Rech Meteorol, Toulouse, France;

    Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA;

    NASA, Goddard Space Flight Ctr, Global Modeling & Assimilat Off, Greenbelt, MD USA|Sci Syst & Applicat Inc, Greenbelt, MD USA;

    Naval Res Lab, Hancock Cty, MS USA;

    Univ Washington, Joint Inst Study Atmosphere & Ocean, Seattle, WA 98195 USA|NOAA, Pacific Marine Environm Lab, 7600 Sand Point Way Ne, Seattle, WA 98115 USA;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Sea ice; Seasonal forecast; Arctic; Forecast uncertainty;

    机译:海冰;季节预报;北极;预报不确定性;

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