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sebastiaan1973

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Posts posted by sebastiaan1973

  1. https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2019GL085592

    The impact of the Arctic stratospheric polar vortex on persistent weather regimes over North
    America is so far underexplored. Here we show the relationship between four wintertime North American
    weather regimes and the stratospheric vortex strength using reanalysis data. We find that the strength of
    the vortex significantly affects the behavior of the regimes. While a regime associated with Greenland
    blocking is strongly favored following weak vortex events, it is not the primary regime associated with a
    widespread, elevated risk of extreme cold in North America. Instead, we find that the regime most strongly
    associated with widespread extremely cold weather does not show a strong dependency on the strength of
    the lower stratospheric zonal mean zonal winds. We also suggest that stratospheric vortex morphology
    may be particularly important for cold air outbreaks during this regime

  2. 16 hours ago, RUNNAWAYICEBERG said:

    http://www.nature.com/articles/s41558-019-0551-4.epdf?author_access_token=lev7cCLvJaqZgqEL2fkrCtRgN0jAjWel9jnR3ZoTv0OkPw7OWz-ctumf1Sllaa-sNqBW8kixcwl-ojSoyKUmUfvHbXmZ3llXRmZN-HO_pmKRWEHLwCuZqZkuv4bolog-ehQV4R4jg8i93P7ntZX4_w%3D%3D

    Observations show that reduced regional sea-ice cover is coincident with cold mid-latitude winters on interannual timescales.

    However, it remains unclear whether these observed links are causal, and model experiments suggest that they might not be.

    Here we apply two independent approaches to infer causality from observations and climate models and to reconcile these

    sources of data. Models capture the observed correlations between reduced sea ice and cold mid-latitude winters, but only

    when reduced sea ice coincides with anomalous heat transfer from the atmosphere to the ocean, implying that the atmosphere

    is driving the loss. Causal inference from the physics-based approach is corroborated by a lead–lag analysis, showing that

    circulation-driven temperature anomalies precede, but do not follow, reduced sea ice. Furthermore, no mid-latitude cooling is

    found in modelling experiments with imposed future sea-ice loss. Our results show robust support for anomalous atmospheric

    circulation simultaneously driving cold mid-latitude winters and mild Arctic conditions, and reduced sea ice having a minimal

    influence on severe mid-latitude winters.

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