Seasonal variability in Northern Hemisphere atmospheric circulation during the Medieval Climate Anomaly and the Little Ice Age
Autor: | Hans Linderson, Christophe Sturm, Brandi W. Newton, Dan Hammarlund, Natalie A. St. Amour, Jesper Sjolte, Joscelyn N.-L. Bailey, Thomas W. D. Edwards, Anders Nilsson |
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Rok vydání: | 2017 |
Předmět: |
010506 paleontology
Archeology Global and Planetary Change Meteorological reanalysis 010504 meteorology & atmospheric sciences Atmospheric circulation Anomaly (natural sciences) Northern Hemisphere Geology Circumpolar star 01 natural sciences Geography Arctic oscillation 13. Climate action North Atlantic oscillation Climatology Paleoclimatology Ecology Evolution Behavior and Systematics 0105 earth and related environmental sciences |
Zdroj: | Quaternary Science Reviews. 165:102-110 |
ISSN: | 0277-3791 |
DOI: | 10.1016/j.quascirev.2017.04.018 |
Popis: | Here we report new reconstructions of winter temperature and summer moisture during the past millennium in southeastern Sweden, based on stable-isotope data from a composite tree-ring sequence, that further enhances our knowledge and understanding of seasonal climate variability in the Northern Hemisphere over the past millennium. Key features of these new climate proxy records include evidence for distinctive fluctuations in winter temperature in SE Sweden, superimposed upon the general pattern of cooling between the so-called Medieval Climate Anomaly (MCA) of the early millennium and the Little Ice Age (LIA) of the late millennium, as well as evidence for sustained summer wetness during the MCA, followed by drier and less variable conditions during the LIA. We also explore these new records within a circumpolar spatial context by employing self-organizing map analysis of meteorological reanalysis data to identify potential modern analogues of mid-tropospheric synoptic circulation types in the Northern Hemisphere extratropics that can reconcile varying seasonal climate states during the MCA and LIA in SE Sweden with less variable conditions in southwestern Canada, as portrayed by paleoclimate records developed in the same manner in an earlier study. |
Databáze: | OpenAIRE |
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