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Observations of climate changes across the last thousand years suggest that it must be so. In the Medieval Warm Period, Greenland had agriculture and the Western Isles of Scotland were prosperous with a much larger population than today—which implies more poleward climate zones and zonal jets at that time. In contrast, ships logs from the Little Ice Age show much greater Atlantic storminess and more equatorward mid latitude depression tracks at that time (depressions generally follow the tracks of the jet streams).
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