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The major differences between the various proxy reconstructions relate to the magnitude of past cool excursions, principally during the twelfth to fourteenth, seventeenth and nineteenth centuries." but a series of events before the known climatic minima has often been referenced.
In the 13th century, pack ice began advancing southwards in the North Atlantic, as did glaciers in Greenland.
(2012) The first River Thames frost fair was in 1607 and the last in 1814; changes to the bridges and the addition of the Thames Embankment affected the river flow and depth, greatly diminishing the possibility of further freezes.
Freezing of the Golden Horn and the southern section of the Bosphorus took place in 1622.
Climatologists and historians working with local records no longer expect to agree on either the start or end dates of the period, which varied according to local conditions.
The IPCC Fourth Assessment Report (AR4) of 2007 discusses more recent research, giving particular attention to the Medieval Warm Period.