previous modifications within the local weather. Within the case of the Norse, the medieval heat period was associated with the Norse age of exploration and arctic colonization, and the later colder durations led to the decline of those colonies ( Patterson, W.P., et al., 2007 ). Climate change in the latest past may be detected by corresponding changes in settlement and agricultural patterns. Notable intervals of local weather change in recorded historical past embrace the medieval heat period and the little ice age.
The environmental method uses paleoclimatic proof to indicate that actions within the
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