The Little Ice Age, which lasted from the 14th to the mid-19th century, is believed to have begun around the early 1300s. Several factors contributed to its onset, including a decline in solar activity, increased volcanic activity, and changes in ocean circulation patterns. These factors led to cooler temperatures, particularly in the Northern Hemisphere, resulting in harsher winters and shorter growing seasons. The period was marked by significant climatic shifts that affected agriculture, population dynamics, and societal structures in various regions.
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