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Climate

The climate of New England varies greatly across its 500 miles (800 km) span from northern Maine to southern Connecticut:

Maine, New Hampshire, Vermont, and western Massachusetts have a humid continental climate (Dfb in Köppen climate classification). In this region the winters are long and cold, and heavy snow is common (most locations receive 60–120 inches (150–300 cm) of snow annually in this region). The summer's months are moderately warm, though summer is rather short and rainfall is spread through the year.

In central and eastern Massachusetts, northern Rhode Island, and northern Connecticut, the same humid continental prevails (Dfa), though summers are warm to hot, winters are shorter, and there is less snowfall (especially in the coastal areas where it is often warmer).

Southern and coastal Connecticut is the broad transition zone from the cold continental climates of the north to the milder subtropical climates to the south. The frost free season is greater than 180 days across far southern/coastal Connecticut, coastal Rhode Island, and the islands (Nantucket and Martha's Vineyard). Winters also tend to be much sunnier in southern Connecticut and southern Rhode Island compared to the rest of New England.