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Climate of Virginia : ウィキペディア英語版
Climate of Virginia

The climate of Virginia, a state on the east coast of the United States, is considered mild compared to other areas of the United States. Most of Virginia east of the Blue Ridge Mountains,the southern part of the Shenandoah Valley, and the Roanoke Valley, has a humid subtropical climate (Köppen climate classification ''Cfa''). In the mountainous areas west of the Blue Ridge, the climate becomes humid continental (Köppen ''Dfa'') and
maritime temperate (Köppen ''Cfb'').〔(【引用サイトリンク】title=World Map of Köppen−Geiger Climate Classification ) 〕 Severe weather, in the form of tornadoes, tropical cyclones, and winter storms, impacts the state on a regular basis. Central Virginia received significant snowfall of 20 inches in December of 2009.
==Climate zones==

Many variations occur because of the state's significant relief. Elevations in Virginia vary from sea level to Mount Rogers at 5,729 ft (1,746 m) above sea level, with major gradations occurring at the edges of the Atlantic Ocean, the end of the Piedmont, and the Blue Ridge and Allegheny chains of the Appalachian Mountains. The moderating influence of the ocean from the east, powered by the Gulf Stream, also creates the potential for hurricanes near the mouth of Chesapeake Bay. Cold air masses arrive over the mountains, especially in winter, which can lead to significant snowfalls when coastal storms known as noreasters move up the Atlantic coast. Much of central and southern Virginia however has not had over one foot of snow in a single storm since the Blizzard of February 5, 2010.
The interaction of these elements with the state's topography create micro-climates in the Shenandoah Valley, the mountainous southwest, and the coastal plains that are slightly but noticeably distinct from each other.〔(【引用サイトリンク】 publisher = Charles A. Grymes )

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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