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

The climate of Pennsylvania is diverse due to the multitude of geographic features found within the state. Straddling two major climate zones, the southeastern corner of Pennsylvania has the warmest climate. Greater Philadelphia lies at the southernmost tip of the Humid continental climate zone, with some characteristics of the Humid subtropical climate that lies in Delaware and Maryland to the south. Moving west toward the mountainous interior of the state, the climate becomes markedly colder, the number of cloudy days increases,〔The Pennsylvania State Climatologist. (Annual Average Number of Cloudy Days In Pennsylvania. ) Retrieved on 2008-01-28.〕 and winter snowfall amounts are greater.
==Precipitation==
Western areas of the state, particularly cities near Lake Erie, can receive over of snowfall annually, and the entire state receives an average of of rainfall every year. Floods are more common in March and April than other months of the year.〔The Pennsylvania State Climatologist. (Climate of Pennsylvania. ) Retrieved on 2008-01-28.〕

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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