A Continental Climate is characterized by significant temperature variations between seasons, typically found in the interior regions of continents. This climate features hot summers and cold winters, with limited precipitation throughout the year. The temperature range can be quite extreme, often exceeding 30°C (86°F) in summer and dropping below -30°C (-22°F) in winter. Regions with a continental climate, such as parts of the United States and Europe, experience distinct seasonal changes. The lack of large bodies of water nearby contributes to these temperature fluctuations, as water moderates temperatures. Vegetation in these areas often includes deciduous and coniferous forests, adapted to the varying conditions.