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This climate is characterized by relatively high temperatures and evenly distributed precipitation throughout the year. This climate type is found on the eastern sides of the continents between 20° and 35° N and S latitude. In summer, these regions are largely under the influence of moist, maritime airflow from the western side of the subtropical anticyclonic cells over low-latitude ocean waters. Temperatures are high and can lead to warm, oppressive nights. Summers are usually somewhat wetter than winters, with much of the rainfall coming from convectional thunderstorm activity; tropical cyclones also enhance warm-season rainfall in some regions. The coldest month is usually quite mild, although frosts are not uncommon, and winter precipitation is derived primarily from frontal cyclones along the polar front.
The Köppen Climate Classification subtype for this climate is "Cfa". (Humid Subtropical Climate).
The average temperature for the year in Kobe is 61.0°F (16.1°C). The warmest month, on average, is August with an average temperature of 82.0°F (27.8°C). The coolest month on average is January, with an average temperature of 42.0°F (5.6°C).
The highest recorded temperature in Kobe is 101.0°F (38.3°C), which was recorded in August. The lowest recorded temperature in Kobe is 19.0°F (-7.2°C), which was recorded in February.
There are an average of 168.0 days of precipitation, with the most precipitation occurring in March with 17.0 days and the least precipitation occurring in November with 11.0 days.
In terms of liquid precipitation, there are an average of 157.0 days of rain, with the most rain occurring in March with 16.0 days of rain, and the least rain occurring in January with 10.0 days of rain.