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The Köppen climate classification is the most widely used climate classification scheme. [2] It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, [3] [4] with several later modifications by Köppen, notably in 1918 and 1936.
According to the Köppen climate classification system, the most popular climate classification system in the world, only South Florida is considered tropical. Orlando has the same climate
The Gulf and South Atlantic states have a humid subtropical climate with mostly mild winters and hot, humid summers. Most of the Florida peninsula including Tampa and Jacksonville, along with other coastal cities like Houston, New Orleans, Savannah, Charleston and Wilmington all have average summer highs from near 90 to the lower 90s F, and lows generally from 70 to 75 °F (21 to 24 °C ...
Santa Monica and its environs may be 10 to 15 °F (6 to 8 °C) cooler than areas only 5 miles (8.0 km) further inland. Under the Köppen climate classification, the airport has a semi-arid climate due to its modest winter rainfall and mild mean temperatures. For monthly statistics, see Climate of Los Angeles#Temperatures and seasons
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Trewartha climate types of Oregon. According to the Köppen climate classification, most of Western Oregon has a warm-summer Mediterranean climate (or Csb type), which features warm, dry summers, and wet winters with frequent overcast and cloudy skies. Eastern Oregon falls into the cold semi-arid climate (or BSk type), which features drier weather.
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Modern climate classification methods can be broadly divided into genetic methods, which focus on the causes of climate, and empiric methods, which focus on the effects of climate. Examples of genetic classification include methods based on the relative frequency of different air mass types or locations within synoptic weather disturbances.