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About: Humid continental climate     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatPlantsOfHumidContinentalClimate, within Data Space : dbpedia.org associated with source document(s)

Type: yago:WikicatTreesOfHumidContinentalClimateyago:LivingThing100004258yago:Object100002684yago:Organism100004475yago:PhysicalEntity100001930yago:Plant100017222yago:WoodyPlant113103136settlementyago:Tree113104059yago:VascularPlant113083586yago:Whole100003553yago:WikicatPlantsOfHumidContinentalClimate New Facet based on Instances of this Class

A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers and freezing cold (sometimes severely cold in the northern areas) winters. Precipitation is usually distributed throughout the year but often do have dry seasons. The definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below 0 °C (32.0 °F) or −3 °C (26.6 °F) depending on the isotherm, and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). In addition, the location in question must not be semi-arid or arid. The cooler Dfb, Dwb, and Dsb subtypes are also known as