North Dakota's climate is typical of a continental climate with cold winters and warm-hot summers. The state's location in the Upper Midwest allows it to experience some of the widest variety of weather in the United States, and each of the four seasons has its own distinct characteristics. The eastern half of the state has a humid continental climate (Köppen climate classification Dfb) with warm to hot, somewhat humid summers and cold, windy winters, while the western half has a semi-arid climate (Köppen climate classification BSk) with less precipitation and less humidity but similar temperature profiles. The areas east of the Missouri River get slightly colder winters, while those west of the stream get higher summer daytime temperatures. In general, the diurnal temperature difference is prone to be more significant in the west due to higher elevation and less humidity.
General climatology
Due to its location in the center of North America North Dakota experiences temperature extremes characteristic of a continental climate, with cold winters and hot summers. Each season has distinctive upper air patterns which bring different weather conditions with them. One feature of a continental climate is that weather patterns can be unpredictable. For example, an Alberta clipper, a low pressure system originating in the province of Alberta in Canada, would be a common winter occurrence in North Dakota. But with the general unpredictability of weather in a continental climate, such a storm system could occur in spring, or in late autumn. Hot weather, though usually confined to July and August, can sometimes begin as early as April or May, and could spill over into September or October.
Being from any large body of water (with the exception of Lake Superior), temperatures and precipitation in North Dakota can vary widely. North Dakota is far enough north to experience −60 °F (−51 °C) temperatures and blizzards during the winter months, but far enough south to experience 121 °F (49 °C) temperatures and tornado outbreaks in the summer. The 181 °F degree (100 °C) variation between North Dakota's highest and lowest temperature is the 3rd largest variation of any U.S. State, and the largest of any non-mountainous state.
North Dakota is far from major sources of moisture and is in the transition zone between the moist East and the semi-arid West, as precipitation and humidity decrease from east to west. Annual average precipitation across the state ranges from around 14 in (35.6 cm) in the west to 22 in (55.9 cm) in the east. Snow is the main form of precipitation from November through March, while rain is the most common the rest of the year. It has snowed in North Dakota during every month except August. The ENSO also has a significant impact on North Dakota's weather. During El Niño, the jet stream is often weakened and shoved further north into Canada. This usually blocks arctic air from entering North Dakota and a milder zonal pattern takes place. The opposite phase, La Niña, strengthens the jet stream even more, making arctic air even colder and more dominant.
Statistics for ThreadEx cities
Seasons
Winter in North Dakota is characterized by cold (below freezing) temperatures and snowfall. Snow is the main form of winter precipitation, but freezing rain, ice, sleet, and sometimes even rain are all possible during the winter months. Common storm systems include Alberta clippers or Panhandle hooks, some of which evolve into blizzards. Annual snowfall averages from 26 inches (66 cm) in the central part of the state to 38 inches (96.5 cm) in the northeast and southwest. Temperatures as low as −60 °F (−51 °C) have occurred during North Dakota winters.
Spring is a time of major transition in North Dakota. Early spring commonly sees snowstorms, but by late spring as temperatures begin to moderate the state can experience tornado outbreaks, a risk which diminishes but does not cease through the summer and into the fall as North Dakota lies at the northern edge of Tornado Alley. Springtime flooding is a relatively common event in the Red River Valley, due to the river flowing north into Canada. The spring melt and the eventual runoff typically begins earlier in the southern part of the valley than in the northern part. The most destructive flooding in eastern North Dakota occurred in 1997, which caused extensive damage to Grand Forks.