Classifier Instance:

Anchor text: Big Horn Basin
Target Entity: Bighorn_Basin
Preceding Context: Wyoming's climate is generally semi-arid and continental (Köppen climate classification BSk), and is drier and windier in comparison to most of the United States with greater temperature extremes. Much of this is due to the topography of the state. Summers in Wyoming are warm with July high temperatures averaging between and in most of the state. With increasing elevation, however, this average drops rapidly with locations above averaging around . Summer nights throughout the state are characterized by a rapid cooldown with even the hottest locations averaging in the range at night. In most of the state, most of the precipitation tends to fall in the late spring and early summer. Winters are cold, but are variable with periods of sometimes extreme cold interspersed between generally mild periods, with Chinook winds providing unusually warm temperatures in some locations. Wyoming is a dry state with much of the land receiving less than of rainfall per year. Precipitation depends on elevation with lower areas in the
Succeeding Context: averaging (making the area nearly a true desert). The lower areas in the North and on the eastern plains typically average around , making the climate there semi-arid. Some mountain areas do receive a good amount of precipitation, or more, much of it as snow, sometimes or more annually. The states highest recorded temperature is at Basin on July 12, 1900 and the lowest recorded temperature is at Riverside on February 9, 1933.
Paragraph Title: Climate
Source Page: Wyoming

Ground Truth Types:

Predicted Types:

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