In the Eastern Hemisphere, this climate regime is found within interior Eurasia, east-central Asia, and parts of India. The Dfb, Dwb and Dsb subtypes are also known as hemiboreal. Other articles where Continental climate is discussed: Köppen climate classification: Type C and D climates: Through a major portion of the middle and high latitudes (mostly from 25° to 70° N and S) lies a group of climates classified within the Köppen scheme as C and D types. In the UK, continental polar air in winter is very cold and temperatures associated with this air stream are usually well below average. [11] Within wetter areas, maple, spruce, pine, fir, and oak can be found. [6] These temperatures were not arbitrary. The western states of the central United States (namely Montana, Wyoming, parts of southern Idaho, most of Lincoln County in Eastern Washington, parts of Colorado, parts of Utah, western Nebraska, and parts of western North and South Dakota) have thermal regimes which fit the Dfa climate type, but are quite dry, and are generally grouped with the steppe (BSk) climates.

In the Eastern Hemisphere, this climate regime is found within interior Eurasia, east-central Asia, and parts of India. The Dfb, Dwb and Dsb subtypes are also known as hemiboreal. Other articles where Continental climate is discussed: Köppen climate classification: Type C and D climates: Through a major portion of the middle and high latitudes (mostly from 25° to 70° N and S) lies a group of climates classified within the Köppen scheme as C and D types. In the UK, continental polar air in winter is very cold and temperatures associated with this air stream are usually well below average. [11] Within wetter areas, maple, spruce, pine, fir, and oak can be found. [6] These temperatures were not arbitrary. The western states of the central United States (namely Montana, Wyoming, parts of southern Idaho, most of Lincoln County in Eastern Washington, parts of Colorado, parts of Utah, western Nebraska, and parts of western North and South Dakota) have thermal regimes which fit the Dfa climate type, but are quite dry, and are generally grouped with the steppe (BSk) climates.

In the Eastern Hemisphere, this climate regime is found within interior Eurasia, east-central Asia, and parts of India. The Dfb, Dwb and Dsb subtypes are also known as hemiboreal. Other articles where Continental climate is discussed: Köppen climate classification: Type C and D climates: Through a major portion of the middle and high latitudes (mostly from 25° to 70° N and S) lies a group of climates classified within the Köppen scheme as C and D types. In the UK, continental polar air in winter is very cold and temperatures associated with this air stream are usually well below average. [11] Within wetter areas, maple, spruce, pine, fir, and oak can be found. [6] These temperatures were not arbitrary. The western states of the central United States (namely Montana, Wyoming, parts of southern Idaho, most of Lincoln County in Eastern Washington, parts of Colorado, parts of Utah, western Nebraska, and parts of western North and South Dakota) have thermal regimes which fit the Dfa climate type, but are quite dry, and are generally grouped with the steppe (BSk) climates.

In the Eastern Hemisphere, this climate regime is found within interior Eurasia, east-central Asia, and parts of India. The Dfb, Dwb and Dsb subtypes are also known as hemiboreal. Other articles where Continental climate is discussed: Köppen climate classification: Type C and D climates: Through a major portion of the middle and high latitudes (mostly from 25° to 70° N and S) lies a group of climates classified within the Köppen scheme as C and D types. In the UK, continental polar air in winter is very cold and temperatures associated with this air stream are usually well below average. [11] Within wetter areas, maple, spruce, pine, fir, and oak can be found. [6] These temperatures were not arbitrary. The western states of the central United States (namely Montana, Wyoming, parts of southern Idaho, most of Lincoln County in Eastern Washington, parts of Colorado, parts of Utah, western Nebraska, and parts of western North and South Dakota) have thermal regimes which fit the Dfa climate type, but are quite dry, and are generally grouped with the steppe (BSk) climates.