The subarctic is a very cold place. 
The subarctic is a cold land. 
The subarctic is a large region in the North.
The weather here is very cold. For most of the year, it stays chilly. In the summer, it stays warm for only a few months. The air is cold, so it does not hold much moisture. This means there is not much rain. Because of this, most places do not have huge glaciers.
Many trees grow here in forests called taiga. 
Large animals live in these lands. You might see moose, elk, or bears. You may also see wolves and reindeer. People also use the land to find minerals. They also fish in the cold seas. Today, many people visit to see the beautiful ice and mountains.
The subarctic is a huge region in the Northern Hemisphere. 
Weather in the subarctic works in a very specific way. The air is cold and does not hold much moisture. This means there is usually low precipitation, or rain and snow. Temperatures stay above freezing for only one to three months each year. In the summer, the sun stays up for a very long time. Near the summer solstice, the sun might never go far below the horizon. This creates long periods of twilight or even full daylight. 
History shows that humans found this land quite difficult to live on. Most of the subarctic was not explored until the 1700s or 1800s. Many early settlements were built just to find minerals. Some of these towns, like those in the Yukon, are now abandoned. In Russia, Joseph Stalin led big industrial projects in the Central Siberian Plateau. This helped people settle the area to reach mineral resources. Later, Canada used hydroelectric power in the 1950s and 1960s to help development.
There are many important facts about the land and its life. The soil is often called podsols or gelisols. In many places, the ground has permafrost, which is soil that stays frozen. This makes building roads and cities very hard and expensive. Murmansk is the largest city in this region. Large animals like moose, elk, and bears live in the taiga forests. You can also find reindeer and wolves there. The Grand Banks and Sea of Okhotsk are two of the richest fisheries in the world.
Today, the subarctic connects to our world through travel and resources. Many people visit the region for tourism to see glacial landscapes. It is often expensive to visit because of the hard travel. People use "bush" planes, helicopters, and riverboats to move around. This is because there are very few roads or rail lines. You might know about mining for metals like nickel or cobalt. These minerals often come from the rich ground in Canada and Siberia. Even though it is a tough place to live, it is full of wonder.
The subarctic is a vast geographic zone located in the Northern Hemisphere.
Weather patterns in the subarctic are shaped by extreme temperature changes. Temperatures stay above freezing for only one to three months each year. The air is very cold and holds very little moisture. Because of this, precipitation is usually low. However, precipitation is often higher during the warmer summer months. In the Russian Far East, summer precipitation can be extreme. In most areas, glaciers are small because there is not enough winter precipitation. In the wettest areas, however, glaciers can be very abundant. 
Vegetation in the subarctic is defined by the taiga. The taiga is a forest of mostly coniferous trees. Deciduous trees, which lose their leaves, often cannot survive the long winters. In northern Norway, winters are milder, allowing some broadleaf forests to grow. In some areas, the soil stays saturated with water almost all year. This prevents tree growth and creates peaty herblands. These lands are dominated by grasses and sedges. 
Many large terrestrial mammals call the subarctic home. These animals must be able to survive the harsh conditions. The most important species include elk and moose (Alces alces). You can also find bears, reindeer (Rangifer tarandus), and wolves (Canis lupus). Because many crops cannot grow in this climate, agriculture is difficult. Most farming is limited to animal husbandry. In some specific locations, farmers can grow barley. This makes the region's food production very different from warmer climates.
Building in the subarctic presents massive engineering challenges. Much of the region sits on permafrost. Permafrost is ground that remains frozen for much of the year. This occurs in areas that lack warm ocean currents or good drainage. Building roads and cities on frozen ground is very difficult and expensive. Consequently, cities are generally small. Murmansk is the largest city in the subarctic. Transportation is also limited by the terrain. Most travel relies on "bush" planes, helicopters, or riverboats during the summer. Subarctic rail lines are rare. They exist in parts of Europe, the Alaska Railroad, and a few lines in Siberia and Canada.
Human history in the subarctic is tied to resource extraction. Most of the region was not explored until the 18th and 19th centuries. Many early settlements were established specifically for mining. Some of these, such as those in the Yukon and Northwest Territories, are now abandoned. In Russia, the Trans-Siberian Railway helped people settle the area. Industrialization under Joseph Stalin also boosted settlement to reach minerals in the Central Siberian Plateau. Canada saw development through hydroelectric projects in the 1950s and 1960s. These projects, like Hydro-Quebec, helped supply power to the south.
The economy of the subarctic relies on several key industries. Canada and Siberia are very rich in minerals. These include nickel, molybdenum, cobalt, lead, zinc, and uranium. The Grand Banks and the Sea of Okhotsk are also vital. These two areas are among the richest fisheries in the world. They provide essential support for many small coastal towns. Today, tourism is a growing source of revenue. Travelers are drawn to the beautiful glacial landscapes. However, visiting is often very expensive due to high living costs and difficult transportation. Older industries like fishing and mining now face threats from overfishing and environmental opposition.
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