Climate, Weather, and Geography

Temperature is influenced by a combination of factors including latitude, altitude, distance from the ocean, and prevailing wind patterns.

Humid continental climates are found in regions with large landmasses, such as Eastern North America, Central Europe, and Eastern Asia.

Desert climates are found in regions with little to no rainfall, such as the Sahara Desert, Atacama Desert, and Arabian Desert.

Steppe climates are found in regions with moderate rainfall and hot summers, such as the Great Plains of North America, Patagonian Steppe, and Eurasian Steppe.

The bow shock is the boundary between the solar wind and the magnetosphere. The bow shock is formed when the solar wind encounters the magnetosphere and is deflected.

The auroral oval is the region of the Earth's atmosphere where the aurora borealis and aurora australis occur. The auroral oval is located at high latitudes, and it is shaped by the interaction of the solar wind with the Earth's magnetic field.

Permafrost is found in regions with a mean annual temperature of 0 degrees Celsius or below.

Permafrost can contain ice wedges, thermokarst lakes, and pingos.

A pingo is a hill or mound of ice-rich permafrost.

Extreme cold during the winter season is a major challenge for farmers in the Northern Zone, as it can damage crops and reduce yields.

Industrial areas often have large amounts of impervious surfaces, generate heat from industrial processes, and lack vegetation, all of which contribute to higher surface temperatures.

Permafrost is defined as ground that remains frozen for at least two consecutive years, regardless of the surface temperature.

Pingos are mounds of earth and ice that form in permafrost regions, typically as a result of the expansion of ice lenses within the ground.

The trade winds are a global wind pattern that flows from the tropics towards the poles.

A sea breeze is a local wind system that is caused by differences in temperature between land and water.