* Cold temperatures. The average temperature in high-latitude climates is below freezing for most of the year. This is because the sun's rays are less direct at high latitudes, so they provide less heat.
* High levels of precipitation. High-latitude climates typically receive a lot of precipitation, in the form of snow or rain. This is because the air in these climates is often cold and dense, so it can hold more moisture.
* Strong winds. High-latitude climates are often windy, especially in winter. This is because the temperature difference between the polar regions and the tropics creates strong air currents.
* Lack of vegetation. High-latitude climates are often too cold for trees and other plants to grow. This is why these climates are often referred to as "treeless tundra" or "polar desert."