The maximum amount of moisture carried in the air is proportional to the air temperature. Note that hot deserts usually have the water removed before it gets to the hot, dry area (usually by mountains).
The tundra biome can be both cold and warm but has low precipitation due to cold temperatures that prevent much evaporation.
An example of a place that is cold and experiences low rainfall is a polar desert, such as Antarctica. These regions have extremely low precipitation levels due to the cold temperatures leading to minimal moisture in the air.
Arid climate regions have low precipitation and tend to be hot, while semi-arid regions also have low precipitation but can be either hot or cold. The desert climate is an example of an arid climate, characterized by extreme dryness and high temperatures.
You would expect to find a cold desert biome in a region with low temperatures and low precipitation. Cold deserts typically have sparse vegetation, rocky terrain, and are characterized by cold winters and hot summers. Examples of cold deserts include the Gobi Desert in Asia and the Atacama Desert in South America.
Cold, precipitation, windy and yucky :P
The climate region characterized by low to moderate precipitation and cold temperatures is typically classified as a subarctic or boreal climate. This region experiences long, harsh winters with cold temperatures and short, mild summers. Precipitation is generally low, often falling as snow during the winter months. Examples of areas with this climate include parts of Canada, Alaska, and northern Scandinavia.
The tundra is very cold due to its high latitude. Its cold temperatures inhibit the amount of moisture in the air, resulting in little rainfall or precipitation. This combination of cold temperatures and low precipitation creates the characteristic harsh environment of the tundra.
The precipitation in the tundra biome is typically low, ranging from about 6 to 10 inches (15 to 25 cm) per year. This low precipitation mainly falls as snow during the colder months, with minimal rainfall in the warmer seasons.
A climate region that has low to moderate precipitation and cold temperatures is typically a subarctic climate. These regions are characterized by short summers and long, cold winters with temperatures often below freezing. Examples include parts of Siberia, Canada, and Alaska.
A cold front typically brings cooler temperatures and heavy precipitation. When a cold front moves into an area, it can trigger the lifting of warm, moist air which leads to the formation of clouds and precipitation. This can result in significant amounts of rain or snow depending on the temperature.
Antarctica's lack of humidity and precipitation is caused by the lack of moisture, not necessarily by cold. It is true, however, that cold air holds less moisture due to it having a lower saturation point than warm air.
Both have low precipitation and high evaporation rates.