it is cold and there is low rainfall
Frontal rainfall is common in the subpolar low pressure belts because they are regions where warm air masses from the tropics meet cold air masses from the polar regions. As the warm air rises over the denser cold air, it cools and condenses, leading to the formation of clouds and precipitation. This collision of air masses at the boundaries of the subpolar low pressure belts creates the ideal conditions for frontal rainfall.
Port Nolloth has a low rainfall due to its location in the rain shadow of the Namibian Escarpment which blocks moisture-laden winds from the Indian Ocean. Additionally, the cold ocean currents offshore further inhibit the development of rain-bearing clouds.
The biome with very cold temperatures and little rainfall is called a tundra. This ecosystem has a short growing season and is characterized by permafrost and low-growing vegetation such as mosses and lichens. Wildlife in the tundra includes animals like reindeer, arctic foxes, and polar bears.
The subarctic region receives an average annual rainfall of about 10-20 inches (250-500 mm) per year. This relatively low precipitation amount is due to the cold temperatures limiting the amount of evaporation and moisture in the air.
Savannas are always in warm climate while temperate grasslands are in warm and cold climate!
The average annual rainfall in tundras is typically very low, ranging from 6 to 10 inches. Tundras are characterized by cold, dry conditions with limited precipitation, often in the form of snow. This low rainfall is a result of the cold temperatures and low moisture content in the atmosphere.
The tundra biome typically has low temperatures and low amounts of rainfall. It is characterized by cold, treeless landscapes with permafrost, and vegetation like mosses, lichens, and shrubs adapted to the harsh conditions.
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.
All deserts, hot or cold, receive low rainfall. It is due to the geographic location of the particular desert. Some are located in mountain shadows, some are in areas with sinking air, some are along coastal areas with cold ocean currents. Some combine more than one of these features.
Both have low precipitation and high evaporation rates.
In a tundra, the annual rainfall typically ranges from 6 to 10 inches. This low precipitation level, combined with cold temperatures, creates a harsh environment with limited plant growth.
Deserts get little rainfall and some of them are quite hot - but not all. There are cold deserts also.
Arctic and Tundra biomes are both characterized by low temperatures and little rainfall. Alpine biomes also have low temperatures but have more rainfall.
Frontal rainfall is common in the subpolar low pressure belts because they are regions where warm air masses from the tropics meet cold air masses from the polar regions. As the warm air rises over the denser cold air, it cools and condenses, leading to the formation of clouds and precipitation. This collision of air masses at the boundaries of the subpolar low pressure belts creates the ideal conditions for frontal rainfall.
Port Nolloth has a low rainfall due to its location in the rain shadow of the Namibian Escarpment which blocks moisture-laden winds from the Indian Ocean. Additionally, the cold ocean currents offshore further inhibit the development of rain-bearing clouds.
convectional rainfall
Low rainfall or no rainfall leads to failure of crops .