Because the prevailing winds are from the west and there is a coastal mountain range between the sea in the west and the inland western areas.
The inland West region, such as the Great Basin and parts of the Western United States, receives little rainfall due to its distance from oceanic moisture sources. These areas are often in the rain shadow of mountain ranges, which block moisture from reaching the interior. Additionally, the dry climate is influenced by prevailing wind patterns and the region's high elevation, which can inhibit the formation of rain clouds.
The northeastern part of India, specifically the states of Meghalaya and Assam, receive the largest amount of rainfall in South Asia due to the influence of the Indian monsoon and the orographic effect of the Himalayas. Cherapunji in Meghalaya holds the record for the highest annual rainfall in the world.
The American Great Plains generally receive between 20-25 inches of rainfall per year, with the West Coast states like California and Washington getting more rainfall due to their proximity to the Pacific Ocean and mountain ranges. Rainfall in the West varies from less than 10 inches in arid regions to over 100 inches in some mountainous areas.
The amount of rainfall in the Old American West varied greatly depending on the specific region and time period. Generally, the western United States is known for its arid and semi-arid climate, with some areas receiving very little rainfall while others may experience seasonal monsoons or periodic droughts. It is important to research specific regions and time periods to get accurate rainfall data for the Old American West.
Rainfall decreases as it moves from east to west in Texas due to the rain shadow effect caused by the Rocky Mountains. The mountains block moisture-laden air from reaching the western regions, creating drier conditions. This leads to a drier climate in areas west of the mountains.
The inland West region, such as the Great Basin and parts of the Western United States, receives little rainfall due to its distance from oceanic moisture sources. These areas are often in the rain shadow of mountain ranges, which block moisture from reaching the interior. Additionally, the dry climate is influenced by prevailing wind patterns and the region's high elevation, which can inhibit the formation of rain clouds.
Punjab receives rainfall from 3 sources- western disturbances, south west monsoon winds and retreating monsoon winds.
The address of the Arkansas Inland Maritime Museum is: 300 West Markham Street, Little Rock, AR 72201-1406
There is more precipitation along the coast in the pacific west than the farther land because of the convectional currents that cause convectional rainfall.
as they are in south, so the south west monsoon winds carry moisture to it and hence it rains
The annual average rainfall in West Texas ranges from 10 to 20 inches, though this can vary depending on the specific location within the region. Some areas may receive less rainfall due to the semi-arid climate, while others may experience slightly higher amounts.
The northeastern part of India, specifically the states of Meghalaya and Assam, receive the largest amount of rainfall in South Asia due to the influence of the Indian monsoon and the orographic effect of the Himalayas. Cherapunji in Meghalaya holds the record for the highest annual rainfall in the world.
Sweden and Finland receive less rain than Norway because they are located in the rain shadow of the Scandinavian mountain range. This mountain range blocks moisture-laden air masses coming from the west, resulting in less rainfall in the eastern regions of Sweden and Finland. Additionally, Norway's coastal location allows it to receive more moisture from the Atlantic Ocean, increasing its rainfall levels.
In Europe, the areas that are west of the mountains receive more rainfall due to the prevailing westerly winds carrying moisture from the Atlantic Ocean. This leads to a wetter climate on the western side of the mountains and a drier climate on the eastern side, known as the rain shadow effect.
Areas west of the mountains in Europe, such as the UK, Ireland, and parts of France and Spain, receive a significant amount of rainfall due to the prevailing westerly winds carrying moisture from the Atlantic Ocean. These regions are known for their wet and temperate climates, with annual rainfall typically ranging from 700mm to 2000mm.
Annual rainfall varies throughout the country. For example, it can be as much as 2000mm a year in the Southern Mountains or a much lower 400mm in the vicinity of Mainz which is more to the North West. As an average for the whole country, around 600-800mm is a good approximation. In comparison to other countries, this is quite a lot. London, UK, will get around 32-64mm per year.
Because it is dry country- little rainfall.