because of the rain shadow effect and it has more humid climate because of pollution
Western Washington experiences more rain than Eastern Washington primarily due to the presence of the Cascade Mountain Range. When moist air from the Pacific Ocean moves inland, it is forced to rise over the mountains, leading to cooling and condensation, which results in precipitation on the western slopes. In contrast, Eastern Washington is situated in a rain shadow, where the descending dry air from the mountains reduces rainfall, leading to a drier climate. This geographic and climatic contrast creates the significant difference in rainfall between the two regions.
well, eastern Washington is much drier than western Washington, due to rain shadowing. but overall Washington gets over 135 inches of rain a year.
Washington has two different temperate zones. Eastern Washington's average temperature is around 80 in the summer and 30 in the winter with only about 14 inches of rain. Western Washington is around 75 summer and 40 winter with about 20 inches of rain.
the eastern coast gets more rainfall because of its tall mountains which turn water vapour to droplets of rain.
Because the water cycle rains, evaporates and then soaks in the clouds and rains again. The more humidity, the more rain. Humidity doesn't always have anything to do with it. In Western Washington the clouds get stuck on the Western side of the mountains until the release enough water. They can then go over the mountains to the dry side of Eastern Washington. 2 totally differant cliamates.
More clouds are there on the eastern coastal and its very sunny there throughout the year which makes the water from the gulf of Oman evaporate and rain fast.
The western side of Oregon receives more rain due to its proximity to the Pacific Ocean, which brings moisture-laden air masses that result in precipitation. In contrast, the eastern side of Oregon is in rain shadow of the Cascade Mountain Range, which blocks much of the moisture from reaching that region, resulting in a drier climate.
It's because the western slopes get much heavier rainfall than the eastern slopes. Moisture-laden air moves eastwards across the Western Ghats during monsoon season. The elevation of the region forces most of the moisture out of the air on the western side. By the time the air reaches the eastern side, it is dry; thus, the eastern slopes lie in the region's rain shadow.
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There is more precipitation in the eastern half of the U.S. than the western half of the country. This is due to the Rockie Mountain chain that determines where the precipitation will fall. Moisture is also picked up in the Gulf of Mexico which results in more rain being deposited on the eastern half of the country.
Washington's climate is influenced by the Cascade Mountain range, which acts as a barrier to the prevailing moisture-laden air from the Pacific Ocean. As a result, the western part of Washington, particularly the coastal areas, receives more rainfall and has a wetter climate, while the eastern part, shielded by the mountains, is drier, leading to a rain shadow effect.