how did the chesapeake bay form
How Did The Chesapeake Bay Form? About 35.5 million yea...
Mountains and other topographic features can have tremendous influence on precipitation. Rain shadows, or dry regions on the protected side of some mountain ranges, can be some of the driest places on Earth; the Atacama desert in the rain shadow of the Andes Mountains can go decades without receiving any rainfall.
Rain shadows are common on the western coast of the United States, where mountain ranges run parallel to the coast and perpendicular to the prevailing winds coming off the Pacific Ocean.
So in short, absence of rain clouds in leeward side of mountains are responsible for rain shadow regions. Example: the west side of Western Ghats receive high rain from South western monsoon winds and the east side is the rain shadow region.
Rain shadows have an essential ecological significance, just as many other natural phenomena. They can replenish new forests and allow old ones to grow. Since mountains need air and moisture, the rain shadow effect can provide a warm moist that lasts long enough for the ecosystem to thrive in it.
mountains
The rain shadow effect is associated with mountains. A rain shadow is formed when wind carries moist, warm air towards the mountain.
Hint:Rainshadow is a blotch of land that has been forced to become a desert due to mountain ranges that have blocked all its plant growing, and also rainy weather. Rain shadows often can be seen next to some of the world’s most famous mountain ranges.
(i) The leeward side of the hill is called ‘Rain Shadow’ area which remains dry because the winds are blocked by the hills. (ii) An example of ‘Rain Shadow’ area in India is: For Arabian Sea branch Chennai lies at leeward side of western ghats and falls under Rain Shadow area.
A rain shadow area is an area of dry land that lies on the leeward(or downwind) side of a mountain. High mountains act as barriers for cold or hot winds; they may also cause precipitation if they are high enough and lie in the path of rain-bearing winds. The leeward side of the mountains remains dry.
Rain shadow deserts are created when mountain ranges lie parallel to moist, coastal areas. Prevailing winds moving inland cool as air is forced to rise over the mountains. Moisture falls on slopes facing the winds. When the winds move over the mountain crests and down the far side, they are very dry.
The sudden ascent of warm moist air on the windward sides causes cooling of air, leading to condensation and precipitation. … Consequently, the relative humidity drops and there is evaporation and little or no precipitation in the rain shadow area. Hence, a rain shadow area is generally dry.
Orographic rainfall occurs in most of the world. Winds coming from lakes or seas are moisture-laden. They are obstructed by the high mountain ranges coming in their way. They start going upwards along the slope of the mountains, The temperature of these winds drop and condensation occurs and rainfall takes place.
Graupel is typically white, soft, and crumbly. Sleet starts off as a snowflake in the atmosphere, melts in a warmer layer below, and then refreezes into ice as it falls into a below freezing layer below that. Hail forms in a thunderstorm and is a convective process.
Hail can occur at any season, and it occurs during strong thunderstorms. Every storm has an updraft that gathers super-cooled water droplets in an updraft. … Hail is more common than snow, because you don’t need the air to be at freezing temperatures, like snow.
As it passes through a thin layer of warm air in the atmosphere, it melts a bit. … Freezing rain begins as snow, but when it reaches the warm pocket, it melts and becomes rain. Before hitting the ground, it passes through a very shallow pocket of cold air, which cools it some but not enough to turn it into sleet.
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