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The image diagrams "The formation of rain-shadow deserts" over a scale of thousands of kilometres, illustrating a 7-step process. Step 1: Winds approach coast from the sea. Step 2: Winds are pushed upwards along the windward side of the mountains. Step 3: Moist air rises and cools. Step 4: Clouds form. Step 5: Rain falls. Step 6: Dry air continues over the mountain onto the leeward side. Step 7: Dry winds reach inland areas, creating a rain-shadow desert.
Given the complexity of the image, the above description may not be entirely accurate.
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The diagram demonstrates the formation process od the dessert usually called ‘rain-shadow’.
Overall, it is a 7-stage natural process driven by the movements of wind from the sea through thousands kilometres that is subsequently leading to occurene of a dessert on inland areas.
To begin with, the wind approaches coast and is pushed upwards. As the air rises, it becomes cooler and moister which is leading to formation of the clouds. Afterwards, clouds forming causes the dropping of the rain.
After raining, the air that continues moving over the mountain becomes much drier then before. Subsequently, after thousands of kilometres, dry winds finally reach the inland areas where the rain-shadow deserts are forming
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