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The image, titled 'The formation of rain-shadow deserts', diagrams a 7-step process across a geographical cross-section spanning 'Thousands of kilometres'. The process begins over the 'Sea' and 'Coast' with step 1: 'Winds approach coast'. Step 2 shows 'Winds pushed upwards' onto the 'Windward side' of the 'Mountains'. Step 3 is when 'Moist air rises and cools', leading to step 4: 'Clouds form'. In step 5, 'Rain falls' over the mountain's peak and windward side. Following this, step 6 shows 'Dry air continues over mountain' down the 'Leeward side'. Finally, in step 7, 'Dry winds reach inland areas', creating an 'Inland' 'Rain-shadow desert'.
Given the complexity of the image, the above description may not be entirely accurate.
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The graph illustrates the formation of one type of desert, known as a rain‑shadow desert.
Overall, the process consists of seven steps and can be broadly divided into two stages, depending on whether the wind passes before or after the mountain peak.
When winds approach the coast, seawater evaporates and accumulates. On the windward side of mountains, wind pushes upwards. As moist air rises and cools, clouds start to form. Near the peak, the wind can no longer hold moisture, so rainfall occurs.
After precipitation, dry air flows over to the leeward side of the mountain.
After that, dry winds move inland, forming the rain‑shadow desert. This effect can extend for thousands of kilometres. Rain‑shadow deserts always appear on the leeward side of high mountains, which block moist air from reaching inland.
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