Topographic rain occurs when a warm and humid air stream meets a topographical barrier of higher terrain and is forced to climb along the windward slope. The warm and humid air cools while ascending, which causes condensation and rainfall.
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(2020). Topographic Rain. In: Chen, A., Ng, Y., Zhang, E., Tian, M. (eds) Dictionary of Geotourism. Springer, Singapore. https://doi.org/10.1007/978-981-13-2538-0_2496
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DOI: https://doi.org/10.1007/978-981-13-2538-0_2496
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