Figure 14. An example of the rate of cooling of an airmass rising from ground level to higher altitudes, and the effect on rate of cooling when reaching the point of saturation with respect to water vapor (level of condensation).
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- The Orographic Effect
https://serc.carleton.edu/integrate/teaching_materials/water_science_society/student_materials/751
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Source: Mike Arthur and Demian Saffer
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