Orographic lifting occurs when an air mass is forced to rise
over a topographic barrier, such as a mountain range. The rising
air mass expands and cools, with water condensing and forming
droplets as the temperature drops below the dew point.
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Orographic effect is just a change in atmospheric conditions due to elevation, especially when mountains are involved.
That storm is caused by orographic effect.
We studied orographic effect in class.
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Orographic lifting (mountain)
Conditional/Absolute Instability
Frontal Wedging (Cold, Warm Front)
Convergence
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types of rainfall. orographic is commonly called relief
rainfall.