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| | THE EFFECTS OF MOUNTAINS AND COMPLEX TERRAIN ON AIRFLOW AND DEVELOPMENT OF CLOUDS AND PRECIPITATION |
 | | Airflow around orographic features, particularly isolated mesoscale mountains or hills, may cause vortices to form on the lee side of the obstacle. |
 | | Those relevant to this discussion are: the moisture content of low-level air, the stability of the atmosphere, the shape of the mountain, the slope of the hill perpendicular to the wind direction, the strength of the wind normal to the mountain, and cloud water content. |
 | | The kinds of lift that mountains and complex terrain provide can be direct, such as forced orographic ascent when airflow encounters an obstacle, or more indirect, such as when stable flow produces blocking or waves or when mountain slopes are heated and the mountain acts as a high-level heat and moisture source (Banta, 1990). |
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