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AbstractTypically, the cool side of an airmass boundary is stable to vertical motions due to its associated negative buoyancy. However, under certain conditions, the air on the cool side of… Click to show full abstract
AbstractTypically, the cool side of an airmass boundary is stable to vertical motions due to its associated negative buoyancy. However, under certain conditions, the air on the cool side of the bou...
Keywords:
modeling study;
air masses;
air;
mesoscale air;
study mesoscale;
observational modeling
Journal Title: Monthly Weather Review
Year Published: 2017
Link to full text (if available)
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Journal Title: Monthly Weather Review
Year Published: 2017
Link to full text (if available)
Share on Social Media: Sign Up to like & get
recommendations!