The Colorado Low forms (or redevelops)on the eastern side of the Canadian Rockies in Alberta, then rapidly skirts across the northern tier of US states.
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Q12: Like hurricanes, polar lows have a clear
Q13: Jet streaks often occur away from jet
Q14: The polar jet stream removes air above
Q15: Aloft, waves are a fundamental feature of
Q16: The polar front theory of a developing
Q18: Storms typically form along the polar front.
Q19: Like hurricanes, polar lows normally have a
Q20: Temperature advection does not occur when the
Q21: When a deep upper-level trough is located
Q22: The name _ is given to a
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