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The relationship between circulation and heavy snowfall over the western United States is studied as a means of improving operational forecasts for that region. The models developed relate occurrence of heavy snowfall in 12-hr. periods to initial circulation features and are suitable for direct use on available circulation prognoses.
The relationship between circulation and heavy snowfall over the western United States is studied as a means of improving operational forecasts for that region. The models developed relate occurrence of heavy snowfall in 12-hr. periods to initial circulation features and are suitable for direct use on available circulation prognoses.
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