Eastern United States Winter Storm of 14-15 December 2013Eastern United States Winter Storm of 14-15 December 2013
Utc 14 December (Fig. 1b). The system followed a Miller-b type (Miller 1946, Kocin and Uccellini 1990, Mote et al. 1997) of evolution with a secondary cyclone developing along the coast around 0000 utc 15 December
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Nws state College Case Examples Pre-Christmas Warm-up 21-23 December 2013-Draft ByNws state College Case Examples Pre-Christmas Warm-up 21-23 December 2013-Draft By
Atlantic by 0000 utc 21 peaking on 23 December when a closed 5940 m high developed (Fig. 1e). As the tough moved into the eastern United States the gradient between the trough and ridge increased producing a surge of deep moisture into the eastern United
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Poorly Forecast Winter Storm of 2-3 March 2014-draftPoorly Forecast Winter Storm of 2-3 March 2014-draft
Stuart et al. 2013, despite a convergence of solutions of several models and ensemble forecast systems, the event proved to be difficult to forecast
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Eastern United States Winter Storm of 12-14 February 2014 Dealing with Divergent Model and Ensemble Forecast SystemsEastern United States Winter Storm of 12-14 February 2014 Dealing with Divergent Model and Ensemble Forecast Systems
Most fatalities were associated with automobile accidents. The snow closed the Federal Government and schools in the Washington, dc metropolitan area and caused thousands of canceled flights from Atlanta to Boston
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Eastern United States Snow event of 5 February 2014 Dealing with uncertainty and varying predictability horizonsEastern United States Snow event of 5 February 2014 Dealing with uncertainty and varying predictability horizons
The flow between the ridge and trough produce a surge of warm moist air into the eastern United States. In the mmv this led to heavy rainfall and in the Mid-Atlantic region
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