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Table of contents |
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Convection and Mesoscale Convective Systems |
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Scale Characteristics of MCSs |
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On the evolution, shape and cell movement of MCSs |
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Propagation and movement |
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An example of a backbuilding MCS |
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The original vector method |
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The revised vector method |
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Exercise I. Forecasting convective movement |
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Exercise 2. Forecasting convective movement |
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An ingredients based methodology for predicting convective rainfall. |
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How long will an MCS last before dissipation |
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Original Maddox et al. MCS arch-types associated with flash flooding |
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Synoptic type heavy rainfall events |
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Frontal type heavy rainfall events |
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Mesohigh type heavy rainfall events |
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Use of Climatological thickness |
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“saturated thickness” concept |
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A few thoughts about elevated convection |
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Synoptic Scale Circulation Systems |
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Latent heat and the generation of mesoscale convective vortices |
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A mesoscale convective vortex exercise |
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Rainfall rates, vertical moisture flux and precipitation efficiency |
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Regions of weak inertial stability |
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Western U.S. heavy rains. Overview |
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Maddox type I |
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East slope of the front range events |
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Maddox Type IV events |
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Hurricanes and heavy rainfall |
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Chappell deformation type heavy rainfall event |
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An example of a warm season western flash flood |
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Maddox type II |
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Rainfall at Landfall |
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Kraft rule of thumb |
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TRaP rainfall |
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Rainfall primarily west of track storms |
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Rainfall primarily east of track storms |
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East Pacific Storms |
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Effects over southwestern U.S. |
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Effects over Texas and Oklahoma |
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Hurricanes and the Appalachians |
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References |
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When is a forward propagating MCS likely |
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More on hurricanes and the Appalachians, an exercise |
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Hugo and Fran, a quick comparison |
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A forecast exercise, using pattern recognition and ensemble guidance to predict an heavy rainfall event |
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West coast cold season heavy rainfall events. |
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Role of tropical convection and atmospheric rivers |