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Team Scalar and Momentum Advection

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1 Team Scalar and Momentum Advection
Assignment #1 Kirstin Gleicher, Michelle Pitcel, and Andrew Rosenow

2 Simulation Differences
Used Milbrandt microphysics scheme Altered momentum and scalar advection closure order Control Run Momentum was 5th order Scalar was 3rd order Experimental Run Momentum was 4th order Scalar was 2nd order

3 Reflectivity Images

4 Mesocyclone Tracking Algorithm
Δx Looks for the first time with precipitation (reflectivity) Finds the maximum column-average vorticity Searches for the next vorticity maximum in two moving domains-one for each post-split supercell Δx, Δy = 10 km Left Mover Domain Δy Previous meso location Right Mover Domain Δy Δx

5 Reflectivity Images Experiment Run Control Run

6 Reflectivity Images Experiment Run Control Run

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39 Planview Plots

40 Reflectivity Images Experiment Run Control Run

41 Vorticity Tendency – m

42 Vorticity Tendency – 1km

43 Vorticity Tendency – 4km

44 Vorticity Tendency – 10km

45 Timeseries Plots

46 Advection Red = Experimental Blue = Control S-1 S-1 Time Step

47 Divergence Red = Experimental Blue = Control S-1 S-1 Time Step

48 Stretching Red = Experimental Blue = Control S-1 S-1 Time Step

49 Solenoidal Red = Experimental Blue = Control S-1 S-1 Time Step

50 Vorticity Tendency Red = Experimental Blue = Control S-1 S-1
Comparison of Maximum in Total Vorticity Tendency at 1km Red = Experimental Blue = Control Comparison of Maximum in Total Vorticity Tendency at 5km Comparison of Maximum in Total Vorticity Tendency at 10km S-1 S-1 Time Step Time Step

51 Conclusions Changing Advection schemes causes spurious waves to propagate throughout the model domain. May need to change resolution if changing advection schemes Despite the waves, simulated supercell showed similar structure within models runs.


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