WFO Morristown, Tennessee Local 4km-WRF Model

Instability-Thermodynamic Parameters

 
Surface |  Instability |  Shear |  Misc |  Precip |  Upper Air |  Soundings |  Bufkit Files |  Model Info
 
Latest Run: 0600 UTC 08/23/2014 Forecast Hours
 
Surface Based Lifted Index 00 01 02 03 04 05 06 07 08 09 10 11 12
Hover   13 14 15 16 17 18 19 20 21 22 23 24
Loop   25 26 27 28 29 30 31 32 33 34 35 36
Surface Based CAPE 00 01 02 03 04 05 06 07 08 09 10 11 12
Hover   13 14 15 16 17 18 19 20 21 22 23 24
Loop   25 26 27 28 29 30 31 32 33 34 35 36
1-hourly CAPE Tendency 00 01 02 03 04 05 06 07 08 09 10 11 12
Hover   13 14 15 16 17 18 19 20 21 22 23 24
Loop   25 26 27 28 29 30 31 32 33 34 35 36
Surface Based CIN 00 01 02 03 04 05 06 07 08 09 10 11 12
Hover   13 14 15 16 17 18 19 20 21 22 23 24
Loop   25 26 27 28 29 30 31 32 33 34 35 36
MU CAPE 00 01 02 03 04 05 06 07 08 09 10 11 12
Hover   13 14 15 16 17 18 19 20 21 22 23 24
Loop   25 26 27 28 29 30 31 32 33 34 35 36
0-3km Lapse Rate 00 01 02 03 04 05 06 07 08 09 10 11 12
Hover   13 14 15 16 17 18 19 20 21 22 23 24
Loop   25 26 27 28 29 30 31 32 33 34 35 36
Total Totals Index 00 01 02 03 04 05 06 07 08 09 10 11 12
Hover   13 14 15 16 17 18 19 20 21 22 23 24
Loop   25 26 27 28 29 30 31 32 33 34 35 36
K Index 00 01 02 03 04 05 06 07 08 09 10 11 12
Hover   13 14 15 16 17 18 19 20 21 22 23 24
Loop   25 26 27 28 29 30 31 32 33 34 35 36
LCL Height (m) 00 01 02 03 04 05 06 07 08 09 10 11 12
Hover   13 14 15 16 17 18 19 20 21 22 23 24
Loop   25 26 27 28 29 30 31 32 33 34 35 36
 
Note: The mesoscale prognostics depicted on these pages are experimental and may not be available at all times. The accuracy or reliability of the data is not guaranteed nor warranted in any way. The data is provided as is and should not be used as the sole resource for decision making. Mesoscale forecast guidance is best interpreted by a professional meteorologist who is familiar with the particular modeling system, including any model biases. This version of the WRF model is greatly influenced by the quality of the NMM model that provides the boundary conditions.

National Weather Service, WFO Morristown, Tennessee

Email: David Hotz


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