


Soaring Guidance
Issued by NWS Pueblo, CO
Issued by NWS Pueblo, CO
273 UXUS97 KPUB 111206 SRGPUB Soaring Forecast National Weather Service Pueblo, Colorado 0606 MDT Tuesday, March 11, 2025 This forecast is for the Air Force Academy for Tuesday, March 11, 2025: If the trigger temperature of 50.2 F/10.1 C is reached...then Thermal Soaring Index....................... Excellent Maximum rate of lift........................ 1464 ft/min (7.4 m/s) Maximum height of thermals.................. 22608 ft MSL (15002 ft AGL) Forecast maximum temperature................... 63.0 F/17.7 C Time of trigger temperature.................... 1030 MDT Time of overdevelopment........................ None Middle/high clouds during soaring window....... None Surface winds during soaring window............ 20 mph or less Height of the -3 thermal index................. 17379 ft MSL (9772 ft AGL) Thermal soaring outlook for Wednesday 03/12.... Excellent Wave Soaring Index............................. Not available Remarks... Sunrise/Sunset.................... 07:15:48 / 19:02:26 MDT Total possible sunshine........... 11 hr 46 min 38 sec (706 min 38 sec) Altitude of sun at 13:09:07 MDT... 47.58 degrees Upper air data from numerical model forecast valid on 03/11/2025 at 0600 MDT Freezing level.................. 10722 ft MSL (3116 ft AGL) Convective condensation level... 20623 ft MSL (13017 ft AGL) Lifted condensation level....... 21292 ft MSL (13686 ft AGL) Lifted index.................... -0.3 K index......................... -27.7 Height Temperature Wind Wind Spd Lapse Rate ConvectionT Thermal Lift Rate ft MSL deg C deg F Dir kt m/s C/km F/kft deg C deg F Index fpm m/s -------------------------------------------------------------------------------- 50000 -57.3 -71.1 255 68 35 2.0 1.1 M M M M M 45000 -54.3 -65.7 250 80 41 2.0 1.1 M M M M M 40000 -51.4 -60.5 255 83 43 1.9 1.0 M M M M M 38000 -51.6 -60.9 255 78 40 -3.9 -2.2 M M M M M 36000 -54.2 -65.6 255 62 32 -3.9 -2.1 M M M M M 34000 -55.8 -68.4 250 49 25 8.0 4.4 M M M M M 32000 -51.4 -60.5 255 45 23 7.3 4.0 M M M M M 30000 -46.9 -52.4 255 42 22 9.1 5.0 21.1 69.9 2.9 M M 29000 -44.3 -47.7 260 41 21 8.9 4.9 20.6 69.1 2.6 M M 28000 -41.6 -42.9 260 39 20 8.9 4.9 20.3 68.6 2.4 M M 27000 -38.9 -38.0 260 38 20 8.9 4.9 20.2 68.3 2.3 M M 26000 -36.5 -33.7 260 37 19 8.0 4.4 19.5 67.0 1.8 M M 25000 -34.1 -29.4 255 35 18 8.0 4.4 18.8 65.8 1.3 M M 24000 -31.7 -25.1 255 34 17 8.0 4.4 18.2 64.8 0.8 M M 23000 -29.3 -20.7 255 31 16 8.0 4.4 17.6 63.6 0.3 M M 22000 -26.9 -16.4 255 29 15 8.0 4.4 16.9 62.5 -0.3 1413 7.2 21000 -23.9 -11.0 260 25 13 7.7 4.2 16.2 61.2 -0.8 1287 6.5 20000 -21.6 -6.9 260 22 11 7.6 4.2 15.5 59.8 -1.6 1188 6.0 19500 -20.4 -4.7 260 20 10 7.6 4.2 15.1 59.2 -1.9 1139 5.8 19000 -19.3 -2.7 265 18 9 7.6 4.2 14.8 58.6 -2.2 1090 5.5 18500 -18.1 -0.6 265 16 8 8.0 4.4 14.5 58.1 -2.4 1040 5.3 18000 -16.9 1.6 265 15 8 8.1 4.5 14.2 57.5 -2.7 989 5.0 17500 -15.7 3.7 265 14 7 8.1 4.4 13.9 57.1 -3.0 938 4.8 17000 -14.5 5.9 265 13 7 7.5 4.1 13.6 56.5 -3.3 888 4.5 16500 -13.4 7.9 260 13 7 7.6 4.2 13.2 55.8 -3.7 840 4.3 16000 -12.3 9.9 255 12 6 7.3 4.0 12.8 55.1 -4.0 792 4.0 15500 -11.2 11.8 245 11 6 7.3 4.0 12.4 54.4 -4.4 745 3.8 15000 -10.1 13.8 235 11 6 7.8 4.3 12.1 53.7 -4.8 697 3.5 14500 -8.9 16.0 235 10 5 8.1 4.5 11.8 53.2 -5.1 646 3.3 14000 -7.7 18.1 230 9 5 8.2 4.5 11.5 52.8 -5.4 595 3.0 13500 -6.5 20.3 235 9 5 8.4 4.6 11.3 52.3 -5.7 543 2.8 13000 -5.2 22.6 240 8 4 10.1 5.5 11.1 51.9 -5.9 491 2.5 12500 -3.8 25.2 245 9 4 6.6 3.6 11.0 51.8 -6.0 434 2.2 12000 -2.9 26.8 260 10 5 6.7 3.7 10.5 50.9 -6.5 391 2.0 11750 -2.3 27.9 265 11 5 7.9 4.4 10.3 50.5 -6.7 367 1.9 11500 -1.7 28.9 270 11 6 7.8 4.3 10.2 50.3 -6.9 341 1.7 11250 -1.2 29.8 275 12 6 6.9 3.8 10.0 49.9 -7.1 319 1.6 11000 -0.7 30.7 275 13 7 7.1 3.9 9.7 49.5 -7.3 296 1.5 10750 -0.2 31.6 280 14 7 7.0 3.8 9.5 49.2 -7.6 273 1.4 10500 0.3 32.5 280 14 7 6.9 3.8 9.3 48.8 -7.8 251 1.3 10250 0.9 33.6 280 14 7 8.2 4.5 9.1 48.4 -8.1 227 1.2 10000 1.5 34.7 275 14 7 9.2 5.1 9.1 48.3 -8.2 200 1.0 9750 2.2 36.0 275 13 7 9.0 4.9 9.0 48.2 -8.3 174 0.9 9500 2.8 37.0 275 13 6 8.8 4.9 9.0 48.1 -8.4 146 0.7 9250 3.5 38.3 275 12 6 9.6 5.3 8.9 48.0 -8.5 119 0.6 9000 4.2 39.6 275 12 6 8.5 4.6 8.9 48.0 -8.5 91 0.5 8750 4.7 40.5 270 12 6 6.9 3.8 8.7 47.6 -8.7 67 0.3 8500 5.2 41.4 270 12 6 3.9 2.1 8.4 47.1 -9.0 47 0.2 8250 5.6 42.1 270 12 6 14.0 7.7 8.1 46.6 -9.3 26 0.1 8000 6.5 43.7 265 11 6 -4.8 -2.7 8.3 47.0 -9.2 M M 7750 3.8 38.8 270 9 5 -65.1 -35.7 4.9 40.8 -12.6 64 0.3 7500 M M M M M M M M M M M M 7250 M M M M M M M M M M M M 7000 M M M M M M M M M M M M 6750 M M M M M M M M M M M M * * * * * * Numerical weather prediction model forecast data valid * * * * * * 03/11/2025 at 0900 MDT | 03/11/2025 at 1200 MDT | CAPE... 0.0 LI... +3.0 | CAPE... 0.0 LI... +2.8 CINH... 0.0 K Index... -17.3 | CINH... 0.0 K Index... -20.0 | Height Temperature Wnd WndSpd Lapse Rate | Temperature Wnd WndSpd Lapse Rate ft MSL deg C deg F Dir kt m/s C/km F/kft | deg C deg F Dir kt m/s C/km F/kft -------------------------------------------------------------------------------- 50000 -57.0 -70.6 250 63 33 1.6 0.9 | -57.8 -72.0 250 68 35 1.1 0.6 45000 -54.6 -66.3 245 72 37 1.4 0.8 | -56.1 -69.0 245 75 39 1.2 0.6 40000 -53.1 -63.6 255 79 41 1.0 0.5 | -54.9 -66.8 255 80 41 0.8 0.4 38000 -53.3 -63.9 255 77 40 -2.6 -1.4 | -55.0 -67.0 255 76 39 -1.4 -0.8 36000 -54.9 -66.8 255 68 35 -2.6 -1.4 | -55.9 -68.6 255 65 33 -1.4 -0.8 34000 -55.9 -68.6 255 57 29 8.6 4.7 | -56.3 -69.3 255 54 28 6.9 3.8 32000 -51.4 -60.5 260 49 25 7.5 4.1 | -51.7 -61.1 255 46 24 7.6 4.2 30000 -46.8 -52.2 265 41 21 8.9 4.9 | -47.1 -52.8 260 39 20 8.8 4.8 29000 -44.1 -47.4 265 41 21 8.8 4.9 | -44.5 -48.1 260 38 20 8.7 4.8 28000 -41.5 -42.7 265 40 21 8.8 4.9 | -41.9 -43.4 265 37 19 8.7 4.8 27000 -38.8 -37.8 265 39 20 8.8 4.8 | -39.2 -38.6 270 37 19 8.7 4.8 26000 -36.3 -33.3 265 38 19 8.6 4.7 | -36.6 -33.9 270 36 19 8.9 4.9 25000 -33.7 -28.7 265 37 19 8.6 4.7 | -33.9 -29.0 265 35 18 8.9 4.9 24000 -31.1 -24.0 270 35 18 8.8 4.8 | -30.6 -23.1 265 34 17 8.7 4.8 23000 -28.8 -19.8 265 33 17 7.4 4.0 | -28.0 -18.4 265 33 17 8.3 4.6 22000 -26.6 -15.9 265 30 16 7.4 4.0 | -25.5 -13.9 265 32 16 8.4 4.6 21000 -24.3 -11.7 265 28 14 7.4 4.1 | -23.0 -9.4 265 30 16 7.5 4.1 20000 -21.5 -6.7 260 24 12 7.6 4.2 | -20.8 -5.4 265 28 15 7.3 4.0 19500 -20.4 -4.7 260 22 11 7.6 4.2 | -19.7 -3.5 265 27 14 7.3 4.0 19000 -19.2 -2.6 260 21 11 7.6 4.2 | -18.6 -1.5 265 26 13 7.3 4.0 18500 -18.1 -0.6 260 19 10 7.8 4.3 | -17.5 0.5 265 25 13 7.5 4.1 18000 -16.9 1.6 260 18 9 7.9 4.3 | -16.4 2.5 260 24 12 7.6 4.2 17500 -15.7 3.7 260 16 8 7.9 4.3 | -15.2 4.6 260 23 12 7.6 4.2 17000 -14.5 5.9 260 15 8 7.7 4.2 | -14.1 6.6 260 22 11 7.6 4.2 16500 -13.4 7.9 260 13 7 7.8 4.3 | -13.0 8.6 260 21 11 7.6 4.2 16000 -12.3 9.9 255 12 6 6.6 3.6 | -11.8 10.8 255 20 10 7.5 4.1 15500 -11.3 11.7 245 11 6 6.5 3.6 | -10.7 12.7 255 19 10 7.5 4.1 15000 -10.3 13.5 235 10 5 6.9 3.8 | -9.6 14.7 255 18 9 7.4 4.0 14500 -9.3 15.3 230 9 5 7.2 3.9 | -8.5 16.7 255 16 8 7.3 4.0 14000 -8.2 17.2 220 8 4 7.4 4.1 | -7.4 18.7 255 15 8 7.0 3.8 13500 -7.1 19.2 220 7 3 7.7 4.2 | -6.5 20.3 260 13 7 6.3 3.4 13000 -6.0 21.2 220 5 3 8.7 4.8 | -5.5 22.1 260 12 6 7.1 3.9 12500 -4.7 23.5 230 4 2 6.7 3.7 | -4.5 23.9 260 11 6 6.4 3.5 12000 -3.8 25.2 265 4 2 6.8 3.7 | -3.6 25.5 265 9 5 6.4 3.5 11750 -3.3 26.1 280 4 2 7.3 4.0 | -3.1 26.4 270 9 5 6.9 3.8 11500 -2.7 27.1 285 4 2 7.8 4.3 | -2.5 27.5 270 9 4 7.8 4.3 11250 -2.1 28.2 290 4 2 8.1 4.4 | -2.0 28.4 270 8 4 8.3 4.6 11000 -1.5 29.3 295 4 2 7.9 4.3 | -1.4 29.5 270 7 4 8.3 4.5 10750 -1.0 30.2 300 4 2 7.4 4.1 | -0.8 30.6 270 7 4 8.3 4.6 10500 -0.4 31.3 295 4 2 7.1 3.9 | -0.1 31.8 265 6 3 8.2 4.5 10250 0.1 32.2 295 4 2 8.8 4.8 | 0.5 32.9 260 6 3 10.4 5.7 10000 0.9 33.6 290 4 2 9.6 5.3 | 1.4 34.5 260 5 3 11.4 6.2 9750 1.5 34.7 290 4 2 8.4 4.6 | 2.1 35.8 260 5 3 9.4 5.2 9500 2.1 35.8 290 4 2 7.9 4.3 | 2.8 37.0 260 5 3 8.5 4.7 9250 2.7 36.9 290 4 2 9.2 5.0 | 3.5 38.3 260 5 2 10.1 5.6 9000 3.4 38.1 290 4 2 8.8 4.8 | 4.3 39.7 255 5 2 11.6 6.4 8750 4.0 39.2 285 5 2 6.9 3.8 | 5.1 41.2 255 4 2 10.4 5.7 8500 4.5 40.1 285 5 3 6.2 3.4 | 5.9 42.6 255 4 2 10.7 5.9 8250 5.0 41.0 285 5 3 8.8 4.8 | 6.7 44.1 255 4 2 8.7 4.8 8000 5.6 42.1 275 6 3 4.0 2.2 | 7.4 45.3 255 4 2 13.0 7.1 7750 5.3 41.5 275 5 3 -11.4 -6.2 | 8.8 47.8 245 3 2 25.9 14.2 7500 M M M M M M M | M M M M M M M 7250 M M M M M M M | M M M M M M M 7000 M M M M M M M | M M M M M M M 6750 M M M M M M M | M M M M M M M 03/11/2025 at 1500 MDT | 03/11/2025 at 1800 MDT | CAPE... 0.0 LI... +2.5 | CAPE... +1.3 LI... +0.1 CINH... 0.0 K Index... -9.3 | CINH... -5.5 K Index... +4.6 | Height Temperature Wnd WndSpd Lapse Rate | Temperature Wnd WndSpd Lapse Rate ft MSL deg C deg F Dir kt m/s C/km F/kft | deg C deg F Dir kt m/s C/km F/kft -------------------------------------------------------------------------------- 50000 -56.8 -70.2 255 67 35 0.7 0.4 | -57.1 -70.8 255 60 31 0.2 0.1 45000 -55.8 -68.4 250 78 40 0.9 0.5 | -56.8 -70.2 250 74 38 0.2 0.1 40000 -53.7 -64.7 255 75 38 1.4 0.8 | -54.9 -66.8 255 69 35 1.3 0.7 38000 -53.8 -64.8 250 70 36 -2.8 -1.5 | -54.8 -66.6 250 62 32 -1.6 -0.9 36000 -55.5 -67.9 250 61 32 -2.8 -1.5 | -55.8 -68.4 250 50 26 -1.6 -0.9 34000 -57.1 -70.8 245 53 27 3.4 1.9 | -56.4 -69.5 245 40 20 5.9 3.3 32000 -51.7 -61.1 245 47 24 8.0 4.4 | -51.8 -61.2 240 34 17 7.6 4.1 30000 -46.7 -52.1 245 42 22 9.8 5.4 | -47.2 -53.0 235 29 15 9.7 5.3 29000 -43.8 -46.8 245 39 20 9.7 5.3 | -44.3 -47.7 235 31 16 9.5 5.2 28000 -40.9 -41.6 245 36 19 9.7 5.3 | -41.5 -42.7 235 33 17 9.5 5.2 27000 -38.0 -36.4 245 33 17 9.4 5.1 | -38.6 -37.5 235 34 18 9.7 5.3 26000 -35.5 -31.9 245 33 17 7.9 4.4 | -36.2 -33.2 235 35 18 7.8 4.3 25000 -33.2 -27.8 245 32 17 8.0 4.4 | -33.8 -28.8 235 34 18 7.9 4.3 24000 -30.8 -23.4 250 32 16 7.9 4.3 | -31.5 -24.7 235 34 18 7.9 4.3 23000 -28.3 -18.9 250 32 16 8.5 4.7 | -29.2 -20.6 235 33 17 7.1 3.9 22000 -25.7 -14.3 250 32 16 8.5 4.7 | -26.6 -15.9 240 31 16 7.1 3.9 21000 -23.2 -9.8 250 32 16 8.3 4.6 | -24.4 -11.9 240 30 15 7.6 4.2 20000 -20.8 -5.4 255 30 15 7.8 4.3 | -22.1 -7.8 245 27 14 7.8 4.3 19500 -19.0 -2.2 260 28 15 7.8 4.3 | -20.9 -5.6 250 25 13 7.8 4.3 19000 -17.9 -0.2 260 27 14 7.8 4.3 | -19.7 -3.5 255 24 12 7.8 4.3 18500 -16.7 1.9 265 27 14 6.7 3.7 | -18.5 -1.3 255 22 12 7.9 4.4 18000 -15.8 3.6 265 26 13 6.1 3.4 | -17.3 0.9 255 21 11 8.1 4.5 17500 -14.9 5.2 265 25 13 6.2 3.4 | -16.1 3.0 255 20 10 8.2 4.5 17000 -13.9 7.0 265 25 13 7.2 3.9 | -14.9 5.2 255 19 10 8.2 4.5 16500 -12.8 9.0 265 24 13 7.1 3.9 | -13.7 7.3 255 17 9 8.3 4.5 16000 -11.8 10.8 265 24 12 7.5 4.1 | -12.5 9.5 255 16 8 8.4 4.6 15500 -10.7 12.7 260 23 12 7.6 4.2 | -11.3 11.7 260 15 8 8.5 4.7 15000 -9.5 14.9 260 22 11 7.7 4.2 | -10.0 14.0 265 15 8 8.9 4.9 14500 -8.4 16.9 260 20 10 7.8 4.3 | -8.7 16.3 265 14 7 9.3 5.1 14000 -7.3 18.9 255 18 9 8.2 4.5 | -7.3 18.9 260 13 7 9.5 5.2 13500 -6.1 21.0 250 15 8 9.1 5.0 | -5.9 21.4 260 12 6 10.3 5.6 13000 -4.8 23.4 245 11 6 11.3 6.2 | -4.4 24.1 255 12 6 13.2 7.2 12500 -3.2 26.2 240 10 5 7.6 4.2 | -2.7 27.1 255 11 6 7.1 3.9 12000 -2.0 28.4 230 8 4 8.3 4.6 | -1.4 29.5 250 10 5 7.9 4.4 11750 -1.3 29.7 225 7 4 9.0 4.9 | -0.8 30.6 250 10 5 9.1 5.0 11500 -0.6 30.9 215 7 4 9.4 5.2 | -0.1 31.8 245 10 5 9.4 5.2 11250 0.1 32.2 215 7 4 9.3 5.1 | 0.6 33.1 245 10 5 8.7 4.8 11000 0.7 33.3 210 7 4 9.4 5.1 | 1.2 34.2 240 9 5 8.9 4.9 10750 1.4 34.5 205 7 4 9.0 4.9 | 1.9 35.4 235 9 5 8.8 4.8 10500 2.1 35.8 200 7 4 9.1 5.0 | 2.5 36.5 230 9 4 8.8 4.8 10250 2.8 37.0 200 7 3 10.7 5.9 | 3.2 37.8 220 9 4 9.5 5.2 10000 3.7 38.7 195 7 3 11.4 6.2 | 4.0 39.2 215 8 4 9.8 5.4 9750 4.5 40.1 195 7 3 9.8 5.4 | 4.7 40.5 215 8 4 9.5 5.2 9500 5.1 41.2 195 7 3 8.6 4.7 | 5.4 41.7 210 8 4 9.2 5.1 9250 5.8 42.4 190 7 3 9.9 5.4 | 6.1 43.0 200 8 4 9.5 5.2 9000 6.6 43.9 190 7 3 11.1 6.1 | 6.8 44.2 195 8 4 9.8 5.4 8750 7.4 45.3 185 7 3 10.3 5.6 | 7.5 45.5 190 8 4 9.4 5.2 8500 8.2 46.8 185 7 3 10.2 5.6 | 8.2 46.8 190 8 4 9.1 5.0 8250 8.9 48.0 185 7 3 9.1 5.0 | 8.9 48.0 185 8 4 9.3 5.1 8000 9.6 49.3 180 7 3 12.4 6.8 | 9.6 49.3 180 8 4 9.4 5.2 7750 10.9 51.6 180 6 3 22.9 12.6 | 10.3 50.5 175 7 4 9.5 5.2 7500 M M M M M M M | M M M M M M M 7250 M M M M M M M | M M M M M M M 7000 M M M M M M M | M M M M M M M 6750 M M M M M M M | M M M M M M M ________________________________________________________________________________ This product is issued twice per day, once by approximately 0630 MST/0730 MDT (1330 UTC). It is not continuously monitored nor updated after its initial issuance. The information contained herein is based on rawinsonde observation and/or numerical weather prediction model data taken near the Air Force Academy in Colorado Springs, Colorado at North Latitude: 38 deg 58 min 48.000 sec West Longitude: 104 deg 49 min 12.000 sec Elevation: 6572 feet (2003 meters) and may not be representative of other areas along the Front Range of the Colorado Rocky Mountains. Note that some elevations in numerical weather prediction models differ from actual station elevations, which can lead to data which appear to be below ground. Erroneous data such as these should not be used. The content and format of this report as well as the issuance times are subject to change without prior notice. Comments and suggestions are welcome and should be directed to one of the addresses or phone numbers shown at the bottom of this page. To expedite a response to comments, be sure to mention your interest in the soaring forecast. DEFINITIONS: CAPE (Convective Available Potential Energy) - An integrated measure of the energy available for convective development, also known as the positive area on a thermodynamic diagram. Units are Joules per kilogram. Larger values are indicative of greater instability and the possibility of stronger convective activity, including thunderstorms. Values around or greater than 1000 suggest the possibility of severe weather should convective activity develop. CIN (Convective Inhibition) - An integrated measure of the amount of energy needed to initiate convective activity, also known as the negative area on a thermodynamic diagram. Units are Joules per kilogram. The more negative this number, the more energy is required to initiate convection. This inhibitive energy can be overcome through surface heating, cooling aloft, lifting mechanisms (orographic, frontal, gravity waves, etc.) Convective Condensation Level - The height to which an air parcel possessing the average saturation mixing ratio in the lowest 4000 feet of the airmass, if heated sufficiently from below, will rise dry adiabatically until it just becomes saturated. It estimates the base of cumulus clouds that are produced by surface heating only. Convection Temperature (ConvectionT) - The surface temperature required to make the airmass dry adiabatic up to the given level. It can be considered a "trigger temperature" for that level. Freezing Level - The height where the temperature is zero degrees Celsius. Height of Stable Layer - The height (between 12,000 and 18,000 feet above mean sea level) where the smallest lapse rate exists. The location and existence of this feature is important in the generation of mountain waves. K Index - A measure of stability which combines the temperature difference between approximately 5,000 and 18,000 feet above the surface, the amount of moisture at approximately 5,000 feet above the surface, and a measure of the dryness at approximately 10,000 feet above the surface. Larger positive numbers indicate more instability and a greater likelihood of thunderstorm development. One interpretation of K index values regarding soaring in the western United States is given in WMO Technical Note 158 and is reproduced in the following table: below -10 no or weak thermals -10 to 5 dry thermals or 1/8 cumulus with moderate thermals 5 to 15 good soaring conditions 15 to 20 good soaring conditions with occasional showers 20 to 30 excellent soaring conditions, but increasing probability of showers and thunderstorms above 30 more than 60 percent probability of thunderstorms Lapse Rate - The change with height of the temperature. Negative values indicate inversions. Lifted Condensation Level - The height to which an air parcel possessing the average dew point in the lowest 4000 feet of the airmass and the forecast maximum temperature must be lifted dry adiabatically to attain saturation. Lifted Index (LI) - The difference between the environmental temperature at a level approximately 18,000 feet above the surface and the temperature of an air parcel lifted dry adiabatically from the surface to its lifted condensation level and then pseudoadiabatically thereafter to this same level. The parcel`s initial temperature is the forecast maximum temperature and its dew point is the average dew point in the lowest 4000 feet of the airmass. Negative values are indicative of instability with positive values showing stable conditions. Lift Rate - An experimental estimate of the strength of thermals. It is computed the same way as the maximum rate of lift but uses the actual level rather than the maximum height of thermals in the calculation. Also, none of the empirical adjustments based on cloudiness and K-index are applied to these calculations. Maximum Height of Thermals - The height where the dry adiabat through the forecast maximum temperature intersects the environmental temperature. Maximum Rate of Lift - An estimate of the maximum strength of thermals. It is computed from an empirical formula which combines the expected maximum height of thermals with the difference in the environmental temperatures between the maximum height of thermals and the temperature 4,000 feet above the ground. After this computation, further empirical adjustments are made based on the value of the K-index and the amount and opacity of middle and high level cloudiness expected between the time of trigger temperature and the time of overdevelopment. Middle/High Clouds - The amount and opacity of middle (altostratus, altocumulus) or high (cirrus, cirrostratus, cirrocumulus) clouds. Broken means that between 60% and 90% of the sky is covered by the cloud, with overcast conditions occurring when more than 90% of the sky is covered by the cloud. Thin implies that the clouds are predominantly transparent, meaning that some sunlight is reaching the ground, in contrast to opaque which suggests that little sunlight is reaching the ground. Potential Height of Wave - The minimum of the following two heights: 1. Level above the height of stable layer (or 14,000 feet if none exists) where the wind direction changes by 30 degrees or more 2. Level above the height of stable layer (or 14,000 feet if none exists) where the wind speed no longer increases with height PVA/NVA - Positive vorticity advection (PVA)/negative vorticity advection (NVA) on the 500 millibar isobaric surface (approximately 18,000 feet above mean sea level). Weak PVA has been shown to assist in mountain wave soaring. Soaring Window - The time between the time the trigger temperature is reached and the time of overdevelopment. Thermal Index - The difference between the environmental temperature and the temperature at a particular level determined by following the dry adiabat through the forecast maximum temperature up to that level. Negative values are indicative of thermal lift. Thermal Soaring Index - An adjective rating (for sailplanes) based on the computed maximum rate of lift, and the wind speed and middle and high cloud cover expected during the soaring window (the time of the trigger temperature and the time of overdevelopment) according to the following: Maximum rate of lift Adjective Rating >= 800 fpm Excellent >= 400 and < 800 fpm Good >= 200 and < 400 fpm Fair < 200 fpm Poor Time of Overdevelopment - The time one or more of the following phenomena, which essentially shut off thermal lift, is expected to occur: 1. formation of broken to overcast convective cloud cover 2. formation of scattered to numerous downbursts 3. initiation of widespread precipitation Time of Trigger Temperature - The time the surface temperature is expected to reach the trigger temperature. Trigger Temperature - The surface temperature required to make the first 4000 feet of the atmosphere dry adiabatic. Wave Soaring Index - An empirical, adjective rating (for sailplanes) which attempts to combine a variety of phenomena important in mountain wave soaring into a single index number. Objective points are assigned to these phenomena: wind speed and direction at 14,000 ft MSL, the static stability in the 12,000-18,000 ft MSL layer, the wind speed gradient above the stable layer, jet stream location and frontal and upper trough movements. 042613