751  
UXUS97 KBOU 240129  
SRGBOU  
 
SOARING FORECAST  
NATIONAL WEATHER SERVICE DENVER/BOULDER, COLORADO  
1922 MDT SUNDAY, SEPTEMBER 23, 2018  
 
THIS FORECAST IS FOR MONDAY, SEPTEMBER 24, 2018:  
 
IF THE TRIGGER TEMPERATURE OF 74.1 F/23.4 C IS REACHED...THEN  
THERMAL SOARING INDEX....................... GOOD  
MAXIMUM RATE OF LIFT........................ 676 FT/MIN (3.4 M/S)  
MAXIMUM HEIGHT OF THERMALS.................. 15140 FT MSL (9790 FT AGL)  
 
FORECAST MAXIMUM TEMPERATURE................... 80.0 F/27.1 C  
TIME OF TRIGGER TEMPERATURE.................... 1145 MDT  
TIME OF OVERDEVELOPMENT........................ NONE  
MIDDLE/HIGH CLOUDS DURING SOARING WINDOW....... BROKEN/OVERCAST OPAQUE MIDDLE  
SURFACE WINDS DURING SOARING WINDOW............ 20 MPH OR LESS  
HEIGHT OF THE -3 THERMAL INDEX................. 9579 FT MSL (4230 FT AGL)  
THERMAL SOARING OUTLOOK FOR TUESDAY 09/25...... FAIR  
 
WAVE SOARING INDEX............................. POOR  
WAVE SOARING INDEX TREND (TO 1800 MDT)......... SLIGHT IMPROVEMENT AFTER MID-MOR  
HEIGHT OF STABLE LAYER (12-18K FT MSL)......... NONE  
WEAK PVA/NVA (THROUGH 1800 MDT)................ WEAK PVA  
POTENTIAL HEIGHT OF WAVE....................... 45783 FT MSL (40433 FT AGL)  
WAVE SOARING OUTLOOK FOR TUESDAY 09/25......... POOR  
 
REMARKS... WEAK UPPER LEVEL TROUGH WILL PASS OVER THE FORECAST AREA LATE TONIGHT  
AND MONDAY MORNING. NOT MUCH PRECIPITATION WITH IT.  
 
***ATTENTION SOARING FORECAST USERS***THE NATIONAL WEATHER SERVICE IN BOULDER WANTS TO HEAR FROM YOU.  
PLEASE SEND AND EMAIL TO PAUL.T.SCHLATTER@NOAA.GOV AND LET US KNOW HOW YOU USE THE SOARING FORECAST. THANKS!  
 
SUNRISE/SUNSET.................... 06:49:17 / 18:53:37 MDT  
TOTAL POSSIBLE SUNSHINE........... 12 HR 4 MIN 20 SEC (724 MIN 20 SEC)  
ALTITUDE OF SUN AT 12:51:27 MDT... 49.53 DEGREES  
 
UPPER AIR DATA FROM NUMERICAL MODEL FORECAST VALID ON 09/24/2018 AT 0600 MDT  
 
FREEZING LEVEL.................. 14022 FT MSL (8672 FT AGL)  
CONVECTIVE CONDENSATION LEVEL... 15686 FT MSL (10336 FT AGL)  
LIFTED CONDENSATION LEVEL....... 15626 FT MSL (10277 FT AGL)  
LIFTED INDEX.................... -1.4  
K INDEX......................... +26.0  
 
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 -59.8 -75.6 265 32 16 0.9 0.5 M M M M M  
45000 -58.4 -73.1 260 42 22 1.0 0.5 M M M M M  
40000 -57.0 -70.6 255 46 24 0.9 0.5 M M M M M  
38000 -53.2 -63.8 255 43 22 6.1 3.3 M M M M M  
36000 -49.5 -57.1 250 40 21 6.1 3.3 M M M M M  
34000 -45.2 -49.4 250 37 19 7.8 4.3 M M M M M  
32000 -40.5 -40.9 250 33 17 7.8 4.3 M M M M M  
30000 -35.9 -32.6 250 29 15 7.5 4.1 39.8 103.6 9.9 M M  
29000 -33.6 -28.5 250 27 14 7.5 4.1 38.9 102.0 9.3 M M  
28000 -31.4 -24.5 250 26 13 7.5 4.1 38.2 100.7 8.9 M M  
27000 -29.1 -20.4 250 24 12 7.5 4.1 37.3 99.1 8.3 M M  
26000 -26.9 -16.4 250 22 11 7.5 4.1 36.4 97.5 7.6 M M  
25000 -24.6 -12.3 245 20 10 7.5 4.1 35.6 96.1 7.1 M M  
24000 -22.4 -8.3 245 18 9 7.2 3.9 34.8 94.6 6.5 M M  
23000 -20.3 -4.5 240 16 8 7.2 3.9 33.8 92.8 5.7 M M  
22000 -18.1 -0.6 235 15 7 7.2 4.0 32.9 91.2 5.0 M M  
21000 -15.5 4.1 235 13 7 7.4 4.0 31.8 89.2 4.1 M M  
20000 -13.3 8.1 240 13 7 7.4 4.1 30.9 87.7 3.4 M M  
19500 -12.2 10.0 240 13 7 7.4 4.1 30.5 87.0 3.0 M M  
19000 -11.1 12.0 240 13 7 7.3 4.0 30.2 86.3 2.7 M M  
18500 -10.1 13.8 240 13 7 7.2 4.0 29.7 85.5 2.3 M M  
18000 -9.0 15.8 240 13 7 7.3 4.0 29.3 84.7 1.9 M M  
17500 -7.9 17.8 245 13 7 7.8 4.3 28.9 84.1 1.6 M M  
17000 -6.8 19.8 245 13 7 7.8 4.3 28.6 83.4 1.2 M M  
16500 -5.6 21.9 250 14 7 7.6 4.2 28.2 82.8 0.9 M M  
16000 -4.5 23.9 250 14 7 7.7 4.2 27.9 82.2 0.5 M M  
15500 -3.4 25.9 250 14 7 7.8 4.3 27.5 81.6 0.2 M M  
15000 -2.3 27.9 250 13 7 8.1 4.4 27.2 81.0 -0.1 859 4.4  
14500 -1.1 30.0 250 13 7 8.1 4.4 27.0 80.5 -0.4 808 4.1  
14000 0.1 32.2 250 13 7 8.2 4.5 26.7 80.0 -0.7 758 3.9  
13500 1.3 34.3 250 12 6 8.2 4.5 26.4 79.6 -1.0 708 3.6  
13000 2.5 36.5 255 11 6 8.2 4.5 26.2 79.1 -1.2 658 3.3  
12500 3.7 38.7 255 10 5 8.2 4.5 25.9 78.7 -1.5 607 3.1  
12000 4.9 40.8 255 9 5 9.0 4.9 25.7 78.3 -1.7 554 2.8  
11500 6.3 43.3 260 8 4 9.1 5.0 25.6 78.1 -1.9 499 2.5  
11000 7.5 45.5 260 7 4 7.7 4.2 25.4 77.8 -2.1 447 2.3  
10500 8.7 47.7 260 6 3 7.3 4.0 25.1 77.1 -2.4 398 2.0  
10250 9.2 48.6 260 5 3 8.5 4.7 24.9 76.8 -2.6 374 1.9  
10000 9.9 49.8 260 4 2 8.3 4.6 24.8 76.7 -2.6 347 1.8  
9750 10.4 50.7 265 4 2 6.9 3.8 24.6 76.4 -2.8 323 1.6  
9500 11.0 51.8 275 3 1 7.6 4.2 24.5 76.0 -3.0 299 1.5  
9250 11.5 52.7 290 2 1 6.2 3.4 24.3 75.7 -3.2 275 1.4  
9000 11.9 53.4 305 2 1 5.5 3.0 23.9 75.1 -3.5 256 1.3  
8750 12.4 54.3 325 3 1 6.2 3.4 23.6 74.6 -3.8 234 1.2  
8500 12.8 55.0 345 3 2 6.5 3.5 23.4 74.1 -4.1 213 1.1  
8250 13.3 55.9 355 4 2 4.9 2.7 23.1 73.6 -4.4 192 1.0  
8000 13.6 56.5 005 5 2 3.3 1.8 22.6 72.7 -4.9 177 0.9  
7750 13.8 56.8 010 6 3 4.0 2.2 22.2 71.9 -5.3 161 0.8  
7500 14.1 57.4 015 7 4 3.8 2.1 21.7 71.1 -5.8 145 0.7  
7250 14.4 57.9 015 8 4 2.7 1.5 21.2 70.2 -6.3 130 0.7  
7000 14.6 58.3 015 9 5 2.1 1.2 20.6 69.2 -6.9 118 0.6  
6750 14.7 58.5 020 10 5 1.9 1.1 20.1 68.1 -7.4 106 0.5  
6500 14.9 58.8 020 11 6 2.8 1.5 19.5 67.1 -8.1 94 0.5  
6250 15.1 59.2 020 10 5 4.2 2.3 19.0 66.2 -8.5 78 0.4  
6000 15.5 59.9 025 9 5 4.3 2.4 18.6 65.5 -9.0 61 0.3  
5750 15.8 60.4 025 8 4 4.7 2.6 18.2 64.8 -9.4 44 0.2  
5500 16.0 60.8 030 6 3 1.6 0.9 17.8 64.0 -9.9 28 0.1  
 
* * * * * * NUMERICAL WEATHER PREDICTION MODEL FORECAST DATA VALID * * * * * *  
 
09/24/2018 AT 0900 MDT | 09/24/2018 AT 1200 MDT  
|  
CAPE... 0.0 LI... +0.1 | CAPE... +89.7 LI... -1.3  
CINH... -0.1 K INDEX... +23.4 | CINH... -55.5 K INDEX... +26.0  
|  
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 -59.9 -75.8 265 31 16 1.0 0.6 | -59.6 -75.3 260 31 16 0.3 0.2  
45000 -58.3 -72.9 260 41 21 1.4 0.8 | -58.7 -73.7 260 39 20 2.1 1.2  
40000 -56.2 -69.2 255 43 22 1.3 0.7 | -55.5 -67.9 255 39 20 1.9 1.1  
38000 -52.8 -63.0 255 42 21 5.4 3.0 | -52.5 -62.5 255 39 20 5.3 2.9  
36000 -49.5 -57.1 255 40 20 5.4 3.0 | -48.9 -56.0 250 38 20 5.3 2.9  
34000 -45.4 -49.7 250 37 19 7.8 4.3 | -45.0 -49.0 250 36 19 7.1 3.9  
32000 -40.7 -41.3 255 35 18 7.8 4.3 | -40.8 -41.4 250 34 17 7.1 3.9  
30000 -36.1 -33.0 250 32 16 7.8 4.3 | -36.4 -33.5 250 31 16 7.5 4.1  
29000 -33.7 -28.7 250 30 15 7.8 4.3 | -34.2 -29.6 250 29 15 7.5 4.1  
28000 -31.4 -24.5 250 28 15 7.8 4.3 | -31.9 -25.4 250 28 14 7.5 4.1  
27000 -29.1 -20.4 250 27 14 7.6 4.2 | -29.7 -21.5 255 26 14 7.6 4.2  
26000 -26.9 -16.4 250 25 13 7.6 4.2 | -27.4 -17.3 255 25 13 7.6 4.2  
25000 -24.6 -12.3 250 23 12 7.6 4.1 | -25.1 -13.2 255 25 13 7.6 4.2  
24000 -22.4 -8.3 245 21 11 7.2 4.0 | -22.9 -9.2 255 24 12 7.2 3.9  
23000 -20.2 -4.4 250 20 10 7.3 4.0 | -20.8 -5.4 260 23 12 7.2 4.0  
22000 -18.0 -0.4 250 19 10 7.3 4.0 | -18.6 -1.5 260 22 11 7.2 4.0  
21000 -16.0 3.2 250 18 9 6.8 3.7 | -16.6 2.1 260 21 11 6.2 3.4  
20000 -13.5 7.7 255 17 9 6.8 3.7 | -14.4 6.1 260 20 10 6.2 3.4  
19500 -12.5 9.5 255 17 9 6.8 3.7 | -13.5 7.7 265 19 10 6.2 3.4  
19000 -11.5 11.3 255 16 8 7.1 3.9 | -12.5 9.5 265 19 10 6.9 3.8  
18500 -10.4 13.3 260 17 9 7.2 4.0 | -11.5 11.3 265 19 10 7.2 3.9  
18000 -9.4 15.1 260 17 9 7.3 4.0 | -10.5 13.1 265 20 10 7.2 4.0  
17500 -8.3 17.1 260 17 9 7.4 4.1 | -9.4 15.1 265 19 10 7.5 4.1  
17000 -7.2 19.0 260 17 9 7.4 4.1 | -8.3 17.1 265 19 10 7.4 4.1  
16500 -6.1 21.0 260 17 9 7.7 4.2 | -7.2 19.0 265 18 9 8.2 4.5  
16000 -5.0 23.0 260 17 9 7.7 4.2 | -6.0 21.2 265 18 9 8.3 4.6  
15500 -3.9 25.0 265 17 9 7.7 4.2 | -4.8 23.4 270 18 9 8.5 4.7  
15000 -2.8 27.0 265 17 9 7.7 4.2 | -3.5 25.7 270 17 9 8.8 4.8  
14500 -1.7 28.9 265 16 8 7.7 4.2 | -2.2 28.0 270 16 8 8.8 4.8  
14000 -0.5 31.1 265 16 8 7.7 4.2 | -0.9 30.4 270 15 8 9.0 4.9  
13500 0.6 33.1 265 15 8 7.7 4.2 | 0.4 32.7 270 14 7 9.0 4.9  
13000 1.7 35.1 265 14 7 7.8 4.3 | 1.8 35.2 270 13 7 9.1 5.0  
12500 2.9 37.2 265 13 7 7.8 4.3 | 3.1 37.6 270 12 6 9.1 5.0  
12000 4.0 39.2 265 12 6 7.7 4.2 | 4.4 39.9 270 11 6 8.9 4.9  
11500 5.1 41.2 265 11 6 7.7 4.2 | 5.8 42.4 265 10 5 9.1 5.0  
11000 6.2 43.2 265 10 5 7.1 3.9 | 7.0 44.6 265 9 5 7.4 4.0  
10500 7.3 45.1 265 8 4 7.5 4.1 | 8.1 46.6 265 8 4 6.4 3.5  
10250 7.8 46.0 265 8 4 5.5 3.0 | 8.7 47.7 265 8 4 10.8 5.9  
10000 8.2 46.8 260 7 4 6.2 3.4 | 9.6 49.3 265 7 4 11.4 6.3  
9750 8.8 47.8 260 6 3 8.4 4.6 | 10.2 50.4 260 6 3 7.4 4.0  
9500 9.4 48.9 265 5 3 8.7 4.8 | 10.8 51.4 260 6 3 9.1 5.0  
9250 10.0 50.0 265 4 2 5.4 2.9 | 11.4 52.5 255 5 3 6.4 3.5  
9000 10.2 50.4 265 4 2 4.4 2.4 | 11.9 53.4 250 4 2 6.8 3.7  
8750 10.7 51.3 265 3 2 7.1 3.9 | 12.5 54.5 245 4 2 9.2 5.1  
8500 11.2 52.2 265 3 1 6.6 3.6 | 13.1 55.6 240 3 2 9.0 4.9  
8250 11.7 53.1 270 2 1 5.1 2.8 | 13.8 56.8 230 3 1 7.1 3.9  
8000 11.9 53.4 275 2 1 3.2 1.8 | 14.2 57.6 210 3 1 6.3 3.5  
7750 12.1 53.8 285 2 1 3.0 1.7 | 14.8 58.6 195 3 1 8.3 4.6  
7500 12.3 54.1 285 2 1 2.3 1.3 | 15.4 59.7 185 3 1 8.1 4.5  
7250 12.4 54.3 295 1 1 1.1 0.6 | 16.0 60.8 175 3 1 6.7 3.7  
7000 12.5 54.5 315 1 1 0.8 0.4 | 16.4 61.5 160 3 2 6.4 3.5  
6750 12.5 54.5 345 1 0 0.3 0.1 | 17.0 62.6 155 4 2 9.1 5.0  
6500 12.5 54.5 000 0 0 3.2 1.7 | 17.7 63.9 150 3 2 10.6 5.8  
6250 12.9 55.2 135 1 0 6.7 3.7 | 18.5 65.3 150 3 2 10.6 5.8  
6000 13.4 56.1 145 1 1 5.6 3.1 | 19.3 66.7 145 3 2 10.3 5.7  
5750 13.8 56.8 150 2 1 8.6 4.7 | 20.1 68.2 145 3 2 11.7 6.4  
5500 14.8 58.6 150 2 1 16.8 9.2 | 21.2 70.2 145 3 2 20.5 11.2  
 
09/24/2018 AT 1500 MDT | 09/24/2018 AT 1800 MDT  
|  
CAPE... +217.6 LI... -2.1 | CAPE... +159.2 LI... -2.2  
CINH... -10.2 K INDEX... +27.3 | CINH... -18.8 K INDEX... +24.8  
|  
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 -59.6 -75.3 260 29 15 1.5 0.8 | -60.0 -76.0 260 28 15 1.9 1.1  
45000 -57.3 -71.1 260 37 19 2.0 1.1 | -57.3 -71.1 265 35 18 1.4 0.8  
40000 -54.2 -65.6 265 37 19 3.3 1.8 | -55.1 -67.2 265 35 18 1.1 0.6  
38000 -51.3 -60.3 265 35 18 4.7 2.6 | -52.0 -61.6 265 34 17 5.1 2.8  
36000 -48.5 -55.3 270 33 17 4.7 2.6 | -48.9 -56.0 270 33 17 5.1 2.8  
34000 -44.9 -48.8 270 32 16 6.9 3.8 | -44.9 -48.8 270 32 17 7.6 4.2  
32000 -40.7 -41.3 265 31 16 6.9 3.8 | -40.3 -40.5 270 31 16 7.6 4.2  
30000 -36.5 -33.7 265 30 15 7.3 4.0 | -35.8 -32.4 270 30 15 7.6 4.2  
29000 -34.3 -29.7 265 29 15 7.3 4.0 | -33.5 -28.3 270 29 15 7.6 4.2  
28000 -32.1 -25.8 265 28 15 7.3 4.0 | -31.2 -24.2 270 29 15 7.6 4.2  
27000 -29.9 -21.8 265 28 14 7.5 4.1 | -29.0 -20.2 270 28 14 7.0 3.8  
26000 -27.7 -17.9 265 27 14 7.5 4.1 | -26.9 -16.4 275 27 14 7.0 3.8  
25000 -25.4 -13.7 265 26 13 7.5 4.1 | -24.9 -12.8 275 25 13 7.0 3.8  
24000 -23.3 -9.9 265 24 13 6.4 3.5 | -22.9 -9.2 275 24 12 5.5 3.0  
23000 -21.3 -6.3 265 23 12 6.5 3.6 | -21.3 -6.3 275 22 11 5.7 3.1  
22000 -19.4 -2.9 265 22 11 6.6 3.6 | -19.6 -3.3 270 20 11 5.8 3.2  
21000 -16.9 1.6 265 20 10 7.1 3.9 | -17.2 1.0 270 18 9 7.3 4.0  
20000 -14.8 5.4 260 19 10 7.2 3.9 | -15.1 4.8 265 16 8 7.3 4.0  
19500 -13.7 7.3 260 18 9 7.2 4.0 | -14.0 6.8 260 16 8 7.4 4.0  
19000 -12.7 9.1 260 17 9 7.9 4.3 | -12.9 8.8 260 15 8 8.1 4.5  
18500 -11.5 11.3 260 17 9 8.3 4.5 | -11.7 10.9 260 14 7 8.5 4.7  
18000 -10.3 13.5 260 16 8 8.3 4.6 | -10.5 13.1 260 13 7 8.6 4.7  
17500 -9.1 15.6 260 15 8 8.1 4.4 | -9.2 15.4 260 13 7 8.5 4.7  
17000 -7.9 17.8 260 14 7 8.1 4.5 | -7.9 17.8 260 12 6 8.5 4.7  
16500 -6.7 19.9 260 14 7 8.7 4.8 | -6.6 20.1 260 11 6 9.2 5.1  
16000 -5.4 22.3 260 13 7 8.8 4.8 | -5.2 22.6 260 11 6 9.4 5.1  
15500 -4.1 24.6 260 12 6 9.0 5.0 | -3.8 25.2 265 11 5 9.4 5.2  
15000 -2.7 27.1 260 12 6 9.4 5.2 | -2.4 27.7 265 10 5 9.6 5.2  
14500 -1.3 29.7 260 11 6 9.4 5.2 | -1.0 30.2 270 9 5 9.5 5.2  
14000 0.1 32.2 260 10 5 9.4 5.2 | 0.4 32.7 270 9 4 9.1 5.0  
13500 1.5 34.7 260 10 5 9.5 5.2 | 1.8 35.2 275 8 4 9.2 5.0  
13000 2.9 37.2 260 9 5 9.2 5.1 | 3.1 37.6 275 7 4 9.1 5.0  
12500 4.3 39.7 260 8 4 9.2 5.1 | 4.5 40.1 280 7 3 9.2 5.0  
12000 5.7 42.3 260 7 4 9.4 5.2 | 5.8 42.4 285 6 3 9.0 5.0  
11500 7.0 44.6 260 7 3 9.5 5.2 | 7.2 45.0 290 6 3 9.1 5.0  
11000 8.4 47.1 260 6 3 8.3 4.6 | 8.5 47.3 290 5 3 8.7 4.8  
10500 9.6 49.3 255 5 3 8.0 4.4 | 9.8 49.6 295 5 3 8.6 4.7  
10250 10.2 50.4 255 4 2 10.6 5.8 | 10.5 50.9 300 5 3 11.3 6.2  
10000 11.1 52.0 250 4 2 10.6 5.8 | 11.4 52.5 300 5 2 11.2 6.1  
9750 11.8 53.2 250 3 2 8.3 4.6 | 12.1 53.8 305 5 2 8.9 4.9  
9500 12.4 54.3 245 3 2 9.3 5.1 | 12.8 55.0 305 5 2 9.8 5.4  
9250 13.1 55.6 245 3 1 7.6 4.2 | 13.5 56.3 310 5 2 8.5 4.7  
9000 13.6 56.5 245 2 1 8.4 4.6 | 14.1 57.4 310 4 2 9.2 5.0  
8750 14.4 57.9 240 2 1 10.7 5.9 | 14.8 58.6 315 4 2 10.8 5.9  
8500 15.1 59.2 240 2 1 9.9 5.5 | 15.6 60.1 320 4 2 10.3 5.7  
8250 15.9 60.6 235 2 1 10.8 5.9 | 16.4 61.5 320 4 2 10.5 5.8  
8000 16.7 62.1 235 2 1 10.4 5.7 | 17.2 63.0 325 4 2 9.9 5.4  
7750 17.4 63.3 230 2 1 9.3 5.1 | 17.9 64.2 330 4 2 9.2 5.1  
7500 18.1 64.6 225 1 1 9.3 5.1 | 18.6 65.5 330 4 2 9.2 5.0  
7250 18.8 65.8 225 1 1 10.6 5.8 | 19.3 66.7 335 4 2 10.3 5.7  
7000 19.7 67.5 220 1 1 11.2 6.1 | 20.1 68.2 340 4 2 10.7 5.9  
6750 20.4 68.7 215 1 1 9.1 5.0 | 20.8 69.4 340 4 2 8.8 4.8  
6500 21.1 70.0 210 1 1 8.9 4.9 | 21.4 70.5 345 4 2 8.5 4.6  
6250 21.8 71.2 210 1 0 10.4 5.7 | 22.1 71.8 345 4 2 9.8 5.4  
6000 22.6 72.7 205 1 0 11.2 6.1 | 22.9 73.2 350 4 2 10.2 5.6  
5750 23.4 74.1 200 1 0 9.0 4.9 | 23.6 74.5 350 4 2 9.6 5.3  
5500 24.1 75.4 195 1 0 11.0 6.1 | 24.3 75.7 350 3 2 8.8 4.8  
________________________________________________________________________________  
 
THIS PRODUCT IS ISSUED TWICE PER DAY, ONCE BY APPROXIMATELY 0630 MST/0730 MDT  
(1330 UTC) AND AGAIN BY APPROXIMATELY 1830 MST/1930 MDT (0130 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 OLD STAPLETON  
AIRPORT SITE IN DENVER, COLORADO AT  
 
NORTH LATITUDE: 39 DEG 46 MIN 5.016 SEC  
WEST LONGITUDE: 104 DEG 52 MIN 9.984 SEC  
ELEVATION: 5285 FEET (1611 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.  
 
CINH (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  
 
CLICK HERE TO GO TO PREVIOUS BULLETINS.

The Nexlab CO Page Main Text Page