560  
UXUS97 KBOU 301242  
SRGBOU  
 
SOARING FORECAST  
NATIONAL WEATHER SERVICE DENVER/BOULDER, COLORADO  
0642 MDT SUNDAY, APRIL 30, 2017  
 
THIS FORECAST IS FOR SUNDAY, APRIL 30, 2017:  
 
IF THE TRIGGER TEMPERATURE OF 39.8 F/4.4 C IS REACHED...THEN  
THERMAL SOARING INDEX....................... POOR  
MAXIMUM RATE OF LIFT........................ 273 FT/MIN (1.4 M/S)  
MAXIMUM HEIGHT OF THERMALS.................. 12527 FT MSL (7242 FT AGL)  
 
FORECAST MAXIMUM TEMPERATURE................... 52.0 F/11.6 C  
TIME OF TRIGGER TEMPERATURE.................... 1030 MDT  
TIME OF OVERDEVELOPMENT........................ NONE  
MIDDLE/HIGH CLOUDS DURING SOARING WINDOW....... OVERCAST OPAQUE HIGH  
SURFACE WINDS DURING SOARING WINDOW............ BETWEEN 20 MPH AND 30 MPH  
HEIGHT OF THE -3 THERMAL INDEX................. 10594 FT MSL (5309 FT AGL)  
THERMAL SOARING OUTLOOK FOR MONDAY 05/01....... GOOD  
 
WAVE SOARING INDEX............................. POOR  
WAVE SOARING INDEX TREND (TO 1800 MDT)......... LITTLE CHANGE  
HEIGHT OF STABLE LAYER (12-18K FT MSL)......... 11924 FT MSL (6639 FT AGL)  
WEAK PVA/NVA (THROUGH 1800 MDT)................ NEITHER  
POTENTIAL HEIGHT OF WAVE....................... 18071 FT MSL (12786 FT AGL)  
WAVE SOARING OUTLOOK FOR MONDAY 05/01.......... EXCELLENT  
 
REMARKS... STRONG NORTHERLY FLOW AT THE SURFACE AND ALOFT TODAY AS A POTENT  
SPRING STORM SYSTEM LINGERS OVER WESTERN KANSAS.  
 
SUNRISE/SUNSET.................... 06:00:31 / 19:52:46 MDT  
TOTAL POSSIBLE SUNSHINE........... 13 HR 52 MIN 15 SEC (832 MIN 15 SEC)  
ALTITUDE OF SUN AT 12:56:39 MDT... 65.21 DEGREES  
 
UPPER AIR DATA FROM RAWINSONDE OBSERVATION TAKEN ON 04/30/2017 AT 0600 MDT  
 
FREEZING LEVEL.................. ENTIRE AIRMASS BELOW 32 F / 0 C  
CONVECTIVE CONDENSATION LEVEL... 19731 FT MSL (14446 FT AGL)  
LIFTED CONDENSATION LEVEL....... 15648 FT MSL (10363 FT AGL)  
LIFTED INDEX.................... +9.2  
K INDEX......................... -22.1  
 
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 -53.4 -64.1 290 21 11 1.7 0.9 111.4 232.6 57.3 M M  
45000 -52.6 -62.7 315 14 7 -2.0 -1.1 88.1 190.6 47.0 M M  
40000 -51.3 -60.3 340 14 7 -2.9 -1.6 65.8 150.5 35.8 M M  
38000 -52.8 -63.0 335 15 8 -1.9 -1.0 54.8 130.6 29.3 M M  
36000 -53.9 -65.0 025 5 3 -2.5 -1.4 44.5 112.1 23.1 M M  
34000 -50.4 -58.7 140 19 10 7.3 4.0 41.2 106.1 21.3 M M  
32000 -48.0 -54.4 125 40 21 -21.0 -11.5 36.3 97.4 18.4 M M  
30000 -45.4 -49.7 120 44 23 9.0 4.9 32.0 89.5 15.5 M M  
29000 -42.1 -43.8 125 27 14 9.1 5.0 31.5 88.7 15.4 M M  
28000 -40.1 -40.2 135 13 7 5.6 3.1 30.3 86.5 14.7 M M  
27000 -38.4 -37.1 020 1 1 6.9 3.8 28.8 83.8 13.7 M M  
26000 -36.3 -33.3 345 6 3 6.8 3.7 27.6 81.7 13.0 M M  
25000 -34.2 -29.6 340 11 6 8.1 4.5 26.7 80.1 12.4 M M  
24000 -31.7 -25.1 360 14 7 8.8 4.8 26.1 79.0 12.1 M M  
23000 -29.3 -20.7 355 19 10 7.7 4.2 25.5 77.8 11.7 M M  
22000 -26.9 -16.4 355 24 13 8.5 4.7 24.9 76.8 11.3 M M  
21000 -24.4 -11.9 350 30 15 6.8 3.8 24.3 75.8 11.0 M M  
20000 -22.3 -8.1 350 35 18 7.0 3.8 23.4 74.1 10.3 M M  
19500 -21.2 -6.2 350 37 19 7.0 3.8 22.8 73.1 10.0 M M  
19000 -20.2 -4.4 355 39 20 7.0 3.9 22.4 72.2 9.6 M M  
18500 -19.2 -2.6 355 41 21 5.3 2.9 21.8 71.3 9.2 M M  
18000 -18.6 -1.5 355 43 22 3.6 2.0 20.8 69.5 8.4 M M  
17500 -18.1 -0.6 360 42 22 3.6 2.0 19.8 67.6 7.5 M M  
17000 -17.5 0.5 010 42 22 3.6 2.0 18.7 65.7 6.6 M M  
16500 -17.0 1.4 010 42 22 3.1 1.7 17.7 63.8 5.7 M M  
16000 -16.1 3.0 010 42 22 8.8 4.8 17.0 62.6 5.2 M M  
15500 -14.8 5.4 010 42 22 8.7 4.7 16.8 62.2 5.0 M M  
15000 -13.5 7.7 010 42 21 9.1 5.0 16.6 61.9 4.9 M M  
14500 -12.4 9.7 015 41 21 2.7 1.5 15.5 59.9 3.9 M M  
14000 -11.9 10.6 015 41 21 2.8 1.5 14.4 57.9 2.9 M M  
13500 -11.5 11.3 010 38 20 2.9 1.6 13.2 55.8 1.9 M M  
13000 -11.1 12.0 005 37 19 2.9 1.6 12.1 53.8 0.8 M M  
12500 -10.7 12.7 355 37 19 2.9 1.6 11.0 51.8 -0.2 467 2.4  
12000 -10.3 13.5 350 38 19 2.6 1.4 9.9 49.8 -1.3 440 2.2  
11500 -9.7 14.5 345 37 19 7.1 3.9 9.1 48.4 -2.1 405 2.1  
11000 -8.6 16.5 340 36 19 7.3 4.0 8.6 47.5 -2.5 360 1.8  
10500 -7.9 17.8 345 37 19 0.2 0.1 7.8 46.1 -3.3 325 1.6  
10250 -8.0 17.6 345 37 19 -1.8 -1.0 7.0 44.5 -4.1 319 1.6  
10000 -8.1 17.4 345 38 20 0.5 0.3 6.1 43.0 -4.9 314 1.6  
9750 -7.9 17.8 345 37 19 3.1 1.7 5.5 41.9 -5.5 302 1.5  
9500 -7.7 18.1 350 36 19 2.0 1.1 5.0 40.9 -6.1 288 1.5  
9250 -7.5 18.5 350 36 18 5.4 2.9 4.4 39.9 -6.6 275 1.4  
9000 -6.9 19.6 355 35 18 9.0 4.9 4.3 39.7 -6.8 250 1.3  
8750 -6.3 20.7 355 35 18 8.4 4.6 4.2 39.5 -6.9 223 1.1  
8500 -5.6 21.9 360 35 18 8.6 4.7 4.1 39.4 -7.0 197 1.0  
8250 -5.0 23.0 360 36 18 8.5 4.7 4.0 39.2 -7.1 170 0.9  
8000 -4.4 24.1 360 36 19 8.6 4.7 3.9 39.1 -7.2 144 0.7  
7750 -3.7 25.3 360 35 18 8.6 4.7 3.8 38.9 -7.3 117 0.6  
7500 -3.1 26.4 360 34 18 8.6 4.7 3.7 38.7 -7.4 91 0.5  
7250 -2.5 27.5 360 34 17 8.6 4.7 3.6 38.6 -7.5 64 0.3  
7000 -1.8 28.8 360 33 17 8.6 4.7 3.6 38.4 -7.7 38 0.2  
6750 -1.2 29.8 360 29 15 8.5 4.7 3.5 38.2 -7.8 12 0.1  
6500 -0.7 30.7 360 26 13 4.1 2.2 3.3 37.9 -8.0 M M  
6250 -0.6 30.9 355 22 11 0.8 0.4 2.6 36.7 -8.7 M M  
6000 -0.5 31.1 355 18 9 1.9 1.0 2.0 35.6 -9.3 M M  
5750 -0.4 31.3 350 13 7 1.0 0.6 1.4 34.5 -10.0 M M  
5500 -0.6 30.9 330 7 4 -8.0 -4.4 0.5 32.9 -10.9 M M  
 
* * * * * * NUMERICAL WEATHER PREDICTION MODEL FORECAST DATA VALID * * * * * *  
 
04/30/2017 AT 0900 MDT | 04/30/2017 AT 1200 MDT  
|  
CAPE... 0.0 LI... +10.3 | CAPE... +1.9 LI... +7.6  
CINH... -0.0 K INDEX... -19.2 | CINH... -0.3 K INDEX... -17.9  
|  
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 -55.0 -67.0 295 7 4 1.4 0.8 | -55.4 -67.7 290 9 5 1.4 0.8  
45000 -52.9 -63.2 325 7 4 1.2 0.6 | -53.3 -63.9 305 9 5 1.0 0.6  
40000 -52.9 -63.2 340 13 7 -0.0 -0.0 | -53.6 -64.5 340 14 7 -0.2 -0.1  
38000 -53.0 -63.4 340 13 7 -0.6 -0.3 | -53.6 -64.5 345 16 8 0.1 0.0  
36000 -53.4 -64.1 340 10 5 -0.6 -0.3 | -53.6 -64.5 350 15 8 0.1 0.0  
34000 -53.4 -64.1 345 7 4 6.5 3.6 | -53.1 -63.6 350 14 7 7.6 4.2  
32000 -49.2 -56.6 055 3 1 6.9 3.8 | -48.7 -55.7 345 10 5 7.2 4.0  
30000 -45.0 -49.0 115 6 3 8.9 4.9 | -44.3 -47.7 340 7 4 9.0 5.0  
29000 -42.4 -44.3 110 4 2 8.6 4.7 | -41.6 -42.9 335 7 4 8.8 4.9  
28000 -39.8 -39.6 095 2 1 8.6 4.7 | -38.9 -38.0 330 7 4 8.8 4.9  
27000 -37.3 -35.1 360 1 1 8.7 4.8 | -36.3 -33.3 325 8 4 9.0 4.9  
26000 -34.8 -30.6 330 3 2 8.1 4.5 | -34.0 -29.2 340 10 5 7.4 4.1  
25000 -32.3 -26.1 330 6 3 8.1 4.5 | -31.7 -25.1 345 14 7 7.4 4.1  
24000 -29.9 -21.8 325 8 4 8.2 4.5 | -29.5 -21.1 350 18 9 7.5 4.1  
23000 -27.6 -17.7 335 11 6 7.0 3.8 | -27.4 -17.3 355 21 11 6.5 3.6  
22000 -25.6 -14.1 345 14 7 7.0 3.8 | -25.5 -13.9 360 23 12 6.5 3.6  
21000 -23.5 -10.3 350 17 9 7.1 3.9 | -23.5 -10.3 360 26 13 6.5 3.6  
20000 -21.8 -7.2 355 19 10 5.0 2.8 | -21.2 -6.2 360 26 13 6.1 3.4  
19500 -21.1 -6.0 355 19 10 5.1 2.8 | -20.2 -4.4 360 26 13 6.1 3.4  
19000 -19.9 -3.8 360 20 10 5.1 2.8 | -19.3 -2.7 360 26 13 6.1 3.3  
18500 -19.2 -2.6 360 21 11 5.0 2.8 | -18.4 -1.1 360 26 13 5.7 3.2  
18000 -18.4 -1.1 360 21 11 5.0 2.7 | -17.6 0.3 360 26 13 5.2 2.8  
17500 -17.6 0.3 360 21 11 5.0 2.7 | -16.8 1.8 360 25 13 5.3 2.9  
17000 -16.9 1.6 360 21 11 5.3 2.9 | -16.1 3.0 355 25 13 4.6 2.5  
16500 -16.1 3.0 360 21 11 5.3 2.9 | -15.4 4.3 355 25 13 4.6 2.5  
16000 -15.3 4.5 360 21 11 5.3 2.9 | -14.7 5.5 355 24 13 4.4 2.4  
15500 -14.5 5.9 360 21 11 5.3 2.9 | -14.1 6.6 355 24 12 4.3 2.4  
15000 -13.7 7.3 355 21 11 5.1 2.8 | -13.4 7.9 355 24 12 4.3 2.4  
14500 -13.0 8.6 355 21 11 4.8 2.6 | -12.8 9.0 350 23 12 4.3 2.4  
14000 -12.3 9.9 355 21 11 4.7 2.6 | -12.1 10.2 350 23 12 4.4 2.4  
13500 -11.7 10.9 350 22 11 4.0 2.2 | -11.5 11.3 350 23 12 4.5 2.5  
13000 -11.1 12.0 350 22 11 4.0 2.2 | -10.8 12.6 350 23 12 4.6 2.5  
12500 -10.5 13.1 350 22 11 3.6 2.0 | -10.1 13.8 345 23 12 5.4 3.0  
12000 -10.0 14.0 350 22 11 3.7 2.0 | -9.3 15.3 345 23 12 5.5 3.0  
11500 -9.4 15.1 350 21 11 4.1 2.3 | -8.4 16.9 345 22 11 6.7 3.7  
11000 -8.8 16.2 350 21 11 4.3 2.4 | -7.4 18.7 345 21 11 6.6 3.6  
10500 -8.0 17.6 350 20 11 5.9 3.2 | -6.5 20.3 345 20 10 6.4 3.5  
10250 -7.6 18.3 350 20 10 5.9 3.2 | -6.1 21.0 345 19 10 6.1 3.4  
10000 -7.2 19.0 350 20 10 5.4 2.9 | -5.6 21.9 345 19 10 7.3 4.0  
9750 -6.8 19.8 350 19 10 6.6 3.6 | -5.0 23.0 340 18 9 7.5 4.1  
9500 -6.2 20.8 355 19 10 8.0 4.4 | -4.6 23.7 340 17 9 6.4 3.5  
9250 -5.7 21.7 355 18 9 7.7 4.2 | -4.1 24.6 340 16 8 6.9 3.8  
9000 -5.1 22.8 355 18 9 7.4 4.1 | -3.6 25.5 340 15 8 6.1 3.4  
8750 -4.6 23.7 355 18 9 7.1 3.9 | -3.2 26.2 345 14 7 6.0 3.3  
8500 -4.0 24.8 355 17 9 7.4 4.0 | -2.7 27.1 345 13 6 6.6 3.6  
8250 -3.5 25.7 355 16 8 7.3 4.0 | -2.2 28.0 345 12 6 6.6 3.6  
8000 -2.9 26.8 355 16 8 8.2 4.5 | -1.8 28.8 345 11 5 7.0 3.8  
7750 -2.3 27.9 355 16 8 6.8 3.7 | -1.2 29.8 350 9 5 7.8 4.3  
7500 -1.9 28.6 355 15 8 5.6 3.1 | -0.6 30.9 350 9 5 8.3 4.6  
7250 -1.5 29.3 355 14 7 4.8 2.6 | -0.0 32.0 355 8 4 8.1 4.4  
7000 -1.2 29.8 350 13 7 3.8 2.1 | 0.5 32.9 355 8 4 7.7 4.2  
6750 -0.9 30.4 350 12 6 2.9 1.6 | 1.1 34.0 360 7 4 8.3 4.5  
6500 -0.8 30.6 350 10 5 1.4 0.8 | 1.8 35.2 360 7 4 8.6 4.7  
6250 -0.7 30.7 345 8 4 2.0 1.1 | 2.4 36.3 360 6 3 8.4 4.6  
6000 -0.6 30.9 345 6 3 1.1 0.6 | 3.0 37.4 005 6 3 8.0 4.4  
5750 -0.5 31.1 345 5 2 4.7 2.6 | 3.6 38.5 010 5 2 9.3 5.1  
5500 0.2 32.4 340 3 2 14.5 7.9 | 4.4 39.9 005 5 2 15.5 8.5  
 
04/30/2017 AT 1500 MDT | 04/30/2017 AT 1800 MDT  
|  
CAPE... +15.0 LI... +5.7 | CAPE... +11.4 LI... +3.5  
CINH... -9.0 K INDEX... -0.7 | CINH... -18.3 K INDEX... +10.6  
|  
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 -55.7 -68.3 290 11 6 0.8 0.4 | -56.0 -68.8 300 13 7 0.6 0.3  
45000 -54.5 -66.1 305 14 7 0.6 0.3 | -55.1 -67.2 310 19 10 0.4 0.2  
40000 -54.6 -66.3 325 16 8 -0.1 -0.1 | -55.4 -67.7 320 19 10 -0.2 -0.1  
38000 -54.2 -65.6 335 18 9 1.7 0.9 | -54.6 -66.3 325 20 10 2.7 1.5  
36000 -53.1 -63.6 340 19 10 1.7 0.9 | -53.0 -63.4 330 20 10 2.7 1.5  
34000 -51.7 -61.1 340 20 10 7.0 3.8 | -51.1 -60.0 330 21 11 6.3 3.4  
32000 -47.9 -54.2 345 19 10 6.4 3.5 | -47.6 -53.7 330 20 10 5.9 3.2  
30000 -43.9 -47.0 345 19 10 7.7 4.2 | -43.9 -47.0 330 19 10 7.8 4.3  
29000 -41.7 -43.1 345 20 10 7.6 4.2 | -41.6 -42.9 330 19 10 7.7 4.2  
28000 -39.4 -38.9 345 21 11 7.6 4.2 | -39.3 -38.7 330 19 10 7.7 4.2  
27000 -37.1 -34.8 345 22 11 7.6 4.2 | -37.0 -34.6 330 19 10 7.7 4.2  
26000 -34.7 -30.5 345 22 11 7.8 4.3 | -34.7 -30.5 330 19 10 7.6 4.2  
25000 -32.4 -26.3 350 23 12 7.8 4.3 | -32.4 -26.3 330 19 10 7.6 4.2  
24000 -30.0 -22.0 350 23 12 7.8 4.3 | -30.1 -22.2 330 19 10 7.6 4.2  
23000 -27.6 -17.7 350 23 12 7.9 4.4 | -27.8 -18.0 335 19 10 7.6 4.1  
22000 -25.3 -13.5 350 23 12 7.9 4.4 | -25.6 -14.1 335 19 10 7.6 4.1  
21000 -22.9 -9.2 350 23 12 7.8 4.3 | -23.3 -9.9 335 19 10 7.4 4.1  
20000 -20.3 -4.5 350 23 12 6.7 3.6 | -20.8 -5.4 335 20 10 6.7 3.7  
19500 -19.3 -2.7 350 24 12 6.7 3.6 | -19.8 -3.6 335 20 10 6.7 3.7  
19000 -18.3 -0.9 350 24 12 6.6 3.6 | -18.8 -1.8 335 21 11 6.7 3.7  
18500 -17.4 0.7 350 24 12 5.9 3.3 | -17.8 -0.0 335 21 11 6.0 3.3  
18000 -16.6 2.1 350 24 12 5.2 2.8 | -17.0 1.4 335 21 11 5.5 3.0  
17500 -15.8 3.6 350 24 12 5.2 2.9 | -16.1 3.0 335 21 11 5.5 3.0  
17000 -15.1 4.8 350 24 12 4.3 2.4 | -15.4 4.3 335 22 11 4.6 2.5  
16500 -14.5 5.9 350 24 12 4.4 2.4 | -14.7 5.5 335 22 11 4.7 2.6  
16000 -13.8 7.2 350 24 12 4.1 2.3 | -14.0 6.8 335 22 11 4.6 2.5  
15500 -13.2 8.2 350 24 12 4.0 2.2 | -13.3 8.1 340 21 11 4.6 2.5  
15000 -12.6 9.3 345 24 12 4.0 2.2 | -12.7 9.1 340 21 11 5.1 2.8  
14500 -12.0 10.4 345 23 12 3.9 2.2 | -11.8 10.8 340 21 11 5.7 3.1  
14000 -11.4 11.5 345 23 12 4.2 2.3 | -11.0 12.2 340 21 11 6.2 3.4  
13500 -10.7 12.7 345 22 12 5.1 2.8 | -10.0 14.0 335 20 10 7.4 4.0  
13000 -10.0 14.0 345 22 11 5.2 2.9 | -8.9 16.0 335 20 10 7.5 4.1  
12500 -9.1 15.6 340 21 11 6.5 3.5 | -7.7 18.1 335 19 10 8.0 4.4  
12000 -8.2 17.2 340 20 10 6.6 3.6 | -6.6 20.1 335 19 10 8.1 4.4  
11500 -7.1 19.2 335 19 10 8.2 4.5 | -5.3 22.5 330 18 9 8.6 4.7  
11000 -6.0 21.2 335 17 9 8.3 4.5 | -4.1 24.6 330 18 9 8.6 4.7  
10500 -4.7 23.5 335 16 8 8.9 4.9 | -2.8 27.0 330 17 9 8.6 4.7  
10250 -4.1 24.6 335 16 8 8.9 4.9 | -2.2 28.0 325 17 9 8.6 4.7  
10000 -3.4 25.9 335 15 8 8.8 4.8 | -1.5 29.3 325 16 8 8.8 4.8  
9750 -2.8 27.0 335 15 8 9.0 5.0 | -0.9 30.4 325 16 8 8.8 4.8  
9500 -2.1 28.2 335 14 7 9.4 5.2 | -0.2 31.6 325 16 8 8.9 4.9  
9250 -1.4 29.5 335 14 7 9.0 4.9 | 0.4 32.7 325 16 8 8.5 4.6  
9000 -0.7 30.7 335 14 7 10.4 5.7 | 1.1 34.0 325 15 8 10.1 5.5  
8750 0.1 32.2 335 14 7 10.3 5.7 | 1.9 35.4 330 15 7 9.9 5.4  
8500 0.8 33.4 340 13 7 8.9 4.9 | 2.5 36.5 330 14 7 8.2 4.5  
8250 1.5 34.7 340 13 7 9.2 5.1 | 3.2 37.8 330 14 7 8.7 4.8  
8000 2.2 36.0 340 12 6 8.7 4.8 | 3.8 38.8 330 13 7 9.2 5.0  
7750 2.8 37.0 340 12 6 9.1 5.0 | 4.5 40.1 330 13 7 9.5 5.2  
7500 3.5 38.3 340 12 6 9.7 5.3 | 5.2 41.4 330 12 6 9.3 5.1  
7250 4.2 39.6 340 11 6 9.1 5.0 | 5.9 42.6 330 12 6 9.3 5.1  
7000 4.9 40.8 345 11 6 8.3 4.6 | 6.6 43.9 335 12 6 9.3 5.1  
6750 5.5 41.9 345 11 5 8.8 4.8 | 7.3 45.1 335 11 6 9.1 5.0  
6500 6.2 43.2 345 10 5 9.3 5.1 | 7.9 46.2 335 11 5 8.9 4.9  
6250 6.8 44.2 345 9 5 9.2 5.0 | 8.6 47.5 335 10 5 9.1 5.0  
6000 7.5 45.5 345 8 4 9.9 5.4 | 9.3 48.7 335 9 5 9.8 5.4  
5750 8.2 46.8 345 8 4 7.6 4.2 | 9.9 49.8 335 8 4 7.6 4.2  
5500 8.6 47.5 340 6 3 7.7 4.2 | 10.3 50.5 335 7 4 3.0 1.7  
________________________________________________________________________________  
 
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