761  
UXUS97 KGJT 141307  
SRGGJT  
 
SOARING FORECAST  
NATIONAL WEATHER SERVICE GRAND JUNCTION, COLORADO  
607 AM MST WEDNESDAY, JANUARY 14, 2026  
 
THIS FORECAST IS FOR WEDNESDAY, JANUARY 14, 2026:  
 
IF THE TRIGGER TEMPERATURE OF 58.2 F/14.5 C IS REACHED...THEN  
THERMAL SOARING INDEX....................... FAIR  
MAXIMUM RATE OF LIFT........................ 226 FT/MIN (1.1 M/S)  
MAXIMUM HEIGHT OF THERMALS.................. 7979 FT MSL (2372 FT AGL)  
 
FORECAST MAXIMUM TEMPERATURE................... 50.0 F/10.5 C  
TIME OF TRIGGER TEMPERATURE.................... NONE  
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................. 6796 FT MSL (1189 FT AGL)  
THERMAL SOARING OUTLOOK FOR THURSDAY 01/15..... FAIR  
 
WAVE SOARING INDEX............................. NOT AVAILABLE  
 
REMARKS...  
 
SUNRISE/SUNSET.................... 07:31:59 / 17:14:36 MST  
TOTAL POSSIBLE SUNSHINE........... 9 HR 42 MIN 37 SEC (582 MIN 37 SEC)  
ALTITUDE OF SUN AT 12:23:17 MST... 29.44 DEGREES  
 
UPPER AIR DATA FROM RAWINSONDE OBSERVATION TAKEN ON 01/14/2026 AT 0500 MST  
 
FREEZING LEVEL.................. 5636 FT MSL (29 FT AGL)  
ADDITIONAL FREEZING LEVEL....... 11950 FT MSL (6343 FT AGL)  
CONVECTIVE CONDENSATION LEVEL... 19903 FT MSL (14296 FT AGL)  
LIFTED CONDENSATION LEVEL....... 12878 FT MSL (7271 FT AGL)  
LIFTED INDEX.................... +12.5  
K INDEX......................... -23.8  
 
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 -65.7 -86.3 325 30 16 3.8 2.1 M M M M M  
45000 -59.7 -75.5 320 36 19 4.1 2.2 M M M M M  
40000 -53.6 -64.5 300 52 27 4.3 2.3 M M M M M  
38000 -52.1 -61.8 305 55 28 2.2 1.2 M M M M M  
36000 -50.8 -59.4 315 57 29 2.2 1.2 M M M M M  
34000 -48.2 -54.8 315 60 31 7.1 3.9 M M M M M  
32000 -43.4 -46.1 320 62 32 7.1 3.9 M M M M M  
30000 -39.2 -38.6 320 61 31 7.0 3.8 35.8 96.4 19.5 M M  
29000 -37.1 -34.8 320 59 30 7.0 3.8 34.7 94.4 18.9 M M  
28000 -35.0 -31.0 320 57 29 7.0 3.8 33.7 92.7 18.4 M M  
27000 -32.7 -26.9 320 55 29 8.4 4.6 33.0 91.4 18.0 M M  
26000 -30.2 -22.4 320 54 28 8.5 4.6 32.4 90.4 17.8 M M  
25000 -27.6 -17.7 320 53 27 8.4 4.6 32.0 89.6 17.7 M M  
24000 -25.1 -13.2 320 51 26 8.1 4.4 31.5 88.7 17.5 M M  
23000 -22.7 -8.9 325 48 25 8.1 4.4 30.8 87.5 17.1 M M  
22000 -20.3 -4.5 325 46 23 8.1 4.4 30.3 86.5 16.9 M M  
21000 -17.9 -0.2 325 44 23 8.1 4.5 29.7 85.4 16.6 M M  
20000 -15.4 4.3 325 43 22 8.1 4.5 29.1 84.3 16.3 M M  
19500 -14.2 6.4 325 42 22 8.1 4.4 28.8 83.9 16.1 M M  
19000 -13.0 8.6 325 42 22 7.9 4.3 28.6 83.4 16.0 M M  
18500 -11.5 11.3 330 40 20 6.6 3.6 27.8 82.1 15.5 M M  
18000 -10.5 13.1 330 38 20 6.5 3.6 27.3 81.1 15.1 M M  
17500 -9.5 14.9 330 36 19 6.1 3.4 26.7 80.0 14.7 M M  
17000 -8.6 16.5 330 34 18 6.2 3.4 26.1 78.9 14.2 M M  
16500 -7.8 18.0 330 32 17 4.9 2.7 25.4 77.7 13.7 M M  
16000 -7.1 19.2 330 30 16 4.8 2.7 24.5 76.2 13.0 M M  
15500 -6.3 20.7 330 29 15 5.2 2.8 23.7 74.7 12.3 M M  
15000 -5.5 22.1 330 27 14 5.5 3.0 23.0 73.4 11.7 M M  
14500 -4.7 23.5 330 25 13 5.8 3.2 22.3 72.2 11.1 M M  
14000 -3.8 25.2 330 24 12 6.7 3.7 21.8 71.2 10.7 M M  
13500 -2.8 27.0 325 23 12 6.6 3.6 21.3 70.3 10.3 M M  
13000 -1.8 28.8 325 21 11 6.2 3.4 20.7 69.3 9.8 M M  
12500 -0.9 30.4 325 20 10 6.3 3.5 20.2 68.3 9.3 M M  
12000 -0.1 31.8 320 19 10 4.9 2.7 19.5 67.1 8.8 M M  
11500 0.7 33.3 315 17 9 5.1 2.8 18.7 65.7 8.1 M M  
11000 1.3 34.3 310 16 8 3.5 1.9 17.9 64.2 7.3 M M  
10500 1.8 35.2 305 14 7 2.6 1.4 16.9 62.4 6.4 M M  
10250 1.9 35.4 305 13 7 2.0 1.1 16.3 61.3 5.8 M M  
10000 2.1 35.8 300 12 6 3.0 1.6 15.7 60.3 5.3 M M  
9750 2.3 36.1 295 11 6 3.0 1.6 15.2 59.4 4.7 M M  
9500 2.5 36.5 290 10 5 2.2 1.2 14.7 58.4 4.2 M M  
9250 2.5 36.5 285 8 4 0.5 0.3 14.0 57.2 3.5 M M  
9000 2.6 36.7 285 7 4 1.2 0.7 13.3 55.9 2.8 M M  
8750 2.7 36.9 275 6 3 2.4 1.3 12.7 54.8 2.2 M M  
8500 2.8 37.0 265 5 2 1.4 0.8 12.1 53.8 1.6 M M  
8250 2.8 37.0 250 4 2 0.5 0.2 11.4 52.5 0.9 M M  
8000 2.9 37.2 230 3 1 1.0 0.6 10.7 51.2 0.2 M M  
7750 2.9 37.2 205 3 1 1.5 0.8 10.0 50.1 -0.4 219 1.1  
7500 3.0 37.4 185 3 2 2.0 1.1 9.4 49.0 -1.1 209 1.1  
7250 3.2 37.8 170 4 2 2.5 1.4 8.9 47.9 -1.6 197 1.0  
7000 3.4 38.1 165 4 2 2.0 1.1 8.3 46.9 -2.2 185 0.9  
6750 3.4 38.1 155 4 2 0.0 0.0 7.6 45.8 -2.9 175 0.9  
6500 3.3 37.9 150 4 2 -1.8 -1.0 6.8 44.3 -3.7 170 0.9  
6250 3.2 37.8 140 5 2 -1.2 -0.7 6.0 42.7 -4.6 167 0.8  
6000 3.1 37.6 135 5 3 -3.2 -1.8 5.1 41.2 -5.4 163 0.8  
5750 2.4 36.3 130 5 2 -18.2 -10.0 3.7 38.6 -6.9 177 0.9  
5500 M M M M M M M M M M M M  
5250 M M M M M M M M M M M M  
5000 M M M M M M M M M M M M  
 
* * * * * * NUMERICAL WEATHER PREDICTION MODEL FORECAST DATA VALID * * * * * *  
 
01/14/2026 AT 0800 MST | 01/14/2026 AT 1100 MST  
|  
CAPE... 0.0 LI... +7.5 | CAPE... 0.0 LI... +7.7  
CINH... 0.0 K INDEX... +3.0 | CINH... -0.3 K INDEX... +2.2  
|  
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 -63.5 -82.3 010 53 27 2.1 1.2 | -64.5 -84.1 010 49 25 1.6 0.9  
45000 -60.6 -77.1 015 69 36 0.4 0.2 | -61.9 -79.4 010 62 32 2.0 1.1  
40000 -60.0 -76.0 020 70 36 0.3 0.2 | -58.9 -74.0 015 62 32 2.3 1.2  
38000 -56.6 -69.9 015 70 36 6.4 3.5 | -55.7 -68.3 010 62 32 5.7 3.1  
36000 -52.7 -62.9 015 71 36 6.4 3.5 | -52.3 -62.1 005 62 32 5.7 3.1  
34000 -48.4 -55.1 015 70 36 7.9 4.4 | -48.1 -54.6 005 63 33 7.8 4.3  
32000 -43.6 -46.5 010 69 36 7.9 4.4 | -43.4 -46.1 005 65 34 7.8 4.3  
30000 -38.9 -38.0 010 67 35 7.8 4.3 | -38.5 -37.3 005 66 34 8.5 4.7  
29000 -36.6 -33.9 005 66 34 7.8 4.3 | -36.0 -32.8 005 66 34 8.5 4.7  
28000 -34.2 -29.6 005 64 33 7.8 4.3 | -33.4 -28.1 005 65 34 8.5 4.7  
27000 -31.9 -25.4 005 64 33 7.8 4.3 | -30.4 -22.7 005 64 33 7.6 4.2  
26000 -29.5 -21.1 005 64 33 7.8 4.3 | -28.1 -18.6 005 62 32 7.6 4.2  
25000 -26.6 -15.9 005 64 33 7.8 4.3 | -25.9 -14.6 360 60 31 7.6 4.2  
24000 -24.3 -11.7 005 63 32 7.6 4.2 | -23.6 -10.5 360 59 31 7.5 4.1  
23000 -22.0 -7.6 005 60 31 7.6 4.2 | -21.3 -6.3 360 59 31 7.5 4.1  
22000 -19.7 -3.5 005 58 30 7.8 4.3 | -19.1 -2.4 360 59 30 7.7 4.2  
21000 -17.7 0.1 005 55 29 6.3 3.5 | -17.1 1.2 360 57 29 6.4 3.5  
20000 -15.9 3.4 005 52 27 6.4 3.5 | -15.2 4.6 005 55 28 6.4 3.5  
19500 -14.9 5.2 005 51 26 6.4 3.5 | -14.2 6.4 005 53 27 6.4 3.5  
19000 -14.0 6.8 005 49 25 6.3 3.5 | -13.3 8.1 005 52 27 6.0 3.3  
18500 -13.0 8.6 005 48 25 6.3 3.5 | -12.4 9.7 005 50 26 5.8 3.2  
18000 -12.1 10.2 005 47 24 6.3 3.5 | -11.5 11.3 005 47 24 5.8 3.2  
17500 -11.2 11.8 005 46 24 5.8 3.2 | -10.7 12.7 005 45 23 5.3 2.9  
17000 -10.3 13.5 010 45 23 5.9 3.2 | -10.0 14.0 005 43 22 5.4 3.0  
16500 -9.5 14.9 010 45 23 5.4 2.9 | -9.2 15.4 005 41 21 5.4 3.0  
16000 -8.7 16.3 010 44 23 5.3 2.9 | -8.4 16.9 005 39 20 5.4 3.0  
15500 -7.9 17.8 010 43 22 5.3 2.9 | -7.6 18.3 010 38 20 5.4 3.0  
15000 -7.1 19.2 010 42 22 5.3 2.9 | -6.8 19.8 010 37 19 5.4 3.0  
14500 -6.3 20.7 015 42 21 5.1 2.8 | -6.0 21.2 015 36 19 5.3 2.9  
14000 -5.7 21.7 015 40 21 4.4 2.4 | -5.2 22.6 015 36 18 4.7 2.6  
13500 -5.0 23.0 015 38 20 4.4 2.4 | -4.6 23.7 015 35 18 4.7 2.6  
13000 -4.4 24.1 015 36 18 4.5 2.5 | -3.9 25.0 015 34 17 4.2 2.3  
12500 -3.7 25.3 015 33 17 4.5 2.5 | -3.3 26.1 015 32 17 4.3 2.3  
12000 -3.1 26.4 015 31 16 4.5 2.4 | -2.6 27.3 015 30 15 5.7 3.1  
11500 -2.4 27.7 015 28 15 4.4 2.4 | -1.8 28.8 015 27 14 5.6 3.1  
11000 -1.7 28.9 020 26 13 5.8 3.2 | -1.1 30.0 015 24 12 4.3 2.4  
10500 -0.9 30.4 020 24 12 5.7 3.1 | -0.4 31.3 020 21 11 4.4 2.4  
10250 -0.5 31.1 025 23 12 5.2 2.8 | -0.1 31.8 020 20 10 3.3 1.8  
10000 -0.1 31.8 025 22 11 5.0 2.7 | 0.1 32.2 020 19 10 3.5 1.9  
9750 0.3 32.5 025 21 11 5.4 3.0 | 0.4 32.7 020 17 9 4.8 2.7  
9500 0.7 33.3 025 20 10 5.2 2.8 | 0.8 33.4 025 16 8 4.7 2.6  
9250 1.0 33.8 030 19 10 4.7 2.6 | 1.1 34.0 025 15 8 4.2 2.3  
9000 1.7 35.1 030 17 9 3.4 1.8 | 1.4 34.5 030 14 7 4.1 2.2  
8750 1.9 35.4 030 15 8 2.7 1.5 | 2.0 35.6 030 12 6 4.0 2.2  
8500 2.1 35.8 035 14 7 2.9 1.6 | 2.3 36.1 035 11 6 4.1 2.2  
8250 2.3 36.1 035 13 7 3.3 1.8 | 2.6 36.7 035 10 5 4.3 2.3  
8000 2.6 36.7 035 12 6 1.5 0.8 | 2.9 37.2 040 9 5 3.1 1.7  
7750 2.6 36.7 035 10 5 1.2 0.7 | 3.1 37.6 040 8 4 2.3 1.3  
7500 2.8 37.0 040 9 5 2.9 1.6 | 3.3 37.9 040 7 4 3.0 1.6  
7250 3.0 37.4 040 8 4 2.2 1.2 | 3.5 38.3 045 6 3 2.7 1.5  
7000 3.2 37.8 045 7 4 3.2 1.7 | 3.7 38.7 045 5 3 2.9 1.6  
6750 3.4 38.1 045 8 4 2.8 1.6 | 4.0 39.2 050 5 2 3.7 2.0  
6500 3.6 38.5 045 6 3 1.8 1.0 | 4.3 39.7 055 4 2 4.3 2.3  
6250 3.7 38.7 050 5 3 2.2 1.2 | 4.6 40.3 060 3 1 3.4 1.8  
6000 3.6 38.5 050 4 2 -10.6 -5.8 | 4.9 40.8 065 2 1 7.9 4.3  
5750 1.9 35.4 055 3 1 -32.3 -17.7 | 5.8 42.4 070 2 1 17.6 9.7  
5500 0.2 32.4 080 1 1 2.2 1.2 | 6.8 44.2 080 1 1 0.8 0.5  
5250 M M M M M M M | M M M M M M M  
5000 M M M M M M M | M M M M M M M  
 
01/14/2026 AT 1400 MST | 01/14/2026 AT 1700 MST  
|  
CAPE... 0.0 LI... +8.0 | CAPE... 0.0 LI... +7.5  
CINH... 0.0 K INDEX... +2.2 | CINH... -0.1 K INDEX... +0.7  
|  
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 -64.8 -84.6 015 44 23 1.7 0.9 | -65.2 -85.4 010 37 19 1.7 0.9  
45000 -61.9 -79.4 015 55 28 2.9 1.6 | -62.2 -80.0 010 46 24 3.0 1.6  
40000 -57.6 -71.7 010 56 29 3.1 1.7 | -57.7 -71.9 360 55 28 2.9 1.6  
38000 -54.7 -66.5 005 56 29 5.0 2.8 | -54.5 -66.1 355 57 29 5.7 3.1  
36000 -51.7 -61.1 360 58 30 5.0 2.8 | -51.1 -60.0 350 58 30 5.7 3.1  
34000 -47.7 -53.9 355 59 30 7.8 4.3 | -46.6 -51.9 345 59 30 7.4 4.1  
32000 -43.1 -45.6 360 60 31 7.8 4.3 | -42.1 -43.8 350 58 30 7.4 4.1  
30000 -38.3 -36.9 360 62 32 8.1 4.4 | -37.7 -35.9 350 59 31 7.4 4.1  
29000 -35.9 -32.6 360 63 33 8.1 4.4 | -35.5 -31.9 350 60 31 7.4 4.1  
28000 -33.5 -28.3 360 65 33 8.1 4.4 | -33.3 -27.9 350 61 32 7.4 4.1  
27000 -30.4 -22.7 360 65 33 8.3 4.6 | -30.9 -23.6 355 61 31 8.1 4.5  
26000 -27.9 -18.2 360 63 33 8.3 4.6 | -28.5 -19.3 355 60 31 8.1 4.5  
25000 -25.4 -13.7 005 62 32 8.4 4.6 | -26.0 -14.8 360 59 30 8.1 4.5  
24000 -23.1 -9.6 005 60 31 7.0 3.8 | -23.7 -10.7 360 58 30 7.5 4.1  
23000 -21.0 -5.8 360 58 30 6.9 3.8 | -21.4 -6.5 360 56 29 7.5 4.1  
22000 -18.9 -2.0 360 55 28 7.0 3.8 | -19.2 -2.6 360 53 27 7.5 4.1  
21000 -17.0 1.4 360 53 27 6.5 3.6 | -16.7 1.9 360 51 26 6.0 3.3  
20000 -15.0 5.0 360 51 26 6.5 3.6 | -14.9 5.2 360 50 26 6.1 3.3  
19500 -14.0 6.8 005 51 26 6.5 3.6 | -14.0 6.8 360 49 25 6.1 3.3  
19000 -13.1 8.4 005 50 25 5.6 3.1 | -13.2 8.2 360 48 25 5.6 3.1  
18500 -12.3 9.9 005 48 24 5.1 2.8 | -12.3 9.9 005 46 24 5.5 3.0  
18000 -11.6 11.1 005 46 24 5.0 2.8 | -11.5 11.3 005 45 23 5.5 3.0  
17500 -10.9 12.4 010 44 23 4.8 2.6 | -10.8 12.6 005 42 22 5.0 2.7  
17000 -10.2 13.6 010 42 22 4.8 2.6 | -10.0 14.0 010 40 21 5.0 2.8  
16500 -9.5 14.9 010 40 21 5.2 2.8 | -9.3 15.3 010 38 19 5.4 3.0  
16000 -8.7 16.3 010 38 20 5.3 2.9 | -8.5 16.7 010 36 18 5.4 3.0  
15500 -7.9 17.8 010 37 19 5.4 3.0 | -7.7 18.1 010 34 17 5.7 3.1  
15000 -7.1 19.2 010 35 18 5.6 3.1 | -6.8 19.8 010 32 16 5.8 3.2  
14500 -6.3 20.7 010 34 18 5.6 3.1 | -6.0 21.2 015 30 16 5.8 3.2  
14000 -5.5 22.1 010 33 17 5.4 3.0 | -5.1 22.8 015 29 15 5.7 3.1  
13500 -4.7 23.5 015 31 16 5.5 3.0 | -4.3 24.3 010 27 14 5.7 3.1  
13000 -3.9 25.0 015 30 15 5.4 3.0 | -3.5 25.7 010 26 13 5.6 3.1  
12500 -3.1 26.4 015 28 14 5.4 3.0 | -2.7 27.1 010 25 13 5.6 3.1  
12000 -2.4 27.7 015 26 13 5.1 2.8 | -1.9 28.6 010 23 12 5.1 2.8  
11500 -1.6 29.1 015 24 12 5.1 2.8 | -1.2 29.8 010 22 11 5.2 2.8  
11000 -0.8 30.6 015 21 11 5.5 3.0 | -0.5 31.1 010 20 10 4.9 2.7  
10500 -0.1 31.8 015 18 10 5.4 3.0 | 0.3 32.5 010 17 9 4.9 2.7  
10250 0.3 32.5 015 17 9 3.8 2.1 | 0.6 33.1 010 16 8 4.1 2.3  
10000 0.5 32.9 015 16 8 3.4 1.9 | 0.9 33.6 010 15 8 4.7 2.6  
9750 0.8 33.4 015 15 8 4.4 2.4 | 1.3 34.3 010 14 7 5.7 3.1  
9500 1.1 34.0 015 14 7 4.4 2.4 | 1.7 35.1 010 13 6 5.4 3.0  
9250 1.5 34.7 020 12 6 4.7 2.6 | 2.1 35.8 010 12 6 5.3 2.9  
9000 2.1 35.8 020 10 5 3.8 2.1 | 2.4 36.3 010 11 5 4.9 2.7  
8750 2.4 36.3 025 9 5 4.7 2.6 | 2.7 36.9 010 9 5 3.2 1.8  
8500 2.8 37.0 025 8 4 6.1 3.3 | 3.0 37.4 010 8 4 4.5 2.5  
8250 3.3 37.9 025 8 4 6.1 3.3 | 3.9 39.0 015 7 3 6.3 3.5  
8000 3.7 38.7 025 7 4 4.1 2.2 | 4.3 39.7 015 6 3 4.2 2.3  
7750 4.0 39.2 025 6 3 4.2 2.3 | 4.6 40.3 015 5 3 4.5 2.5  
7500 4.4 39.9 025 5 3 5.9 3.2 | 5.0 41.0 020 5 2 6.2 3.4  
7250 4.8 40.6 025 4 2 5.7 3.1 | 5.5 41.9 025 4 2 6.4 3.5  
7000 5.2 41.4 025 4 2 4.9 2.7 | 5.9 42.6 035 4 2 3.7 2.0  
6750 5.6 42.1 025 2 1 5.9 3.2 | 6.1 43.0 035 2 1 3.5 1.9  
6500 6.1 43.0 030 2 1 7.0 3.8 | 6.5 43.7 050 2 1 4.8 2.6  
6250 6.6 43.9 035 1 1 8.4 4.6 | 6.8 44.2 070 2 1 8.0 4.4  
6000 7.4 45.3 030 2 1 12.9 7.1 | 7.4 45.3 070 3 1 3.0 1.7  
5750 8.4 47.1 030 2 1 14.4 7.9 | 6.9 44.4 085 2 1 -17.1 -9.4  
5500 9.5 49.1 030 1 1 13.7 7.5 | 6.3 43.3 115 1 1 20.8 11.4  
5250 M M M M M M M | M M M M M M M  
5000 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) 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 AT WALKER FIELD IN GRAND  
JUNCTION, COLORADO AT  
 
NORTH LATITUDE: 39 DEG 07 MIN 00.001 SEC  
WEST LONGITUDE: 108 DEG 31 MIN 59.998 SEC  
ELEVATION: 4839 FEET (1475 METERS)  
 
AND MAY NOT BE REPRESENTATIVE OF OTHER AREAS ALONG THE WESTERN SLOPE OF  
COLORADO. 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  
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