AFOS product SRGBOU
Dates interpreted at 00:00 UTC

Displaying AFOS PIL: SRGBOU
Product Timestamp: 2017-10-10 01:09 UTC

Download date range (UTC midnight)
Bulk Download Bulk Download
370 
UXUS97 KBOU 100109
SRGBOU

Soaring Forecast
National Weather Service Denver/Boulder, Colorado
1909 MDT Monday, October 9, 2017

This forecast is for Tuesday, October 10, 2017:

If the trigger temperature of 50.4 F/10.2 C is reached...then
   Thermal Soaring Index....................... Fair
   Maximum rate of lift........................ 339 ft/min (1.7 m/s)
   Maximum height of thermals.................. 10322 ft MSL (4968 ft AGL)

Forecast maximum temperature................... 54.0 F/12.7 C
Time of trigger temperature.................... 1300 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................. 8735 ft MSL (3381 ft AGL)
Thermal soaring outlook for Wednesday 10/11.... Fair

Wave Soaring Index............................. Poor
Wave Soaring Index trend (to 1800 MDT)......... Slight improvement on tuesday   
Height of stable layer (12-18K ft MSL)......... 12993 ft MSL (7639 ft AGL)
Weak PVA/NVA (through 1800 MDT)................ Neither
Potential height of wave....................... 34188 ft MSL (28834 ft AGL)
Wave soaring outlook for Wednesday 10/11....... Poor

Remarks... Trough moves east and a weak upper ridge moves over the state

Sunrise/Sunset.................... 07:05:11 / 18:27:30 MDT
Total possible sunshine........... 11 hr 22 min 19 sec (682 min 19 sec)
Altitude of sun at 12:46:21 MDT... 43.19 degrees

Upper air data from numerical model forecast valid on 10/10/2017 at 0600 MDT

Freezing level.................. 8028 ft MSL (2674 ft AGL)
Convective condensation level... 21959 ft MSL (16605 ft AGL)
Lifted condensation level....... 14093 ft MSL (8740 ft AGL)
Lifted index.................... +14.9
K index......................... -33.1

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  -62.5 -80.5   270   17    8   0.8   0.4      M     M       M      M    M
 45000  -61.1 -78.0   285   20   10   2.1   1.2      M     M       M      M    M
 40000  -57.9 -72.2   305   26   14   1.7   0.9      M     M       M      M    M
 38000  -53.8 -64.8   305   26   14   6.7   3.7      M     M       M      M    M
 36000  -49.8 -57.6   310   26   14   6.7   3.7      M     M       M      M    M
 34000  -45.4 -49.7   315   25   13   7.8   4.3      M     M       M      M    M
 32000  -40.7 -41.3   320   24   12   7.8   4.3      M     M       M      M    M
 30000  -36.1 -33.0   325   22   11   7.6   4.1   40.8 105.5    21.6      M    M
 29000  -33.8 -28.8   325   21   11   7.6   4.1   40.0 103.9    21.2      M    M
 28000  -31.6 -24.9   330   20   10   7.6   4.2   39.2 102.6    20.9      M    M
 27000  -29.3 -20.7   330   19   10   7.7   4.2   38.4 101.1    20.5      M    M
 26000  -26.9 -16.4   335   18    9   7.7   4.2   37.6  99.6    20.1      M    M
 25000  -24.6 -12.3   340   18    9   7.7   4.2   36.9  98.3    19.7      M    M
 24000  -22.3  -8.1   345   17    9   7.4   4.1   36.1  97.0    19.4      M    M
 23000  -20.1  -4.2   350   18    9   7.5   4.1   35.2  95.4    18.8      M    M
 22000  -17.8  -0.0   355   18    9   7.4   4.1   34.4  94.0    18.4      M    M
 21000  -15.4   4.3   360   18    9   5.8   3.2   33.0  91.4    17.5      M    M
 20000  -13.7   7.3   360   17    9   5.8   3.2   31.6  88.8    16.4      M    M
 19500  -12.8   9.0   005   16    8   5.8   3.2   30.9  87.6    15.9      M    M
 19000  -11.9  10.6   005   16    8   5.8   3.2   30.3  86.5    15.5      M    M
 18500  -11.1  12.0   005   15    8   5.8   3.2   29.6  85.2    14.9      M    M
 18000  -10.2  13.6   010   14    7   5.8   3.2   28.9  84.0    14.4      M    M
 17500   -9.3  15.3   010   13    7   5.8   3.2   28.2  82.7    13.9      M    M
 17000   -8.4  16.9   010   12    6   5.8   3.2   27.5  81.5    13.4      M    M
 16500   -7.5  18.5   010   11    6   5.3   2.9   26.9  80.4    12.9      M    M
 16000   -6.8  19.8   005   10    5   4.9   2.7   26.0  78.8    12.3      M    M
 15500   -6.1  21.0   005    9    5   4.7   2.6   25.2  77.4    11.6      M    M
 15000   -5.5  22.1   360    9    4   3.8   2.1   24.3  75.7    10.8      M    M
 14500   -4.9  23.2   355    8    4   4.0   2.2   23.3  73.9    10.0      M    M
 14000   -4.4  24.1   350    7    4   2.3   1.2   22.2  71.9     9.0      M    M
 13500   -4.1  24.6   350    7    4   2.6   1.4   21.0  69.8     7.9      M    M
 13000   -3.8  25.2   345    7    3   0.9   0.5   19.7  67.4     6.8      M    M
 12500   -3.7  25.3   340    6    3   0.9   0.5   18.2  64.8     5.5      M    M
 12000   -3.6  25.5   340    6    3   1.2   0.7   16.8  62.3     4.2      M    M
 11500   -3.4  25.9   340    6    3   1.2   0.7   15.5  59.8     2.9      M    M
 11000   -3.2  26.2   335    5    3   2.1   1.1   14.2  57.5     1.7      M    M
 10500   -2.9  26.8   335    5    2   2.0   1.1   12.9  55.3     0.5      M    M
 10250   -2.7  27.1   330    4    2   2.8   1.5   12.3  54.2    -0.1    338  1.7
 10000   -2.5  27.5   330    4    2   3.7   2.0   11.8  53.3    -0.6    323  1.6
  9750   -2.2  28.0   330    4    2   3.7   2.0   11.4  52.4    -1.1    308  1.6
  9500   -2.0  28.4   325    3    2   3.7   2.0   10.9  51.6    -1.5    292  1.5
  9250   -1.7  28.9   325    3    2   3.7   2.0   10.4  50.7    -2.0    277  1.4
  9000   -1.4  29.5   325    3    2   3.7   2.0    9.9  49.9    -2.5    261  1.3
  8750   -1.1  30.0   320    3    1   5.1   2.8    9.5  49.1    -2.9    245  1.2
  8500   -0.7  30.7   320    2    1   5.7   3.1    9.2  48.5    -3.2    225  1.1
  8250   -0.4  31.3   320    2    1   4.7   2.6    8.8  47.9    -3.6    207  1.1
  8000   -0.0  32.0   320    2    1   4.4   2.4    8.4  47.2    -4.0    190  1.0
  7750    0.3  32.5   325    1    1   5.2   2.8    8.0  46.5    -4.5    173  0.9
  7500    0.7  33.3   325    1    0   5.5   3.0    7.7  45.9    -4.8    153  0.8
  7250    1.0  33.8   315    1    0   4.8   2.6    7.3  45.2    -5.2    135  0.7
  7000    1.4  34.5   000    0    0   5.6   3.1    7.0  44.6    -5.6    117  0.6
  6750    1.8  35.2   000    0    0   3.0   1.7    6.6  43.9    -6.0     99  0.5
  6500    1.9  35.4   210    1    0   1.3   0.7    6.0  42.8    -6.6     89  0.4
  6250    2.0  35.6   210    1    1   2.9   1.6    5.4  41.8    -7.2     76  0.4
  6000    2.2  36.0   210    2    1   1.4   0.8    4.9  40.8    -7.8     63  0.3
  5750    2.1  35.8   210    2    1  -5.5  -3.0    4.0  39.3    -8.6     60  0.3
  5500    1.3  34.3   205    2    1 -13.7  -7.5    2.5  36.6   -10.2     76  0.4

 * * * * * * Numerical weather prediction model forecast data valid * * * * * * 

           10/10/2017 at 0900 MDT          |       10/10/2017 at 1200 MDT        
                                           |
CAPE...     0.0    LI...      +12.8        | CAPE...     0.0    LI...      +10.2
CINH...     0.0    K Index... -33.1        | CINH...    -0.2    K Index... -32.7
                                           |
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 -63.5 -82.3  265  18  9   0.9   0.5 | -64.0 -83.2  255  19 10   1.3   0.7
 45000 -61.7 -79.1  275  21 11   3.0   1.6 | -61.4 -78.5  255  22 11   3.2   1.7
 40000 -57.0 -70.6  280  24 13   4.7   2.6 | -56.7 -70.1  260  24 12   4.3   2.4
 38000 -53.3 -63.9  285  23 12   6.1   3.3 | -53.3 -63.9  260  23 12   5.7   3.1
 36000 -49.7 -57.5  290  23 12   6.0   3.3 | -49.9 -57.8  265  21 11   5.7   3.1
 34000 -45.4 -49.7  295  21 11   7.9   4.3 | -45.7 -50.3  270  20 10   7.9   4.3
 32000 -40.6 -41.1  300  20 10   7.9   4.3 | -41.0 -41.8  275  18  9   7.9   4.3
 30000 -35.9 -32.6  305  18  9   7.8   4.3 | -35.6 -32.1  280  16  8   8.1   4.4
 29000 -33.5 -28.3  305  18  9   7.8   4.3 | -33.2 -27.8  285  15  8   8.1   4.4
 28000 -31.2 -24.2  310  17  9   7.8   4.3 | -30.8 -23.4  285  14  7   8.1   4.5
 27000 -28.9 -20.0  315  16  8   7.6   4.2 | -28.5 -19.3  290  13  7   7.5   4.1
 26000 -26.6 -15.9  320  15  8   7.6   4.2 | -26.2 -15.2  290  12  6   7.6   4.1
 25000 -24.3 -11.7  325  14  7   7.6   4.2 | -23.9 -11.0  295  11  6   7.6   4.1
 24000 -22.1  -7.8  330  13  7   7.4   4.1 | -21.7  -7.1  300  10  5   7.5   4.1
 23000 -19.9  -3.8  335  13  7   7.4   4.1 | -19.5  -3.1  305   9  4   7.5   4.1
 22000 -17.1   1.2  345  12  6   7.4   4.1 | -17.2   1.0  310   8  4   7.5   4.1
 21000 -14.9   5.2  350  12  6   7.2   3.9 | -15.0   5.0  315   7  3   7.3   4.0
 20000 -12.7   9.1  355  11  6   7.2   3.9 | -12.8   9.0  320   6  3   7.3   4.0
 19500 -11.7  10.9  360  11  6   7.2   3.9 | -11.7  10.9  325   5  3   7.3   4.0
 19000 -10.6  12.9  005  11  5   6.4   3.5 | -10.6  12.9  330   5  2   7.1   3.9
 18500  -9.7  14.5  005  10  5   6.0   3.3 |  -9.6  14.7  335   4  2   6.5   3.6
 18000  -8.8  16.2  010   9  5   6.0   3.3 |  -8.7  16.3  335   4  2   6.6   3.6
 17500  -7.9  17.8  010   9  5   6.0   3.3 |  -7.7  18.1  340   3  2   5.9   3.3
 17000  -7.0  19.4  010   8  4   6.0   3.3 |  -6.4  20.5  335   3  1   5.9   3.2
 16500  -6.1  21.0  010   8  4   5.7   3.1 |  -5.5  22.1  330   2  1   6.0   3.3
 16000  -5.3  22.5  010   7  4   5.6   3.1 |  -4.6  23.7  330   2  1   6.0   3.3
 15500  -4.4  24.1  010   7  4   5.3   2.9 |  -3.7  25.3  325   2  1   5.6   3.0
 15000  -3.7  25.3  010   6  3   4.8   2.6 |  -2.9  26.8  320   2  1   5.3   2.9
 14500  -2.9  26.8  010   6  3   4.7   2.6 |  -2.1  28.2  315   2  1   5.2   2.9
 14000  -2.4  27.7  005   6  3   3.4   1.8 |  -1.3  29.7  315   2  1   5.0   2.7
 13500  -1.8  28.8  360   5  3   3.7   2.0 |  -0.6  30.9  310   2  1   4.9   2.7
 13000  -1.4  29.5  355   5  3   1.5   0.8 |   0.1  32.2  305   2  1   3.9   2.1
 12500  -1.2  29.8  345   5  2   1.8   1.0 |   0.6  33.1  305   2  1   4.0   2.2
 12000  -1.0  30.2  340   5  2   0.7   0.4 |   1.2  34.2  295   2  1   3.3   1.8
 11500  -0.9  30.4  335   4  2   0.7   0.4 |   1.7  35.1  290   3  1   3.4   1.9
 11000  -0.8  30.6  330   4  2   1.0   0.6 |   2.1  35.8  285   3  1   2.5   1.4
 10500  -0.7  30.7  320   3  2   0.9   0.5 |   2.5  36.5  280   3  1   2.6   1.4
 10250  -0.6  30.9  315   3  2   1.8   1.0 |   2.7  36.9  275   3  1   2.4   1.3
 10000  -0.4  31.3  315   3  1   2.5   1.4 |   2.8  37.0  275   3  1   2.0   1.1
  9750  -0.3  31.5  310   3  1   1.9   1.0 |   2.9  37.2  265   3  1   1.9   1.0
  9500  -0.2  31.6  305   2  1   2.0   1.1 |   3.1  37.6  260   3  1   2.0   1.1
  9250  -0.0  32.0  300   2  1   2.6   1.4 |   3.2  37.8  250   3  1   2.0   1.1
  9000   0.2  32.4  295   2  1   3.0   1.6 |   3.4  38.1  245   3  1   2.3   1.2
  8750   0.4  32.7  285   1  1   3.2   1.8 |   3.5  38.3  235   2  1   2.9   1.6
  8500   0.7  33.3  265   1  1   3.9   2.2 |   3.8  38.8  225   2  1   3.1   1.7
  8250   0.9  33.6  245   1  1   4.3   2.4 |   4.0  39.2  215   3  1   2.9   1.6
  8000   1.3  34.3  225   1  1   4.7   2.6 |   4.2  39.6  205   3  1   2.9   1.6
  7750   1.6  34.9  210   1  1   3.7   2.0 |   4.4  39.9  200   3  1   2.8   1.5
  7500   1.8  35.2  200   2  1   4.1   2.3 |   4.5  40.1  195   3  2   3.1   1.7
  7250   2.2  36.0  195   2  1   5.3   2.9 |   4.8  40.6  185   3  2   3.6   2.0
  7000   2.5  36.5  190   2  1   5.6   3.1 |   5.0  41.0  175   3  2   3.3   1.8
  6750   2.9  37.2  185   3  1   3.2   1.8 |   5.2  41.4  170   3  2   4.3   2.4
  6500   3.0  37.4  190   3  1   1.4   0.7 |   5.6  42.1  165   3  2   5.8   3.2
  6250   3.2  37.8  190   3  1   3.3   1.8 |   6.0  42.8  160   3  2   6.1   3.3
  6000   3.4  38.1  195   3  2   0.7   0.4 |   6.4  43.5  155   3  1   5.8   3.2
  5750   3.2  37.8  195   3  1  -2.6  -1.4 |   6.9  44.4  150   3  1  10.3   5.7
  5500   3.0  37.4  190   2  1  -1.8  -1.0 |   7.9  46.2  150   2  1  18.8  10.3

           10/10/2017 at 1500 MDT          |       10/10/2017 at 1800 MDT        
                                           |
CAPE...     0.0    LI...       +8.6        | CAPE...     0.0    LI...       +7.4
CINH...    -0.1    K Index... -28.6        | CINH...     0.0    K Index... -14.1
                                           |
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 -63.2 -81.8  250  22 11   1.2   0.7 | -62.7 -80.9  245  23 12   1.8   1.0
 45000 -61.0 -77.8  250  26 14   2.3   1.2 | -59.9 -75.8  245  28 14   1.7   0.9
 40000 -57.5 -71.5  250  26 13   3.7   2.0 | -57.3 -71.1  245  26 14   3.2   1.7
 38000 -54.0 -65.2  250  24 13   6.0   3.3 | -53.9 -65.0  245  25 13   5.9   3.2
 36000 -50.4 -58.7  250  23 12   6.0   3.3 | -50.3 -58.5  250  23 12   5.9   3.2
 34000 -46.1 -51.0  250  21 11   8.0   4.4 | -46.1 -51.0  250  21 11   7.9   4.3
 32000 -41.4 -42.5  250  19 10   7.9   4.4 | -40.8 -41.4  250  19 10   7.9   4.3
 30000 -35.9 -32.6  255  17  9   8.3   4.6 | -36.0 -32.8  250  18  9   8.1   4.4
 29000 -33.4 -28.1  255  16  8   8.3   4.6 | -33.6 -28.5  245  17  9   8.1   4.4
 28000 -30.9 -23.6  260  15  8   8.4   4.6 | -31.2 -24.2  245  17  9   8.1   4.4
 27000 -28.5 -19.3  260  14  7   7.8   4.3 | -28.9 -20.0  245  16  8   7.7   4.2
 26000 -26.2 -15.2  260  13  7   7.8   4.3 | -26.5 -15.7  240  15  8   7.7   4.2
 25000 -23.8 -10.8  260  12  6   7.8   4.3 | -24.2 -11.6  240  15  8   7.7   4.3
 24000 -21.5  -6.7  260  11  6   7.7   4.2 | -21.9  -7.4  240  14  7   8.0   4.4
 23000 -19.2  -2.6  260  10  5   7.7   4.2 | -19.5  -3.1  240  13  7   8.0   4.4
 22000 -16.9   1.6  260   9  4   7.7   4.2 | -17.1   1.2  235  12  6   8.0   4.4
 21000 -14.6   5.7  260   8  4   7.6   4.2 | -14.7   5.5  235  12  6   8.0   4.4
 20000 -12.4   9.7  260   7  3   7.6   4.2 | -12.3   9.9  235  11  6   8.0   4.4
 19500 -11.2  11.8  260   6  3   7.6   4.2 | -11.1  12.0  235  10  5   8.0   4.4
 19000 -10.1  13.8  260   6  3   7.6   4.1 |  -9.9  14.2  230  10  5   7.9   4.3
 18500  -9.0  15.8  260   6  3   7.4   4.0 |  -8.8  16.2  235  10  5   7.8   4.3
 18000  -7.8  18.0  255   6  3   7.4   4.1 |  -7.6  18.3  235  10  5   7.8   4.3
 17500  -6.8  19.8  255   6  3   6.7   3.7 |  -5.9  21.4  235   9  5   7.2   3.9
 17000  -5.3  22.5  255   6  3   6.6   3.6 |  -4.9  23.2  235   9  5   7.3   4.0
 16500  -4.3  24.3  255   6  3   6.6   3.6 |  -3.8  25.2  240   9  4   6.4   3.5
 16000  -3.3  26.1  255   7  3   6.6   3.6 |  -2.9  26.8  240   8  4   6.4   3.5
 15500  -2.4  27.7  250   7  3   6.3   3.4 |  -1.9  28.6  245   8  4   6.5   3.6
 15000  -1.5  29.3  250   7  4   6.1   3.3 |  -0.9  30.4  245   8  4   6.6   3.6
 14500  -0.6  30.9  250   7  4   6.0   3.3 |   0.0  32.0  250   7  4   6.5   3.6
 14000   0.3  32.5  250   7  3   5.7   3.1 |   1.0  33.8  250   7  4   6.2   3.4
 13500   1.2  34.2  250   6  3   5.7   3.1 |   1.9  35.4  255   7  4   6.2   3.4
 13000   1.9  35.4  250   6  3   4.4   2.4 |   2.7  36.9  255   6  3   5.1   2.8
 12500   2.6  36.7  250   6  3   4.6   2.5 |   3.4  38.1  255   6  3   5.4   3.0
 12000   3.2  37.8  250   5  3   3.6   2.0 |   4.1  39.4  255   6  3   3.9   2.1
 11500   3.8  38.8  245   5  3   3.8   2.1 |   4.7  40.5  250   5  3   4.2   2.3
 11000   4.3  39.7  240   5  2   2.8   1.5 |   5.2  41.4  245   5  2   3.0   1.6
 10500   4.7  40.5  235   4  2   3.1   1.7 |   5.6  42.1  240   4  2   3.3   1.8
 10250   4.9  40.8  235   4  2   2.0   1.1 |   5.8  42.4  235   4  2   1.9   1.0
 10000   5.0  41.0  230   4  2   1.9   1.0 |   5.9  42.6  235   4  2   1.7   1.0
  9750   5.2  41.4  225   4  2   3.0   1.6 |   6.0  42.8  230   4  2   3.0   1.6
  9500   5.3  41.5  225   4  2   2.8   1.5 |   6.2  43.2  230   4  2   3.2   1.8
  9250   5.5  41.9  220   4  2   2.2   1.2 |   6.3  43.3  225   4  2   0.5   0.3
  9000   5.6  42.1  215   4  2   2.2   1.2 |   6.3  43.3  220   4  2  -0.5  -0.3
  8750   5.8  42.4  210   4  2   3.4   1.9 |   6.3  43.3  210   4  2   1.8   1.0
  8500   6.0  42.8  205   4  2   3.1   1.7 |   6.4  43.5  200   3  2   2.2   1.2
  8250   6.2  43.2  195   4  2   1.7   1.0 |   6.7  44.1  190   3  2   5.0   2.7
  8000   6.3  43.3  185   4  2   1.6   0.9 |   7.1  44.8  180   3  2   6.6   3.6
  7750   6.4  43.5  170   4  2   2.3   1.3 |   7.6  45.7  170   3  2   6.5   3.6
  7500   6.6  43.9  155   4  2   5.0   2.8 |   8.1  46.6  165   3  2   7.2   3.9
  7250   7.0  44.6  150   4  2   7.3   4.0 |   8.6  47.5  160   3  2   7.5   4.1
  7000   7.5  45.5  145   4  2   6.9   3.8 |   9.2  48.6  155   3  2   7.7   4.2
  6750   8.0  46.4  140   4  2   7.2   3.9 |   9.7  49.5  150   3  2   6.2   3.4
  6500   8.6  47.5  135   4  2   8.8   4.9 |  10.1  50.2  145   4  2   6.4   3.5
  6250   9.3  48.7  135   4  2   9.5   5.2 |  10.7  51.3  135   3  2   7.4   4.1
  6000  10.0  50.0  130   4  2  10.2   5.6 |  11.2  52.2  130   3  2   8.2   4.5
  5750  10.9  51.6  130   4  2  14.0   7.7 |  11.7  53.1  120   3  1   3.7   2.1
  5500  12.0  53.6  130   3  2  17.1   9.4 |  11.6  52.9  110   2  1  -6.9  -3.8
________________________________________________________________________________

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