Soaring Guidance
Issued by NWS Pueblo, CO

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000
UXUS97 KPUB 221020
SRGPUB

SOARING FORECAST
NATIONAL WEATHER SERVICE PUEBLO CO
420 AM MDT WED MAY 22 2013


EXPERIMENTAL PRODUCT

This forecast is for Wednesday May 22, 2013:

If the trigger temperature of 57.9 F/14.4 C is reached...then
   Thermal Soaring Index....................... Excellent
   Maximum rate of lift........................ 1306 ft/min (6.6 m/s)
   Maximum height of thermals.................. 21456 ft MSL (13796 ft AGL)

Forecast maximum temperature................... 72.0 F/22.7 C
Time of trigger temperature.................... 0830 MDT
Time of overdevelopment........................ 1400 MDT
Middle/high clouds during soaring window....... None
Surface winds during soaring window............ 20 mph or less
Height of the -3 thermal index................. 18542 ft MSL (10882 ft AGL)
Thermal soaring outlook for Thursday 05/23..... Fair

Wave Soaring Index............................. Poor
Wave Soaring Index trend (to 1800 MDT)......... Same
Height of stable layer (12-18K ft MSL)......... None
Weak PVA/NVA (through 1800 MDT)................ Neither
Potential height of wave....................... 15272 ft MSL (7612 ft AGL)
Wave soaring outlook for Thursday 05/23........ Poor

Remarks...

Sunrise/Sunset.................... 05:41:01 / 20:10:46 MDT
Total possible sunshine........... 14 hr 29 min 44 sec (869 min 44 sec)
Altitude of sun at 12:56:05 MDT... 71.53 degrees

Upper air data from numerical model forecast valid on 05/22/2013 at 0600 MDT

Freezing level.................. 12549 ft MSL (4889 ft AGL)
Convective condensation level... 15898 ft MSL (8238 ft AGL)
Lifted condensation level....... 18296 ft MSL (10635 ft AGL)
Lifted index.................... -3.5
K index......................... +19.8

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  -57.7 -71.9   249   19   10   2.4   1.3   89.6 193.2    40.0      M    M
 45000  -54.6 -66.3   261   29   15  -0.9  -0.5   72.5 162.5    31.8      M    M
 40000  -55.9 -68.6   290   44   22  -0.9  -0.5   48.0 118.4    17.4      M    M
 38000  -54.9 -66.8   292   43   22   3.0   1.7   40.9 105.5    13.0      M    M
 36000  -52.9 -63.2   290   37   19   3.0   1.7   34.4  94.0     8.8      M    M
 34000  -49.9 -57.8   287   34   17   7.8   4.3   30.7  87.2     6.2      M    M
 32000  -45.2 -49.4   284   33   17   7.8   4.3   29.1  84.3     5.2      M    M
 30000  -40.4 -40.7   282   32   17   8.3   4.5   27.8  82.0     4.3      M    M
 29000  -37.9 -36.2   282   31   16   8.3   4.5   27.2  80.9     3.8      M    M
 28000  -35.5 -31.9   281   30   16   8.3   4.5   26.7  80.0     3.5      M    M
 27000  -33.0 -27.4   281   29   15   8.2   4.5   26.2  79.1     3.1      M    M
 26000  -30.6 -23.1   282   29   15   8.2   4.5   25.5  77.9     2.6      M    M
 25000  -28.1 -18.6   283   28   14   8.2   4.5   25.0  76.9     2.2      M    M
 24000  -25.7 -14.3   284   27   14   7.7   4.2   24.5  76.1     1.8      M    M
 23000  -22.9  -9.2   287   27   14   7.6   4.2   23.4  74.1     0.9      M    M
 22000  -20.6  -5.1   289   27   14   7.6   4.1   22.7  72.8     0.3      M    M
 21000  -18.5  -1.3   292   27   14   6.5   3.6   21.8  71.2    -0.6   1258  6.4
 20000  -16.6   2.1   296   26   14   6.6   3.6   20.6  69.2    -1.6   1171  5.9
 19500  -15.7   3.7   299   26   14   6.6   3.6   20.1  68.2    -2.1   1127  5.7
 19000  -14.7   5.5   301   26   14   6.6   3.6   19.6  67.3    -2.6   1084  5.5
 18500  -13.8   7.2   302   26   13   6.6   3.6   19.1  66.4    -3.1   1040  5.3
 18000  -12.8   9.0   303   26   13   6.6   3.6   18.6  65.4    -3.6    997  5.1
 17500  -11.8  10.8   303   26   13   7.0   3.9   18.1  64.5    -4.1    953  4.8
 17000  -10.8  12.6   303   26   13   7.3   4.0   17.6  63.7    -4.6    907  4.6
 16500   -9.7  14.5   302   26   13   7.4   4.1   17.2  63.0    -5.0    860  4.4
 16000   -8.6  16.5   301   26   14   8.1   4.4   16.9  62.4    -5.3    811  4.1
 15500   -7.4  18.7   299   27   14   8.1   4.4   16.6  61.9    -5.6    760  3.9
 15000   -6.2  20.8   298   28   14   7.7   4.2   16.3  61.4    -5.9    711  3.6
 14500   -5.1  22.8   297   28   14   7.7   4.2   16.0  60.8    -6.3    662  3.4
 14000   -3.9  25.0   296   28   14   8.2   4.5   15.7  60.3    -6.6    612  3.1
 13500   -2.7  27.1   296   26   13   8.4   4.6   15.5  59.9    -6.9    560  2.8
 13000   -1.4  29.5   296   24   12   8.8   4.8   15.3  59.5    -7.1    508  2.6
 12500   -0.1  31.8   296   22   11   9.0   5.0   15.2  59.3    -7.2    453  2.3
 12000    1.3  34.3   296   20   10   9.1   5.0   15.1  59.1    -7.4    397  2.0
 11750    2.0  35.6   294   19   10   9.2   5.1   15.0  59.0    -7.4    370  1.9
 11500    2.7  36.9   291   18    9   9.1   5.0   15.0  58.9    -7.5    342  1.7
 11250    3.3  37.9   287   16    8   9.6   5.2   14.9  58.9    -7.6    314  1.6
 11000    4.0  39.2   283   15    8   7.9   4.3   14.9  58.8    -7.6    286  1.5
 10750    4.5  40.1   280   14    7   5.8   3.2   14.6  58.3    -7.9    265  1.3
 10500    4.9  40.8   277   13    6   5.9   3.2   14.3  57.8    -8.2    245  1.2
 10250    5.3  41.5   273   11    6   6.1   3.3   14.0  57.3    -8.6    224  1.1
 10000    5.8  42.4   268   10    5   5.4   3.0   13.8  56.8    -8.9    204  1.0
  9750    6.1  43.0   263    9    5   4.6   2.5   13.4  56.1    -9.3    187  0.9
  9500    6.8  44.2   254    8    4   5.1   2.8   12.6  54.7   -10.1    152  0.8
  9250    7.1  44.8   248    8    4   2.9   1.6   12.2  54.0   -10.6    135  0.7
  9000    7.2  45.0   242    8    4   0.7   0.4   11.6  52.8   -11.3    125  0.6
  8750    7.3  45.1   236    8    4   1.7   0.9   10.9  51.6   -11.9    115  0.6
  8500    7.3  45.1   230    9    5   0.1   0.1   10.3  50.5   -12.6    106  0.5
  8250    7.0  44.6   227    8    4  -8.9  -4.9    9.3  48.7   -13.7    107  0.5
  8000    5.9  42.6   231    6    3 -19.5 -10.7    7.4  45.4   -15.5    133  0.7
  7750    4.8  40.6   238    4    2  -2.0  -1.1    5.6  42.1   -17.4    158  0.8
  7500      M     M     M    M    M     M     M      M     M       M      M    M
  7250      M     M     M    M    M     M     M      M     M       M      M    M
  7000      M     M     M    M    M     M     M      M     M       M      M    M
  6750      M     M     M    M    M     M     M      M     M       M      M    M

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

           05/22/2013 at 0900 MDT          |       05/22/2013 at 1200 MDT
                                           |
K index... +18.6                           | K index... +21.2
                                           |
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 -58.2 -72.8  249  23 12   2.0   1.1 | -58.5 -73.3  245  25 13   1.3   0.7
 45000 -55.6 -68.1  261  37 19  -0.4  -0.2 | -56.7 -70.1  262  40 21  -0.2  -0.1
 40000 -56.4 -69.5  287  43 22  -0.5  -0.2 | -57.2 -71.0  280  48 24  -0.2  -0.1
 38000 -54.7 -66.5  287  43 22   3.7   2.1 | -55.3 -67.5  282  46 24   3.8   2.1
 36000 -52.4 -62.3  284  40 21   3.7   2.1 | -53.1 -63.6  284  43 22   3.8   2.1
 34000 -49.2 -56.6  284  38 19   7.8   4.3 | -49.6 -57.3  287  40 21   8.4   4.6
 32000 -44.5 -48.1  288  34 18   7.8   4.3 | -44.5 -48.1  293  37 19   8.4   4.6
 30000 -40.0 -40.0  291  32 16   7.2   4.0 | -39.4 -38.9  299  35 18   8.7   4.8
 29000 -37.8 -36.0  290  32 16   7.2   4.0 | -36.8 -34.2  301  33 17   8.7   4.8
 28000 -35.6 -32.1  290  31 16   7.2   4.0 | -34.2 -29.6  303  32 16   8.7   4.8
 27000 -33.4 -28.1  289  31 16   8.3   4.6 | -31.7 -25.1  305  31 16   7.3   4.0
 26000 -31.0 -23.8  289  31 16   8.2   4.5 | -29.5 -21.1  305  30 16   7.4   4.0
 25000 -28.5 -19.3  288  31 16   8.3   4.5 | -27.3 -17.1  306  30 15   7.4   4.1
 24000 -25.6 -14.1  287  31 16   7.3   4.0 | -24.7 -12.5  304  29 15   6.3   3.5
 23000 -23.4 -10.1  286  31 16   7.4   4.1 | -22.8  -9.0  299  29 15   6.4   3.5
 22000 -21.2  -6.2  285  31 16   7.4   4.1 | -21.0  -5.8  295  29 15   6.5   3.6
 21000 -19.0  -2.2  285  30 15   7.5   4.1 | -19.0  -2.2  291  29 15   7.1   3.9
 20000 -16.7   1.9  287  28 14   7.5   4.1 | -16.9   1.6  289  28 14   7.2   3.9
 19500 -15.6   3.9  287  26 14   7.5   4.1 | -15.8   3.6  288  28 14   7.2   3.9
 19000 -14.5   5.9  288  25 13   7.5   4.1 | -14.7   5.5  287  28 14   7.3   4.0
 18500 -13.5   7.7  292  25 13   6.6   3.6 | -13.7   7.3  287  26 14   7.5   4.1
 18000 -12.5   9.5  298  25 13   6.7   3.7 | -12.5   9.5  287  25 13   7.5   4.1
 17500 -11.5  11.3  303  26 13   6.6   3.6 | -11.4  11.5  288  24 12   7.8   4.3
 17000 -10.6  12.9  309  25 13   6.6   3.6 | -10.3  13.5  289  22 11   7.9   4.3
 16500  -9.6  14.7  315  25 13   6.8   3.7 |  -9.1  15.6  291  21 11   8.0   4.4
 16000  -8.6  16.5  319  24 12   7.3   4.0 |  -7.9  17.8  292  19 10   8.3   4.6
 15500  -7.5  18.5  323  23 12   7.1   3.9 |  -6.7  19.9  294  18  9   8.3   4.6
 15000  -6.3  20.7  325  23 12   9.1   5.0 |  -5.5  22.1  295  16  8   8.6   4.7
 14500  -5.0  23.0  326  23 12   8.9   4.9 |  -4.2  24.4  297  14  7   8.6   4.7
 14000  -3.7  25.3  325  23 12   9.3   5.1 |  -2.9  26.8  298  11  6   9.2   5.0
 13500  -2.3  27.9  322  23 12   9.4   5.1 |  -1.6  29.1  298   9  5   9.2   5.1
 13000  -1.0  30.2  319  23 12   9.0   4.9 |  -0.2  31.6  299   7  4   9.4   5.2
 12500   0.3  32.5  317  21 11   8.7   4.8 |   1.2  34.2  301   6  3   9.5   5.2
 12000   1.6  34.9  315  19 10   8.5   4.7 |   2.6  36.7  302   5  3   9.7   5.3
 11750   2.3  36.1  313  18  9   8.3   4.5 |   3.3  37.9  302   5  2   9.9   5.5
 11500   2.9  37.2  310  16  8   8.3   4.6 |   4.1  39.4  302   4  2   9.9   5.4
 11250   3.5  38.3  306  15  8   8.3   4.5 |   4.8  40.6  302   4  2   9.9   5.5
 11000   4.1  39.4  302  14  7   8.4   4.6 |   5.5  41.9  302   4  2   9.7   5.3
 10750   4.7  40.5  298  12  6   8.6   4.7 |   6.2  43.2  301   3  2   9.5   5.2
 10500   5.4  41.7  292  11  6   8.5   4.7 |   6.9  44.4  300   2  1   9.6   5.2
 10250   6.0  42.8  286  10  5   8.7   4.8 |   7.7  45.9  298   2  1   9.5   5.2
 10000   6.6  43.9  278  10  5   8.1   4.5 |   8.4  47.1  293   1  1   9.8   5.4
  9750   7.8  46.0  273   8  4   7.7   4.2 |   9.9  49.8  000   0  0  10.0   5.5
  9500   8.3  46.9  270   7  4   7.7   4.2 |  10.6  51.1  000   0  0  10.1   5.5
  9250   8.9  48.0  265   6  3   6.9   3.8 |  11.4  52.5  158   1  0  10.2   5.6
  9000   9.3  48.7  259   6  3   6.3   3.5 |  12.1  53.8  147   1  0  10.4   5.7
  8750   9.8  49.6  252   6  3   6.2   3.4 |  12.9  55.2  142   1  1   9.9   5.4
  8500  10.2  50.4  243   5  3   7.5   4.1 |  13.7  56.7  138   1  1  11.7   6.4
  8250  10.9  51.6  236   5  3  13.3   7.3 |  14.7  58.5  132   2  1  18.8  10.3
  8000  12.1  53.8  228   4  2  18.6  10.2 |  16.4  61.5  123   2  1  25.2  13.8
  7750  13.3  55.9  217   4  2  10.6   5.8 |  18.0  64.4  118   3  2  15.5   8.5
  7500     M     M    M   M  M     M     M |     M     M    M   M  M     M     M
  7250     M     M    M   M  M     M     M |     M     M    M   M  M     M     M
  7000     M     M    M   M  M     M     M |     M     M    M   M  M     M     M
  6750     M     M    M   M  M     M     M |     M     M    M   M  M     M     M

           05/22/2013 at 1500 MDT          |       05/22/2013 at 1800 MDT
                                           |
K index... +24.6                           | K index... +25.6
                                           |
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 -58.8 -73.8  252  25 13   1.2   0.6 | -58.9 -74.0  257  24 12   0.9   0.5
 45000 -57.3 -71.1  266  38 20  -0.7  -0.4 | -57.8 -72.0  271  36 19  -0.7  -0.4
 40000 -58.4 -73.1  277  45 23  -0.6  -0.3 | -58.9 -74.0  273  39 20  -0.6  -0.3
 38000 -56.1 -69.0  279  44 22   4.7   2.6 | -56.4 -69.5  272  37 19   5.0   2.7
 36000 -53.3 -63.9  280  41 21   4.7   2.6 | -53.5 -64.3  270  34 17   5.0   2.7
 34000 -49.4 -56.9  282  38 20   8.5   4.7 | -49.4 -56.9  270  31 16   8.4   4.6
 32000 -44.3 -47.7  286  36 18   8.6   4.7 | -44.4 -47.9  273  27 14   8.4   4.6
 30000 -39.2 -38.6  289  33 17   8.5   4.7 | -39.3 -38.7  277  25 13   8.6   4.7
 29000 -36.7 -34.1  290  33 17   8.5   4.7 | -36.7 -34.1  279  25 13   8.6   4.7
 28000 -34.1 -29.4  291  32 16   8.5   4.7 | -34.2 -29.6  280  24 13   8.6   4.7
 27000 -31.6 -24.9  294  30 15   8.2   4.5 | -31.6 -24.9  283  23 12   8.5   4.7
 26000 -29.2 -20.6  298  27 14   8.2   4.5 | -29.1 -20.4  285  22 11   8.5   4.7
 25000 -26.7 -16.1  303  24 13   8.2   4.5 | -26.5 -15.7  288  20 11   8.5   4.7
 24000 -24.4 -11.9  307  22 11   7.2   3.9 | -24.1 -11.4  290  19 10   7.3   4.0
 23000 -21.7  -7.1  301  21 11   7.2   4.0 | -21.3  -6.3  285  20 10   7.4   4.1
 22000 -19.6  -3.3  296  21 11   7.2   4.0 | -19.1  -2.4  282  20 10   7.5   4.1
 21000 -17.5   0.5  288  22 11   6.7   3.7 | -17.0   1.4  274  20 11   6.8   3.8
 20000 -15.6   3.9  278  24 12   6.7   3.7 | -15.0   5.0  265  22 11   6.9   3.8
 19500 -14.6   5.7  274  25 13   6.7   3.7 | -14.0   6.8  261  22 12   7.0   3.9
 19000 -13.7   7.3  271  27 14   7.0   3.8 | -13.1   8.4  257  23 12   7.4   4.0
 18500 -12.6   9.3  267  25 13   7.7   4.2 | -11.9  10.6  253  22 11   7.9   4.3
 18000 -11.5  11.3  263  23 12   7.7   4.2 | -10.8  12.6  249  20 11   7.9   4.3
 17500 -10.4  13.3  260  20 10   7.5   4.1 |  -9.6  14.7  245  19 10   8.1   4.5
 17000  -9.3  15.3  258  17  9   7.5   4.1 |  -8.5  16.7  242  18  9   8.2   4.5
 16500  -8.2  17.2  256  14  7   7.8   4.3 |  -7.3  18.9  238  16  8   8.6   4.7
 16000  -7.0  19.4  255  11  6   8.1   4.4 |  -5.9  21.4  236  15  8   9.1   5.0
 15500  -5.8  21.6  254   8  4   8.1   4.4 |  -4.6  23.7  234  14  7   9.2   5.0
 15000  -4.5  23.9  251   6  3   9.5   5.2 |  -3.2  26.2  231  13  7   9.7   5.3
 14500  -3.1  26.4  244   5  2   9.4   5.2 |  -1.7  28.9  229  13  6   9.8   5.4
 14000  -1.7  28.9  232   4  2   9.1   5.0 |  -0.4  31.3  223  12  6   8.2   4.5
 13500  -0.4  31.3  220   3  2   9.1   5.0 |   0.8  33.4  212  11  6   8.2   4.5
 13000   0.9  33.6  201   3  1   8.6   4.7 |   2.1  35.8  201  11  6   8.0   4.4
 12500   2.2  36.0  174   3  2   8.5   4.7 |   3.2  37.8  191  10  5   8.0   4.4
 12000   3.4  38.1  156   4  2   8.4   4.6 |   4.4  39.9  180  10  5   8.2   4.5
 11750   4.0  39.2  153   5  2   8.4   4.6 |   5.0  41.0  176  10  5   8.4   4.6
 11500   4.7  40.5  150   5  3   8.5   4.6 |   5.6  42.1  171  10  5   8.4   4.6
 11250   5.3  41.5  149   6  3   8.3   4.5 |   6.3  43.3  166  10  5   8.3   4.6
 11000   5.9  42.6  147   7  4   9.1   5.0 |   6.9  44.4  161  10  5   9.0   4.9
 10750   6.6  43.9  147   7  4   9.8   5.4 |   7.6  45.7  159  10  5   9.6   5.3
 10500   7.3  45.1  146   7  4   9.6   5.3 |   8.3  46.9  157  10  5   9.4   5.2
 10250   8.1  46.6  145   7  4   9.6   5.3 |   9.0  48.2  155  10  5   9.4   5.2
 10000   8.8  47.8  145   8  4   9.8   5.3 |   9.7  49.5  153  10  5   9.6   5.3
  9750  10.3  50.5  144   8  4   9.8   5.4 |  11.2  52.2  152  10  5   9.8   5.4
  9500  11.0  51.8  144   8  4   9.9   5.4 |  11.9  53.4  151  10  5   9.8   5.4
  9250  11.7  53.1  144   8  4   9.7   5.3 |  12.6  54.7  150  10  5   9.7   5.3
  9000  12.4  54.3  144   8  4   9.7   5.3 |  13.3  55.9  150  10  5   9.7   5.3
  8750  13.1  55.6  144   8  4   9.5   5.2 |  14.1  57.4  149  10  5   9.6   5.2
  8500  13.9  57.0  144   8  4  10.2   5.6 |  14.8  58.6  149  10  5  10.1   5.5
  8250  14.7  58.5  143   8  4  14.0   7.7 |  15.6  60.1  147  10  5  12.9   7.1
  8000  15.9  60.6  139   9  4  17.8   9.7 |  16.7  62.1  143   9  5  15.9   8.7
  7750  17.1  62.8  135   9  5  11.8   6.5 |  17.7  63.9  139   9  5  11.2   6.1
  7500     M     M    M   M  M     M     M |     M     M    M   M  M     M     M
  7250     M     M    M   M  M     M     M |     M     M    M   M  M     M     M
  7000     M     M    M   M  M     M     M |     M     M    M   M  M     M     M
  6750     M     M    M   M  M     M     M |     M     M    M   M  M     M     M
________________________________________________________________________________

This product is issued one per day by approximately 0630 MST/0730 MDT
(1330 UTC).  It is not continuously monitored nor updated after its initial
issuance.

The information contained herein is based on numerical weather prediction
model data taken near the Air Force Academy in Colorado Springs, Colorado
at

                   North Latitude:  38 deg 58 min 48.000 sec
                   West Longitude: 104 deg 49 min 12.000 sec
                   Elevation: 6572 feet (2003 meters)

and may not be representative of other areas along the Front Range of the
Colorado Rocky Mountains.  Note that some elevations in numerical weather
prediction models differ from actual station elevations, which can lead to
data which appear to be below ground.  Erroneous data such as these should
not be used.

The content and format of this report as well as the issuance times are subject
to change without prior notice.  Comments and suggestions are welcome and should
be directed to one of the addresses or phone numbers shown at the bottom of this
page.  To expedite a response to comments, be sure to mention your interest in
the soaring forecast.

At this time, the output from this considered experimental.

DEFINITIONS:

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 - 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, cirrostatus, 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.

071806



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