Soaring Guidance
Issued by NWS Pueblo, CO

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000
UXUS97 KPUB 110956
SRGPUB

SOARING FORECAST
NATIONAL WEATHER SERVICE PUEBLO CO
356 AM MDT TUE JUN 11 2013


EXPERIMENTAL PRODUCT

This forecast is for Tuesday June 11, 2013:

If the trigger temperature of 79.1 F/26.2 C is reached...then
   Thermal Soaring Index....................... Good
   Maximum rate of lift........................ 2404 ft/min (12.2 m/s)
   Maximum height of thermals.................. 30827 ft MSL (23164 ft AGL)

Forecast maximum temperature................... 95.0 F/35.5 C
Time of trigger temperature.................... 0830 MDT
Time of overdevelopment........................ None
Middle/high clouds during soaring window....... None
Surface winds during soaring window............ Between 20 mph and 30 mph
Height of the -3 thermal index................. 23559 ft MSL (15896 ft AGL)
Thermal soaring outlook for Wednesday 06/12.... Excellent

Wave Soaring Index............................. Poor
Wave Soaring Index trend (to 1800 MDT)......... Improving
Height of stable layer (12-18K ft MSL)......... None
Weak PVA/NVA (through 1800 MDT)................ Neither
Potential height of wave....................... 40460 ft MSL (32797 ft AGL)
Wave soaring outlook for Wednesday 06/12....... Fair

Remarks...

Sunrise/Sunset.................... 05:33:23 / 20:24:31 MDT
Total possible sunshine........... 14 hr 51 min 8 sec (891 min 8 sec)
Altitude of sun at 12:59:06 MDT... 74.12 degrees

Upper air data from numerical model forecast valid on 06/11/2013 at 0600 MDT

Freezing level.................. 16709 ft MSL (9046 ft AGL)
Convective condensation level... 23859 ft MSL (16196 ft AGL)
Lifted condensation level....... 25370 ft MSL (17707 ft AGL)
Lifted index.................... -2.6
K index......................... +10.2

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  -62.7 -80.9   213   15    8   1.7   0.9   78.4 173.2    26.0      M    M
 45000  -59.4 -74.9   229   23   12   3.0   1.6   59.9 139.8    16.0      M    M
 40000  -54.5 -66.1   236   47   24   5.8   3.2   45.8 114.4     7.4      M    M
 38000  -51.0 -59.8   235   45   23   5.8   3.2   42.0 107.6     5.0      M    M
 36000  -47.5 -53.5   233   42   22   5.6   3.1   39.0 102.2     2.9      M    M
 34000  -43.0 -45.4   234   39   20   7.9   4.4   37.0  98.7     1.5      M    M
 32000  -38.2 -36.8   234   35   18   8.0   4.4   35.8  96.4     0.6      M    M
 30000  -33.2 -27.8   233   32   17   8.5   4.7   34.6  94.3    -0.3   2326 11.8
 29000  -30.6 -23.1   233   31   16   8.5   4.7   34.2  93.5    -0.7   2220 11.3
 28000  -27.4 -17.3   232   30   15   8.7   4.8   33.7  92.7    -1.0   2087 10.6
 27000  -24.8 -12.6   231   30   15   8.7   4.8   33.2  91.8    -1.5   1979 10.1
 26000  -22.2  -8.0   231   30   15   8.7   4.8   32.8  91.1    -1.8   1871  9.5
 25000  -19.6  -3.3   230   30   15   8.4   4.6   32.5  90.6    -2.1   1764  9.0
 24000  -17.3   0.9   230   30   16   7.9   4.3   31.8  89.2    -2.8   1663  8.5
 23000  -14.9   5.2   230   31   16   7.9   4.3   31.1  88.0    -3.4   1563  7.9
 22000  -12.6   9.3   230   31   16   7.9   4.3   30.5  87.0    -3.9   1464  7.4
 21000  -10.2  13.6   230   31   16   7.9   4.3   29.8  85.6    -4.6   1364  6.9
 20000   -7.9  17.8   229   30   15   7.9   4.3   29.2  84.5    -5.3   1265  6.4
 19500   -6.7  19.9   229   30   15   8.0   4.4   28.9  84.0    -5.6   1215  6.2
 19000   -5.6  21.9   230   29   15   7.8   4.3   28.6  83.5    -5.9   1166  5.9
 18500   -4.4  24.1   231   29   15   7.9   4.3   28.3  82.9    -6.3   1116  5.7
 18000   -3.3  26.1   233   29   15   8.1   4.5   28.0  82.3    -6.6   1067  5.4
 17500   -2.1  28.2   234   27   14   8.3   4.6   27.7  81.9    -6.9   1015  5.2
 17000   -0.8  30.6   234   26   13   8.3   4.6   27.5  81.5    -7.2    964  4.9
 16500    0.5  32.9   234   25   13   9.0   5.0   27.3  81.2    -7.4    910  4.6
 16000    1.8  35.2   234   24   12   9.0   4.9   27.2  80.9    -7.6    855  4.3
 15500    3.1  37.6   234   23   12   9.3   5.1   27.1  80.7    -7.7    800  4.1
 15000    4.5  40.1   233   22   11   9.4   5.2   27.0  80.6    -7.8    743  3.8
 14500    5.9  42.6   233   21   11   9.5   5.2   27.0  80.6    -7.9    686  3.5
 14000    7.4  45.3   233   20   10   9.6   5.3   26.9  80.5    -8.0    629  3.2
 13500    8.8  47.8   234   19   10   9.6   5.3   26.9  80.5    -8.0    571  2.9
 13000   10.2  50.4   234   18    9   9.5   5.2   26.9  80.4    -8.1    513  2.6
 12500   11.6  52.9   234   18    9   9.5   5.2   26.8  80.3    -8.2    456  2.3
 12000   13.0  55.4   235   19   10   9.1   5.0   26.8  80.2    -8.3    400  2.0
 11750   13.7  56.7   236   19   10   9.1   5.0   26.7  80.1    -8.4    372  1.9
 11500   14.4  57.9   238   19   10   9.3   5.1   26.7  80.0    -8.5    344  1.7
 11250   15.1  59.2   239   19   10   8.5   4.7   26.6  79.9    -8.5    316  1.6
 11000   15.7  60.3   242   19   10   7.4   4.1   26.5  79.6    -8.7    291  1.5
 10750   16.3  61.3   246   19   10   7.4   4.1   26.3  79.3    -8.9    266  1.4
 10500   16.8  62.2   250   20   10   7.4   4.1   26.1  79.0    -9.1    242  1.2
 10250   17.9  64.2   258   20   10   6.9   3.8   25.7  78.3    -9.5    194  1.0
 10000   18.4  65.1   263   20   10   6.8   3.7   25.5  77.9    -9.7    171  0.9
  9750   19.0  66.2   267   20   10   7.0   3.9   25.3  77.5   -10.0    148  0.8
  9500   19.5  67.1   272   20   10   6.3   3.4   25.1  77.1   -10.2    125  0.6
  9250   19.9  67.8   274   21   11   5.5   3.0   24.7  76.5   -10.5    105  0.5
  9000   20.3  68.5   274   22   11   4.0   2.2   24.4  75.9   -10.9     86  0.4
  8750   20.7  69.3   275   23   12   9.0   4.9   24.0  75.3   -11.3     67  0.3
  8500   21.1  70.0   275   23   12  -9.3  -5.1   23.7  74.6   -11.7     48  0.2
  8250   19.0  66.2   274   20   10 -36.7 -20.1   20.9  69.7   -14.5    103  0.5
  8000   16.4  61.5   272   16    8 -27.2 -14.9   17.6  63.7   -17.9    175  0.9
  7750   13.7  56.7   268   11    6 -60.2 -33.0   14.3  57.8   -21.3    246  1.3
  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 * * * * * *

           06/11/2013 at 0900 MDT          |       06/11/2013 at 1200 MDT
                                           |
K index... +8.6                            | K index... +4.0
                                           |
Height Temperature  Wnd WndSpd  Lapse Rate | Temperature  Wnd WndSpd  Lapse Rate
ft MSL deg C deg F  Dir kt m/s  C/km F/kft | deg C deg F  Dir kt m/s  C/km F/kft
--------------------------------------------------------------------------------
 50000 -62.0 -79.6  221  18 10   1.8   1.0 | -61.7 -79.1  214  22 12   2.2   1.2
 45000 -59.0 -74.2  228  25 13   2.6   1.4 | -58.3 -72.9  224  33 17   2.2   1.2
 40000 -54.7 -66.5  241  43 22   6.1   3.4 | -54.7 -66.5  240  52 27   6.3   3.4
 38000 -51.2 -60.2  236  44 23   5.9   3.2 | -51.1 -60.0  236  54 28   6.0   3.3
 36000 -47.2 -53.0  231  47 24   5.8   3.2 | -47.1 -52.8  232  57 29   5.9   3.2
 34000 -42.8 -45.0  230  44 23   7.5   4.1 | -42.7 -44.9  230  53 27   7.4   4.1
 32000 -38.3 -36.9  229  42 21   7.5   4.1 | -38.3 -36.9  227  48 25   7.4   4.1
 30000 -33.4 -28.1  226  38 20   8.3   4.6 | -33.5 -28.3  229  44 22   8.0   4.4
 29000 -30.9 -23.6  225  37 19   8.3   4.6 | -31.1 -24.0  230  41 21   8.1   4.4
 28000 -28.4 -19.1  223  35 18   8.2   4.5 | -28.7 -19.7  231  39 20   8.4   4.6
 27000 -26.0 -14.8  222  35 18   8.2   4.5 | -26.1 -15.0  232  40 21   8.7   4.8
 26000 -23.6 -10.5  222  35 18   8.2   4.5 | -23.5 -10.3  233  41 21   8.7   4.8
 25000 -21.1  -6.0  221  34 18   8.2   4.5 | -20.9  -5.6  234  42 22   8.8   4.8
 24000 -18.7  -1.7  221  35 18   8.4   4.6 | -18.4  -1.1  237  43 22   8.3   4.5
 23000 -15.6   3.9  222  35 18   8.4   4.6 | -15.3   4.5  240  43 22   8.3   4.6
 22000 -13.1   8.4  222  35 18   8.1   4.4 | -12.8   9.0  242  44 23   8.2   4.5
 21000 -10.8  12.6  223  35 18   8.0   4.4 | -10.4  13.3  241  43 22   8.2   4.5
 20000  -8.4  16.9  225  35 18   8.0   4.4 |  -8.0  17.6  241  43 22   8.2   4.5
 19500  -7.3  18.9  225  35 18   8.0   4.4 |  -6.7  19.9  240  42 22   8.0   4.4
 19000  -6.1  21.0  226  35 18   8.1   4.4 |  -5.6  21.9  239  42 22   7.1   3.9
 18500  -4.9  23.2  227  35 18   8.1   4.4 |  -4.6  23.7  237  42 22   7.2   4.0
 18000  -3.7  25.3  228  36 18   8.7   4.8 |  -3.5  25.7  235  42 22   8.2   4.5
 17500  -2.4  27.7  227  35 18   8.9   4.9 |  -2.3  27.9  233  41 21   8.5   4.7
 17000  -1.1  30.0  227  35 18   9.0   4.9 |  -1.0  30.2  231  40 20   8.4   4.6
 16500   0.3  32.5  227  35 18   9.3   5.1 |   0.2  32.4  232  38 20   7.8   4.3
 16000   1.7  35.1  227  34 17   9.3   5.1 |   1.4  34.5  234  36 19   7.8   4.3
 15500   3.0  37.4  228  33 17   8.7   4.8 |   2.6  36.7  236  34 17   8.7   4.7
 15000   4.4  39.9  230  32 16   8.7   4.8 |   3.8  38.8  238  29 15   8.8   4.8
 14500   5.7  42.3  233  30 16   9.1   5.0 |   5.1  41.2  241  24 13   9.2   5.1
 14000   7.1  44.8  236  30 15   9.4   5.1 |   6.6  43.9  241  23 12   9.6   5.3
 13500   8.6  47.5  239  30 15   9.3   5.1 |   8.0  46.4  241  21 11   9.7   5.3
 13000   9.9  49.8  241  29 15   9.0   4.9 |   9.5  49.1  241  20 10  10.0   5.5
 12500  11.3  52.3  243  29 15   9.0   4.9 |  10.9  51.6  241  20 10  10.0   5.5
 12000  12.6  54.7  245  28 14   8.2   4.5 |  12.4  54.3  241  20 10   9.6   5.3
 11750  13.2  55.8  246  27 14   8.3   4.5 |  13.1  55.6  241  19 10   9.7   5.3
 11500  13.9  57.0  247  26 13   8.5   4.6 |  13.8  56.8  241  19 10   9.6   5.3
 11250  14.5  58.1  248  25 13   7.6   4.1 |  14.6  58.3  241  19 10   9.9   5.4
 11000  15.0  59.0  249  26 13   6.7   3.6 |  15.3  59.5  241  19 10  10.2   5.6
 10750  15.5  59.9  251  26 13   6.9   3.8 |  16.1  61.0  241  19 10  10.1   5.5
 10500  16.0  60.8  253  26 14   6.7   3.7 |  16.8  62.2  241  18 10  10.1   5.5
 10250  16.5  61.7  254  27 14   7.2   3.9 |  17.6  63.7  241  18  9  10.1   5.5
 10000  17.1  62.8  254  25 13   7.7   4.2 |  18.3  64.9  241  18  9  10.1   5.5
  9750  18.2  64.8  254  21 11   7.7   4.2 |  19.8  67.6  241  18  9  10.1   5.6
  9500  18.7  65.7  253  19 10   7.5   4.1 |  20.6  69.1  241  17  9  10.1   5.5
  9250  19.3  66.7  255  19 10   7.3   4.0 |  21.3  70.3  241  17  9   9.8   5.4
  9000  19.8  67.6  258  18  9   7.6   4.2 |  22.1  71.8  241  17  9  10.3   5.7
  8750  20.3  68.5  260  18  9   6.5   3.6 |  22.8  73.0  241  17  9   8.6   4.7
  8500  20.8  69.4  262  17  9  11.1   6.1 |  23.6  74.5  241  16  8  15.1   8.3
  8250  21.9  71.4  262  15  8  16.7   9.1 |  25.1  77.2  241  15  8  23.5  12.9
  8000  23.0  73.4  262  12  6  12.5   6.9 |  26.6  79.9  241  14  7  18.1   9.9
  7750  24.1  75.4  261  10  5  24.1  13.2 |  28.2  82.8  242  13  7  33.7  18.5
  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

           06/11/2013 at 1500 MDT          |       06/11/2013 at 1800 MDT
                                           |
K index... +10.4                           | K index... +11.0
                                           |
Height Temperature  Wnd WndSpd  Lapse Rate | Temperature  Wnd WndSpd  Lapse Rate
ft MSL deg C deg F  Dir kt m/s  C/km F/kft | deg C deg F  Dir kt m/s  C/km F/kft
--------------------------------------------------------------------------------
 50000 -61.1 -78.0  235  30 15   2.6   1.4 | -62.0 -79.6  251  31 16   2.5   1.4
 45000 -57.5 -71.5  236  44 23   1.7   0.9 | -58.2 -72.8  257  49 25   2.5   1.4
 40000 -54.5 -66.1  241  54 28   6.5   3.6 | -54.1 -65.4  257  59 30   6.5   3.6
 38000 -50.8 -59.4  239  55 28   6.1   3.4 | -50.4 -58.7  257  56 29   6.2   3.4
 36000 -46.7 -52.1  237  56 29   6.0   3.3 | -46.2 -51.2  256  53 27   6.1   3.4
 34000 -42.7 -44.9  239  54 28   6.9   3.8 | -42.1 -43.8  261  51 26   7.0   3.8
 32000 -38.5 -37.3  241  52 27   6.9   3.8 | -37.9 -36.2  267  50 26   7.0   3.8
 30000 -33.9 -29.0  242  49 25   8.0   4.4 | -33.5 -28.3  269  48 25   7.4   4.0
 29000 -31.5 -24.7  242  48 24   8.0   4.4 | -31.3 -24.3  270  46 24   7.4   4.0
 28000 -29.1 -20.4  242  46 24   8.4   4.6 | -29.2 -20.6  271  44 23   8.0   4.4
 27000 -26.5 -15.7  244  46 24   8.8   4.8 | -26.6 -15.9  270  42 22   8.6   4.7
 26000 -23.9 -11.0  246  47 24   8.8   4.8 | -24.0 -11.2  269  40 20   8.6   4.7
 25000 -21.3  -6.3  247  47 24   8.8   4.8 | -21.4  -6.5  268  37 19   8.6   4.7
 24000 -18.7  -1.7  247  46 24   8.8   4.8 | -18.8  -1.8  267  37 19   9.1   5.0
 23000 -15.4   4.3  246  45 23   8.8   4.8 | -15.4   4.3  265  38 20   9.1   5.0
 22000 -12.7   9.1  245  44 23   7.9   4.3 | -12.7   9.1  263  39 20   8.0   4.4
 21000 -10.5  13.1  246  41 21   7.3   4.0 | -10.5  13.1  259  37 19   7.5   4.1
 20000  -8.4  16.9  247  38 19   7.3   4.0 |  -8.3  17.1  255  36 18   7.6   4.1
 19500  -7.3  18.9  247  36 19   7.4   4.1 |  -7.2  19.0  253  35 18   7.6   4.2
 19000  -6.2  20.8  247  32 17   7.9   4.3 |  -6.0  21.2  251  34 17   8.2   4.5
 18500  -5.0  23.0  246  28 14   7.9   4.4 |  -4.8  23.4  250  32 16   8.2   4.5
 18000  -3.9  25.0  244  24 12   9.1   5.0 |  -3.6  25.5  249  30 15   8.9   4.9
 17500  -2.4  27.7  244  24 12   9.6   5.3 |  -2.3  27.9  249  29 15   9.2   5.1
 17000  -1.0  30.2  244  24 12   9.7   5.3 |  -0.9  30.4  249  27 14   9.2   5.1
 16500   0.5  32.9  243  24 12   9.8   5.4 |   0.5  32.9  249  26 13   9.2   5.1
 16000   1.9  35.4  243  23 12   9.8   5.4 |   1.8  35.2  250  25 13   9.2   5.1
 15500   3.4  38.1  242  23 12   9.9   5.4 |   3.2  37.8  251  24 12   9.5   5.2
 15000   4.9  40.8  241  22 12   9.9   5.4 |   4.6  40.3  253  24 12   9.6   5.3
 14500   6.3  43.3  240  22 11   9.9   5.4 |   6.0  42.8  255  23 12   9.4   5.2
 14000   7.8  46.0  239  22 11   9.9   5.4 |   7.4  45.3  257  23 12   9.2   5.0
 13500   9.3  48.7  238  21 11   9.9   5.4 |   8.8  47.8  260  22 11   9.3   5.1
 13000  10.7  51.3  238  21 11   9.8   5.4 |  10.2  50.4  261  22 11  10.0   5.5
 12500  12.2  54.0  237  20 11   9.8   5.4 |  11.7  53.1  262  22 11  10.0   5.5
 12000  13.7  56.7  236  20 10   9.7   5.3 |  13.2  55.8  262  22 11   9.6   5.3
 11750  14.4  57.9  236  20 10   9.7   5.3 |  13.9  57.0  263  21 11   9.7   5.3
 11500  15.1  59.2  235  20 10   9.6   5.3 |  14.6  58.3  263  21 11   9.6   5.3
 11250  15.8  60.4  235  20 10   9.8   5.4 |  15.3  59.5  263  21 11   9.7   5.3
 11000  16.6  61.9  234  20 10  10.1   5.5 |  16.1  61.0  264  21 11   9.9   5.4
 10750  17.3  63.1  234  19 10  10.0   5.5 |  16.8  62.2  264  21 11   9.9   5.4
 10500  18.1  64.6  234  19 10  10.1   5.5 |  17.5  63.5  265  21 11   9.8   5.4
 10250  18.8  65.8  233  19 10  10.0   5.5 |  18.3  64.9  265  21 11  10.0   5.5
 10000  19.6  67.3  233  19 10  10.0   5.5 |  19.0  66.2  266  21 11  10.1   5.6
  9750  21.1  70.0  232  18  9  10.0   5.5 |  20.5  68.9  266  20 11  10.2   5.6
  9500  21.8  71.2  232  18  9  10.1   5.5 |  21.3  70.3  267  20 10  10.1   5.5
  9250  22.6  72.7  231  18  9  10.1   5.5 |  22.0  71.6  267  20 10   9.8   5.4
  9000  23.3  73.9  231  18  9  10.5   5.7 |  22.8  73.0  268  20 10  10.0   5.5
  8750  24.1  75.4  231  17  9   9.2   5.1 |  23.5  74.3  269  19 10   9.4   5.1
  8500  24.8  76.6  230  17  9  13.8   7.6 |  24.2  75.6  269  19 10  11.6   6.4
  8250  26.2  79.2  230  16  8  21.5  11.8 |  25.2  77.4  270  18  9  15.0   8.3
  8000  27.7  81.9  229  15  8  20.3  11.1 |  26.3  79.3  270  16  8  14.2   7.8
  7750  29.3  84.7  229  13  7  26.7  14.6 |  27.4  81.3  270  14  7  17.8   9.8
  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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