Soaring Guidance
Issued by NWS Pueblo, CO

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000
UXUS97 KPUB 131248
SRGPUB

SOARING FORECAST
NATIONAL WEATHER SERVICE PUEBLO CO
648 AM MDT THU JUN 13 2013


EXPERIMENTAL PRODUCT

This forecast is for Thursday June 13, 2013:

If the trigger temperature of 77.0 F/25.0 C is reached...then
   Thermal Soaring Index....................... Excellent
   Maximum rate of lift........................ 1736 ft/min (8.8 m/s)
   Maximum height of thermals.................. 24780 ft MSL (17119 ft AGL)

Forecast maximum temperature................... 89.0 F/32.1 C
Time of trigger temperature.................... 1015 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................. 20557 ft MSL (12896 ft AGL)
Thermal soaring outlook for Friday 06/14....... Excellent

Wave Soaring Index............................. Poor
Wave Soaring Index trend (to 1800 MDT)......... Poor
Height of stable layer (12-18K ft MSL)......... None
Weak PVA/NVA (through 1800 MDT)................ Weak PVA
Potential height of wave....................... 22209 ft MSL (14548 ft AGL)
Wave soaring outlook for Friday 06/14.......... Poor

Remarks...

Sunrise/Sunset.................... 05:33:17 / 20:25:26 MDT
Total possible sunshine........... 14 hr 52 min 8 sec (892 min 8 sec)
Altitude of sun at 12:59:31 MDT... 74.24 degrees

Upper air data from numerical model forecast valid on 06/13/2013 at 0600 MDT

Freezing level.................. 16694 ft MSL (9033 ft AGL)
Convective condensation level... 20697 ft MSL (13036 ft AGL)
Lifted condensation level....... 22122 ft MSL (14462 ft AGL)
Lifted index.................... -2.9
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  -63.7 -82.7   250   27   14   2.4   1.3   77.2 170.9    27.2      M    M
 45000  -60.1 -76.2   249   28   14   1.9   1.0   59.1 138.4    17.6      M    M
 40000  -56.3 -69.3   230   36   18   7.6   4.2   43.2 109.8     7.9      M    M
 38000  -51.6 -60.9   226   35   18   7.8   4.3   41.3 106.3     6.8      M    M
 36000  -46.9 -52.4   222   35   18   7.7   4.2   40.0 104.0     6.0      M    M
 34000  -41.9 -43.4   219   34   18   8.5   4.7   38.7 101.6     5.2      M    M
 32000  -36.8 -34.2   216   34   17   8.6   4.7   37.9 100.2     4.7      M    M
 30000  -32.2 -26.0   221   29   15   7.5   4.1   36.2  97.1     3.4      M    M
 29000  -29.9 -21.8   225   26   13   7.5   4.1   35.4  95.7     2.8      M    M
 28000  -27.1 -16.8   231   24   12   7.5   4.1   34.4  94.0     2.1      M    M
 27000  -24.9 -12.8   238   24   12   7.5   4.1   33.5  92.2     1.4      M    M
 26000  -22.6  -8.7   245   25   13   7.5   4.1   32.6  90.7     0.7      M    M
 25000  -20.4  -4.7   251   27   14   7.3   4.0   31.9  89.4     0.1      M    M
 24000  -18.2  -0.8   250   29   15   7.2   4.0   30.9  87.6    -0.8   1656  8.4
 23000  -16.1   3.0   249   32   17   7.3   4.0   30.0  86.0    -1.6   1562  7.9
 22000  -13.9   7.0   248   35   18   8.1   4.5   29.3  84.7    -2.3   1468  7.5
 21000  -11.4  11.5   248   33   17   8.5   4.7   28.7  83.7    -2.8   1363  6.9
 20000   -8.9  16.0   248   32   17   8.5   4.7   28.3  83.0    -3.2   1257  6.4
 19500   -7.6  18.3   248   32   16   8.6   4.7   28.2  82.7    -3.4   1205  6.1
 19000   -6.3  20.7   247   30   16   8.7   4.8   28.0  82.4    -3.6   1151  5.8
 18500   -5.0  23.0   246   29   15   8.7   4.7   27.8  82.1    -3.8   1097  5.6
 18000   -3.7  25.3   245   27   14   9.2   5.0   27.7  81.8    -3.9   1043  5.3
 17500   -2.3  27.9   244   26   13   9.3   5.1   27.6  81.6    -4.0    986  5.0
 17000   -0.9  30.4   243   25   13   9.3   5.1   27.5  81.5    -4.1    930  4.7
 16500    0.4  32.7   243   24   12   9.0   4.9   27.4  81.3    -4.3    874  4.4
 16000    1.8  35.2   243   23   12   9.0   4.9   27.3  81.1    -4.4    819  4.2
 15500    3.1  37.6   244   22   11   8.8   4.8   27.2  80.9    -4.5    764  3.9
 15000    4.4  39.9   246   21   11   8.8   4.8   27.0  80.6    -4.7    710  3.6
 14500    5.7  42.3   248   21   11   8.7   4.8   26.9  80.3    -4.9    655  3.3
 14000    7.0  44.6   252   21   11   8.6   4.7   26.7  80.0    -5.1    602  3.1
 13500    8.3  46.9   256   22   11   8.5   4.6   26.5  79.7    -5.3    548  2.8
 13000    9.5  49.1   261   23   12   8.0   4.4   26.2  79.2    -5.6    497  2.5
 12500   10.7  51.3   267   24   13   8.0   4.4   26.0  78.7    -5.8    446  2.3
 12000   12.0  53.6   269   24   12   8.0   4.4   25.7  78.2    -6.1    395  2.0
 11750   12.6  54.7   269   24   12   8.0   4.4   25.6  78.0    -6.3    370  1.9
 11500   13.2  55.8   270   23   12   8.0   4.4   25.4  77.8    -6.4    344  1.7
 11250   13.8  56.8   270   22   11   8.2   4.5   25.3  77.5    -6.6    319  1.6
 11000   14.4  57.9   270   20   10   8.4   4.6   25.2  77.3    -6.7    293  1.5
 10750   15.0  59.0   269   18    9   8.2   4.5   25.1  77.1    -6.9    267  1.4
 10500   15.6  60.1   268   17    9   8.8   4.8   24.9  76.9    -7.0    242  1.2
 10250   16.2  61.2   268   15    8   5.6   3.1   24.8  76.7    -7.2    217  1.1
 10000   16.6  61.9   274   13    7   3.5   1.9   23.8  74.9    -8.3    190  1.0
  9750   16.8  62.2   277   12    6   4.0   2.2   23.3  74.0    -8.8    177  0.9
  9500   16.9  62.4   280   11    6  -0.4  -0.2   22.8  73.1    -9.4    165  0.8
  9250   16.6  61.9   276    9    5  -4.2  -2.3   21.8  71.2   -10.5    168  0.9
  9000   16.3  61.3   269    7    3  -3.1  -1.7   20.8  69.4   -11.6    170  0.9
  8750   15.9  60.6   256    5    2  -3.5  -1.9   19.8  67.7   -12.7    172  0.9
  8500   15.6  60.1   241    3    2  -5.6  -3.1   18.8  65.8   -13.8    176  0.9
  8250   15.0  59.0   269    3    1  -7.5  -4.1   17.5  63.5   -15.1    184  0.9
  8000   14.5  58.1   298    3    2  -6.1  -3.3   16.2  61.2   -16.4    192  1.0
  7750   14.0  57.2   318    4    2  -9.9  -5.4   15.0  59.0   -17.7    200  1.0
  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 * * * * * *

           06/13/2013 at 0900 MDT          |       06/13/2013 at 1200 MDT
                                           |
K index... +14.2                           | K index... +21.0
                                           |
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 -63.4 -82.1  243  26 13   2.6   1.4 | -63.3 -81.9  230  27 14   2.8   1.5
 45000 -59.7 -75.5  238  29 15   2.1   1.1 | -59.3 -74.7  229  33 17   2.0   1.1
 40000 -55.9 -68.6  225  38 19   7.4   4.1 | -55.6 -68.1  225  40 21   6.9   3.8
 38000 -51.5 -60.7  224  37 19   7.4   4.1 | -51.3 -60.3  224  41 21   7.1   3.9
 36000 -46.5 -51.7  223  37 19   7.4   4.1 | -47.1 -52.8  223  42 22   7.1   3.9
 34000 -42.0 -43.6  224  34 18   7.4   4.1 | -42.8 -45.0  226  40 21   7.2   3.9
 32000 -37.6 -35.7  226  32 16   7.4   4.1 | -38.5 -37.3  230  37 19   7.2   3.9
 30000 -33.0 -27.4  229  28 14   7.7   4.2 | -33.8 -28.8  229  34 18   7.9   4.3
 29000 -30.7 -23.3  231  26 13   7.7   4.2 | -31.5 -24.7  228  33 17   7.9   4.3
 28000 -28.4 -19.1  233  24 12   8.1   4.4 | -28.5 -19.3  227  31 16   8.0   4.4
 27000 -26.0 -14.8  235  24 12   8.2   4.5 | -26.1 -15.0  226  31 16   7.9   4.4
 26000 -23.5 -10.3  237  25 13   8.2   4.5 | -23.7 -10.7  225  32 16   8.0   4.4
 25000 -21.0  -5.8  239  25 13   8.0   4.4 | -21.3  -6.3  224  32 16   7.8   4.3
 24000 -18.9  -2.0  238  26 13   7.2   4.0 | -19.0  -2.2  227  32 17   7.8   4.3
 23000 -16.2   2.8  237  27 14   7.3   4.0 | -16.7   1.9  230  33 17   7.8   4.3
 22000 -14.0   6.8  236  28 15   8.0   4.4 | -14.4   6.1  232  33 17   8.5   4.6
 21000 -11.7  10.9  235  29 15   8.1   4.4 | -11.8  10.8  231  33 17   8.7   4.8
 20000  -9.3  15.3  235  30 16   8.2   4.5 |  -9.3  15.3  230  32 17   8.8   4.8
 19500  -8.2  17.2  235  31 16   8.6   4.7 |  -8.0  17.6  230  32 16   8.7   4.8
 19000  -6.8  19.8  237  30 16   9.1   5.0 |  -6.7  19.9  232  30 16   8.6   4.7
 18500  -5.5  22.1  239  30 15   9.0   5.0 |  -5.5  22.1  234  29 15   8.5   4.7
 18000  -4.1  24.6  240  29 15   9.6   5.3 |  -4.2  24.4  236  27 14   9.1   5.0
 17500  -2.7  27.1  240  27 14   9.6   5.3 |  -2.9  26.8  238  25 13   9.1   5.0
 17000  -1.3  29.7  240  26 13   9.4   5.2 |  -1.5  29.3  240  24 12   9.2   5.1
 16500   0.1  32.2  240  24 12   9.2   5.0 |  -0.1  31.8  241  23 12   9.5   5.2
 16000   1.5  34.7  239  22 11   9.2   5.0 |   1.3  34.3  242  22 11   9.4   5.2
 15500   2.9  37.2  239  21 11   9.6   5.2 |   2.7  36.9  243  20 11   9.8   5.4
 15000   4.3  39.7  238  20 10   9.6   5.2 |   4.2  39.6  242  19 10   9.8   5.4
 14500   5.7  42.3  239  20 10   9.0   4.9 |   5.6  42.1  241  18  9   9.5   5.2
 14000   7.0  44.6  240  19 10   8.9   4.9 |   7.0  44.6  241  17  9   9.4   5.1
 13500   8.4  47.1  241  19 10   8.8   4.9 |   8.4  47.1  240  16  8   9.4   5.1
 13000   9.7  49.5  241  19 10   8.8   4.8 |   9.8  49.6  238  15  8   9.4   5.2
 12500  11.0  51.8  241  19 10   8.7   4.8 |  11.2  52.2  236  14  7   9.4   5.1
 12000  12.3  54.1  243  19 10   8.6   4.7 |  12.6  54.7  233  13  7   9.2   5.0
 11750  13.0  55.4  244  18  9   8.5   4.7 |  13.3  55.9  232  13  7   9.2   5.1
 11500  13.6  56.5  245  18  9   8.7   4.7 |  14.0  57.2  230  12  6   9.1   5.0
 11250  14.3  57.7  245  18  9   9.0   4.9 |  14.6  58.3  227  12  6   8.6   4.7
 11000  14.9  58.8  246  17  9   9.1   5.0 |  15.3  59.5  223  11  6   8.4   4.6
 10750  15.6  60.1  246  16  8   9.1   5.0 |  15.9  60.6  219  11  5   8.5   4.6
 10500  16.3  61.3  246  16  8   9.0   4.9 |  16.5  61.7  214  10  5   8.5   4.7
 10250  16.9  62.4  247  15  8   8.4   4.6 |  17.8  64.0  203   9  5   9.2   5.0
 10000  17.5  63.5  249  14  7   8.1   4.4 |  18.4  65.1  196   9  5   9.1   5.0
  9750  18.1  64.6  250  14  7   8.4   4.6 |  19.1  66.4  190   9  5   9.2   5.1
  9500  19.1  66.4  253  12  6   2.9   1.6 |  19.7  67.5  184   9  5   9.9   5.4
  9250  19.1  66.4  252  11  6   0.8   0.4 |  20.5  68.9  180   9  5  10.5   5.8
  9000  19.1  66.4  252  11  6   1.0   0.6 |  21.3  70.3  177  10  5  10.0   5.5
  8750  19.1  66.4  251  10  5   2.9   1.6 |  22.0  71.6  174  10  5  11.3   6.2
  8500  19.4  66.9  248   9  4   8.6   4.7 |  23.0  73.4  171  10  5  16.4   9.0
  8250  20.1  68.2  241   6  3  11.1   6.1 |  24.4  75.9  170  10  5  19.4  10.7
  8000  20.8  69.4  227   4  2   9.5   5.2 |  25.7  78.3  168   9  5  17.2   9.5
  7750  21.5  70.7  197   3  2  14.0   7.7 |  27.1  80.8  167   9  5  23.0  12.6
  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

           06/13/2013 at 1500 MDT          |       06/13/2013 at 1800 MDT
                                           |
K index... +22.4                           | K index... +22.1
                                           |
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 -63.4 -82.1  230  28 14   2.8   1.5 | -63.8 -82.8  235  30 15   2.9   1.6
 45000 -59.3 -74.7  233  36 19   2.2   1.2 | -59.5 -75.1  237  38 20   2.1   1.1
 40000 -55.4 -67.7  236  44 22   6.3   3.5 | -55.7 -68.3  235  42 22   6.7   3.7
 38000 -51.5 -60.7  236  43 22   6.5   3.6 | -51.5 -60.7  234  41 21   6.9   3.8
 36000 -47.6 -53.7  236  43 22   6.3   3.5 | -47.4 -53.3  234  40 21   6.8   3.7
 34000 -42.9 -45.2  234  42 21   8.0   4.4 | -42.6 -44.7  233  38 20   8.2   4.5
 32000 -38.2 -36.8  233  40 21   8.0   4.4 | -37.7 -35.9  232  37 19   8.2   4.5
 30000 -33.3 -27.9  229  39 20   8.2   4.5 | -32.8 -27.0  232  35 18   8.3   4.5
 29000 -30.8 -23.4  227  39 20   8.2   4.5 | -30.3 -22.5  232  34 17   8.3   4.5
 28000 -27.8 -18.0  225  38 20   7.7   4.2 | -27.3 -17.1  233  33 17   7.5   4.1
 27000 -25.5 -13.9  226  37 19   7.7   4.2 | -25.0 -13.0  236  33 17   7.6   4.2
 26000 -23.2  -9.8  228  36 18   7.7   4.3 | -22.7  -8.9  239  33 17   7.6   4.2
 25000 -20.9  -5.6  229  34 18   7.8   4.3 | -20.4  -4.7  242  34 17   7.7   4.2
 24000 -18.5  -1.3  231  32 17   7.9   4.3 | -18.1  -0.6  242  33 17   7.7   4.2
 23000 -16.2   2.8  233  30 16   7.9   4.3 | -15.8   3.6  242  32 16   7.8   4.3
 22000 -13.8   7.2  236  28 15   7.7   4.2 | -13.6   7.5  242  31 16   7.5   4.1
 21000 -11.6  11.1  237  27 14   7.6   4.2 | -11.4  11.5  241  30 15   7.4   4.0
 20000  -9.4  15.1  238  25 13   7.6   4.2 |  -9.2  15.4  239  29 15   7.4   4.1
 19500  -8.3  17.1  239  25 13   8.0   4.4 |  -8.2  17.2  238  28 15   7.7   4.2
 19000  -7.0  19.4  238  24 12   9.2   5.0 |  -6.9  19.6  235  27 14   9.0   4.9
 18500  -5.7  21.7  237  24 12   9.1   5.0 |  -5.6  21.9  231  26 14   8.9   4.9
 18000  -4.3  24.3  235  23 12   9.6   5.3 |  -4.3  24.3  228  26 13   9.7   5.3
 17500  -2.8  27.0  235  23 12   9.7   5.3 |  -2.8  27.0  227  25 13   9.9   5.4
 17000  -1.4  29.5  235  23 12   9.8   5.4 |  -1.4  29.5  226  25 13   9.8   5.4
 16500   0.1  32.2  234  23 12   9.8   5.4 |   0.1  32.2  225  25 13   9.7   5.3
 16000   1.5  34.7  234  23 12   9.8   5.4 |   1.5  34.7  224  24 13   9.7   5.3
 15500   3.0  37.4  233  23 12   9.8   5.4 |   3.0  37.4  223  24 12   9.8   5.4
 15000   4.5  40.1  233  23 12   9.8   5.4 |   4.4  39.9  223  24 12   9.8   5.4
 14500   5.9  42.6  232  23 12   9.7   5.3 |   5.9  42.6  222  24 12   9.6   5.2
 14000   7.4  45.3  231  23 12   9.6   5.3 |   7.3  45.1  220  23 12   9.4   5.2
 13500   8.8  47.8  230  23 12   9.4   5.2 |   8.7  47.7  218  23 12   9.3   5.1
 13000  10.1  50.2  225  23 12   9.1   5.0 |  10.0  50.0  215  22 11   9.1   5.0
 12500  11.5  52.7  220  23 12   9.1   5.0 |  11.4  52.5  212  22 11   9.1   5.0
 12000  12.8  55.0  215  23 12   8.9   4.9 |  12.7  54.9  206  21 11   8.4   4.6
 11750  13.5  56.3  213  23 12   8.9   4.9 |  13.3  55.9  203  21 11   8.4   4.6
 11500  14.1  57.4  211  23 12   8.9   4.9 |  13.9  57.0  200  21 11   8.4   4.6
 11250  14.8  58.6  208  23 12   8.6   4.7 |  14.5  58.1  197  21 11   8.9   4.9
 11000  15.4  59.7  205  23 12   8.4   4.6 |  15.2  59.4  194  21 11   9.4   5.1
 10750  16.0  60.8  202  23 12   8.5   4.6 |  15.9  60.6  191  21 11   9.3   5.1
 10500  16.6  61.9  198  23 12   8.4   4.6 |  16.5  61.7  188  21 11   9.3   5.1
 10250  17.9  64.2  192  23 12   9.4   5.1 |  17.9  64.2  185  21 11   9.6   5.3
 10000  18.6  65.5  189  23 12   9.3   5.1 |  18.7  65.7  184  21 11   9.6   5.2
  9750  19.3  66.7  186  23 12   9.3   5.1 |  19.4  66.9  182  21 11   9.5   5.2
  9500  19.9  67.8  183  23 12   9.5   5.2 |  20.1  68.2  181  20 11   9.7   5.3
  9250  20.7  69.3  182  23 12   9.6   5.3 |  20.8  69.4  181  20 10   9.9   5.5
  9000  21.4  70.5  182  22 12   9.6   5.2 |  21.6  70.9  180  20 10  10.0   5.5
  8750  22.1  71.8  181  22 12   9.6   5.3 |  22.3  72.1  180  20 10   9.8   5.3
  8500  22.9  73.2  181  22 11  12.2   6.7 |  23.1  73.6  179  20 10  11.8   6.5
  8250  23.9  75.0  179  20 10  14.4   7.9 |  24.0  75.2  177  18  9  14.0   7.7
  8000  24.9  76.8  177  18  9  12.8   7.0 |  24.9  76.8  175  16  8  12.4   6.8
  7750  25.9  78.6  175  16  8  17.3   9.5 |  25.9  78.6  172  14  7  16.8   9.2
  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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