Soaring Guidance
Issued by NWS Pueblo, CO

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000
UXUS97 KPUB 161016
SRGPUB

SOARING FORECAST
NATIONAL WEATHER SERVICE PUEBLO CO
416 AM MDT THU MAY 16 2013


EXPERIMENTAL PRODUCT

This forecast is for Thursday May 16, 2013:

If the trigger temperature of 63.7 F/17.6 C is reached...then
   Thermal Soaring Index....................... Excellent
   Maximum rate of lift........................ 1668 ft/min (8.5 m/s)
   Maximum height of thermals.................. 24451 ft MSL (16791 ft AGL)

Forecast maximum temperature................... 78.0 F/26.0 C
Time of trigger temperature.................... 0830 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................. 21505 ft MSL (13845 ft AGL)
Thermal soaring outlook for Friday 05/17....... Good

Wave Soaring Index............................. Poor
Wave Soaring Index trend (to 1800 MDT)......... No change
Height of stable layer (12-18K ft MSL)......... None
Weak PVA/NVA (through 1800 MDT)................ Weak PVA
Potential height of wave....................... 35274 ft MSL (27614 ft AGL)
Wave soaring outlook for Friday 05/17.......... Poor

Remarks...

Sunrise/Sunset.................... 05:45:38 / 20:05:31 MDT
Total possible sunshine........... 14 hr 19 min 53 sec (859 min 53 sec)
Altitude of sun at 12:55:46 MDT... 70.27 degrees

Upper air data from numerical model forecast valid on 05/16/2013 at 0600 MDT

Freezing level.................. 13698 ft MSL (6038 ft AGL)
Convective condensation level... 15860 ft MSL (8200 ft AGL)
Lifted condensation level....... 18801 ft MSL (11141 ft AGL)
Lifted index.................... -5.2
K index......................... +17.0

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  -60.8 -77.4   270   19   10   0.7   0.4   85.3 185.5    35.4      M    M
 45000  -59.9 -75.8   258   21   11  -0.2  -0.1   63.2 145.8    23.9      M    M
 40000  -60.3 -76.5   265   42   22  -0.8  -0.4   40.3 104.6    10.1      M    M
 38000  -56.7 -70.1   263   46   23   7.3   4.0   36.9  98.3     7.9      M    M
 36000  -52.3 -62.1   261   48   25   7.3   4.0   34.9  94.8     6.7      M    M
 34000  -47.5 -53.5   260   50   26   8.5   4.7   33.4  92.2     5.8      M    M
 32000  -42.4 -44.3   260   51   26   8.5   4.7   32.5  90.4     5.2      M    M
 30000  -37.5 -35.5   260   50   26   7.5   4.1   31.2  88.1     4.4      M    M
 29000  -35.3 -31.5   260   48   25   7.5   4.1   30.3  86.5     3.7      M    M
 28000  -32.5 -26.5   259   46   24   7.5   4.1   29.3  84.8     3.0      M    M
 27000  -30.4 -22.7   257   43   22   6.7   3.7   28.3  82.9     2.2      M    M
 26000  -28.4 -19.1   254   39   20   6.7   3.7   27.1  80.8     1.2      M    M
 25000  -26.3 -15.3   251   34   18   6.7   3.7   26.0  78.9     0.4      M    M
 24000  -24.4 -11.9   248   30   16   6.5   3.6   25.0  76.9    -0.5   1621  8.2
 23000  -22.4  -8.3   246   27   14   6.5   3.6   23.7  74.7    -1.6   1533  7.8
 22000  -20.5  -4.9   245   24   12   6.5   3.6   22.6  72.8    -2.6   1446  7.3
 21000  -18.6  -1.5   243   22   11   6.5   3.6   21.5  70.7    -3.6   1358  6.9
 20000  -16.6   2.1   241   21   11   6.5   3.6   20.4  68.7    -4.7   1271  6.5
 19500  -15.7   3.7   241   21   11   6.6   3.6   19.8  67.7    -5.2   1228  6.2
 19000  -14.7   5.5   240   20   11   6.9   3.8   19.4  66.8    -5.7   1184  6.0
 18500  -13.5   7.7   241   20   10   8.7   4.8   19.1  66.3    -6.0   1133  5.8
 18000  -12.3   9.9   242   20   11   8.6   4.7   18.9  66.0    -6.2   1081  5.5
 17500  -11.0  12.2   244   20   11   9.4   5.1   18.8  65.8    -6.4   1026  5.2
 17000   -9.5  14.9   247   20   11   9.5   5.2   18.7  65.7    -6.5    969  4.9
 16500   -8.1  17.4   250   21   11   9.5   5.2   18.7  65.6    -6.6    912  4.6
 16000   -6.7  19.9   253   20   11   9.5   5.2   18.6  65.5    -6.7    854  4.3
 15500   -5.3  22.5   256   20   11   9.5   5.2   18.6  65.4    -6.8    797  4.0
 15000   -3.9  25.0   259   20   10   9.5   5.2   18.5  65.4    -6.8    740  3.8
 14500   -2.5  27.5   261   20   10   9.5   5.2   18.5  65.3    -6.9    683  3.5
 14000   -1.0  30.2   264   20   10   9.4   5.1   18.4  65.2    -7.0    626  3.2
 13500    0.3  32.5   266   20   10   9.4   5.1   18.4  65.1    -7.1    569  2.9
 13000    1.7  35.1   268   20   10   9.4   5.2   18.3  65.0    -7.3    513  2.6
 12500    3.1  37.6   267   19   10   9.5   5.2   18.3  64.9    -7.4    456  2.3
 12000    4.5  40.1   266   19   10   9.4   5.2   18.2  64.8    -7.5    400  2.0
 11750    5.2  41.4   265   18   10   9.4   5.1   18.2  64.8    -7.5    372  1.9
 11500    5.9  42.6   264   18    9   9.4   5.1   18.2  64.7    -7.6    344  1.7
 11250    6.6  43.9   263   18    9   9.5   5.2   18.1  64.7    -7.7    316  1.6
 11000    7.3  45.1   262   18    9   9.0   4.9   18.1  64.6    -7.7    288  1.5
 10750    7.9  46.2   260   17    9   8.5   4.7   18.0  64.4    -7.9    262  1.3
 10500    8.5  47.3   257   16    8   8.6   4.7   17.9  64.3    -8.0    236  1.2
 10250    9.1  48.4   255   15    8   8.8   4.8   17.8  64.1    -8.2    211  1.1
 10000   10.2  50.4   248   13    7   7.4   4.1   17.6  63.7    -8.6    162  0.8
  9750   10.7  51.3   244   12    6   7.5   4.1   17.4  63.4    -8.8    139  0.7
  9500   11.3  52.3   239   11    6   7.9   4.3   17.3  63.1    -9.0    116  0.6
  9250   11.8  53.2   233   10    5   5.4   3.0   17.1  62.7    -9.3     94  0.5
  9000   12.0  53.6   236   11    6   2.8   1.5   16.6  61.9    -9.8     79  0.4
  8750   12.2  54.0   238   12    6   4.6   2.5   16.1  61.0   -10.3     65  0.3
  8500   12.4  54.3   240   14    7   0.0   0.0   15.7  60.2   -10.9     51  0.3
  8250   11.6  52.9   243   13    7 -24.8 -13.6   14.1  57.5   -12.4     68  0.3
  8000    8.6  47.5   249   10    5 -52.3 -28.7   10.4  50.7   -16.2    151  0.8
  7750    5.6  42.1   260    7    4  -7.6  -4.2    6.6  43.9   -20.0    235  1.2
  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 * * * * * *

           05/16/2013 at 0900 MDT          |       05/16/2013 at 1200 MDT
                                           |
K index... +13.6                           | K index... +16.4
                                           |
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 -60.3 -76.5  258  17  9   0.1   0.1 | -61.3 -78.3  252  19 10  -0.7  -0.4
 45000 -60.1 -76.2  262  22 11  -0.0  -0.0 | -62.2 -80.0  262  23 12   0.5   0.3
 40000 -60.2 -76.4  279  37 19  -0.7  -0.4 | -61.4 -78.5  285  31 16  -0.4  -0.2
 38000 -56.4 -69.5  281  39 20   7.4   4.1 | -57.1 -70.8  285  32 16   8.1   4.4
 36000 -51.9 -61.4  283  40 20   7.5   4.1 | -52.2 -62.0  284  32 17   8.1   4.4
 34000 -47.3 -53.1  283  40 21   8.0   4.4 | -47.3 -53.1  284  33 17   8.3   4.5
 32000 -42.4 -44.3  281  40 21   8.0   4.4 | -42.4 -44.3  284  33 17   8.3   4.6
 30000 -37.6 -35.7  280  40 20   8.2   4.5 | -37.4 -35.3  284  32 16   8.1   4.5
 29000 -35.1 -31.2  281  39 20   8.2   4.5 | -35.0 -31.0  284  31 16   8.1   4.5
 28000 -32.1 -25.8  283  38 20   8.2   4.5 | -31.9 -25.4  284  29 15   8.2   4.5
 27000 -29.8 -21.6  283  37 19   7.0   3.8 | -29.6 -21.3  285  28 14   7.3   4.0
 26000 -27.7 -17.9  283  35 18   7.0   3.8 | -27.5 -17.5  286  26 14   7.3   4.0
 25000 -25.6 -14.1  283  34 17   7.0   3.8 | -25.3 -13.5  287  25 13   7.3   4.0
 24000 -23.7 -10.7  282  31 16   6.2   3.4 | -23.2  -9.8  288  24 12   6.4   3.5
 23000 -21.8  -7.2  280  27 14   6.2   3.4 | -21.3  -6.3  289  24 12   6.4   3.5
 22000 -20.0  -4.0  277  23 12   6.3   3.4 | -19.4  -2.9  290  23 12   6.5   3.5
 21000 -18.1  -0.6  276  19 10   6.5   3.6 | -17.5   0.5  287  22 11   6.7   3.7
 20000 -16.2   2.8  276  15  8   6.5   3.6 | -15.5   4.1  281  19 10   6.7   3.7
 19500 -15.2   4.6  276  13  7   6.6   3.6 | -14.5   5.9  278  18  9   6.8   3.7
 19000 -14.2   6.4  277  11  5   6.8   3.7 | -13.5   7.7  274  17  9   7.3   4.0
 18500 -13.1   8.4  278  10  5   7.7   4.2 | -12.2  10.0  272  16  8   8.5   4.6
 18000 -12.0  10.4  280  10  5   7.6   4.2 | -11.0  12.2  270  15  7   8.4   4.6
 17500 -10.8  12.6  283   9  5   8.5   4.7 |  -9.7  14.5  270  13  7   8.4   4.6
 17000  -9.6  14.7  286  10  5   8.6   4.7 |  -8.5  16.7  273  12  6   8.4   4.6
 16500  -8.3  17.1  288  10  5   8.8   4.8 |  -7.3  18.9  277  11  6   8.3   4.5
 16000  -6.9  19.6  289  10  5   9.2   5.0 |  -6.1  21.0  282  11  6   8.2   4.5
 15500  -5.6  21.9  290  11  6   9.2   5.0 |  -4.9  23.2  287  10  5   8.3   4.5
 15000  -4.2  24.4  293  11  6   9.3   5.1 |  -3.7  25.3  291  10  5   9.0   4.9
 14500  -2.8  27.0  298  12  6   9.4   5.1 |  -2.4  27.7  295   8  4   8.9   4.9
 14000  -1.4  29.5  302  12  6   9.2   5.1 |  -1.1  30.0  298   8  4   9.8   5.4
 13500  -0.1  31.8  304  13  7   9.2   5.0 |   0.4  32.7  298   8  4   9.7   5.3
 13000   1.3  34.3  305  13  7   9.6   5.2 |   1.9  35.4  298   8  4  10.0   5.5
 12500   2.8  37.0  304  13  7   9.7   5.3 |   3.4  38.1  299   8  4  10.0   5.5
 12000   4.2  39.6  304  13  7   9.5   5.2 |   4.9  40.8  300   7  4   9.9   5.4
 11750   4.9  40.8  302  13  7   9.3   5.1 |   5.6  42.1  301   7  4   9.8   5.4
 11500   5.6  42.1  300  13  7   9.3   5.1 |   6.3  43.3  301   7  4   9.8   5.4
 11250   6.3  43.3  298  13  7   9.3   5.1 |   7.1  44.8  302   7  4   9.8   5.4
 11000   7.0  44.6  296  13  7   9.3   5.1 |   7.8  46.0  303   7  4  10.0   5.5
 10750   7.7  45.9  292  13  7   9.3   5.1 |   8.5  47.3  303   7  4  10.1   5.6
 10500   8.3  46.9  288  13  7   9.3   5.1 |   9.3  48.7  303   7  4  10.1   5.5
 10250   9.7  49.5  281  13  7   8.9   4.9 |  10.8  51.4  304   7  4  10.0   5.5
 10000  10.3  50.5  279  13  6   8.4   4.6 |  11.5  52.7  305   7  4   9.9   5.4
  9750  11.0  51.8  277  12  6   8.5   4.7 |  12.3  54.1  305   7  3   9.9   5.4
  9500  11.6  52.9  275  12  6   8.6   4.7 |  13.0  55.4  306   7  3   9.9   5.5
  9250  12.2  54.0  274  12  6   7.1   3.9 |  13.8  56.8  306   7  3  10.1   5.5
  9000  12.6  54.7  273  13  7   6.2   3.4 |  14.5  58.1  307   7  3  10.3   5.7
  8750  13.0  55.4  273  14  7   6.3   3.4 |  15.3  59.5  308   6  3   9.7   5.3
  8500  13.4  56.1  273  14  7   7.5   4.1 |  16.1  61.0  309   6  3  11.9   6.5
  8250  14.0  57.2  272  14  7  12.1   6.7 |  17.2  63.0  311   6  3  18.2  10.0
  8000  15.0  59.0  269  11  6  15.9   8.7 |  18.7  65.7  314   6  3  22.2  12.2
  7750  16.0  60.8  265   8  4  10.7   5.9 |  20.2  68.4  319   5  3  17.1   9.4
  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

           05/16/2013 at 1500 MDT          |       05/16/2013 at 1800 MDT
                                           |
K index... +25.9                           | K index... +24.3
                                           |
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 -61.7 -79.1  243  23 12  -0.2  -0.1 | -62.4 -80.3  251  26 13  -0.6  -0.3
 45000 -61.9 -79.4  262  27 14   0.7   0.4 | -63.0 -81.4  267  29 15   1.2   0.7
 40000 -60.8 -77.4  287  30 15   0.1   0.1 | -61.2 -78.2  285  32 17   1.2   0.6
 38000 -56.9 -70.4  286  31 16   7.6   4.2 | -56.8 -70.2  287  30 16   8.0   4.4
 36000 -51.7 -61.1  283  32 16   7.6   4.2 | -52.0 -61.6  288  28 14   8.0   4.4
 34000 -47.0 -52.6  282  31 16   8.2   4.5 | -47.1 -52.8  288  26 13   8.2   4.5
 32000 -42.0 -43.6  283  30 15   8.2   4.5 | -42.2 -44.0  288  25 13   8.2   4.5
 30000 -37.1 -34.8  284  29 15   8.4   4.6 | -37.2 -35.0  285  24 12   8.4   4.6
 29000 -34.6 -30.3  283  28 14   8.4   4.6 | -34.7 -30.5  283  25 13   8.4   4.6
 28000 -32.1 -25.8  283  27 14   8.4   4.6 | -31.6 -24.9  281  25 13   8.5   4.7
 27000 -29.7 -21.5  282  25 13   7.3   4.0 | -29.2 -20.6  277  24 13   7.6   4.2
 26000 -27.6 -17.7  281  24 12   7.3   4.0 | -26.9 -16.4  274  24 12   7.7   4.2
 25000 -25.4 -13.7  280  23 12   7.3   4.0 | -24.7 -12.5  269  23 12   7.7   4.2
 24000 -23.2  -9.8  279  22 11   6.9   3.8 | -22.5  -8.5  268  22 11   7.3   4.0
 23000 -20.7  -5.3  280  22 11   7.0   3.8 | -20.3  -4.5  269  21 11   7.3   4.0
 22000 -18.6  -1.5  281  22 11   7.0   3.9 | -18.1  -0.6  270  20 10   7.3   4.0
 21000 -16.6   2.1  280  21 11   6.9   3.8 | -16.1   3.0  271  20 10   6.9   3.8
 20000 -14.6   5.7  277  19 10   6.9   3.8 | -14.0   6.8  270  20 10   6.9   3.8
 19500 -13.6   7.5  276  19 10   6.9   3.8 | -13.0   8.6  270  20 10   6.9   3.8
 19000 -12.6   9.3  274  18  9   7.1   3.9 | -12.0  10.4  270  20 10   7.0   3.8
 18500 -11.5  11.3  275  15  8   7.2   3.9 | -11.0  12.2  271  18  9   7.0   3.9
 18000 -10.5  13.1  277  12  6   7.1   3.9 |  -9.9  14.2  272  17  9   7.0   3.8
 17500  -9.4  15.1  278  10  5   8.7   4.8 |  -8.9  16.0  272  15  8   7.6   4.2
 17000  -8.1  17.4  280   8  4   8.5   4.7 |  -7.8  18.0  272  13  7   7.6   4.2
 16500  -6.9  19.6  284   6  3   9.2   5.1 |  -6.7  19.9  272  11  5   8.2   4.5
 16000  -5.5  22.1  287   5  3   9.6   5.3 |  -5.4  22.3  272   9  5   8.8   4.8
 15500  -4.0  24.8  291   5  2   9.7   5.3 |  -4.1  24.6  273   7  4   8.9   4.9
 15000  -2.6  27.3  293   4  2  10.0   5.5 |  -2.7  27.1  273   6  3  10.1   5.5
 14500  -1.1  30.0  295   4  2  10.0   5.5 |  -1.2  29.8  273   6  3  10.0   5.5
 14000   0.4  32.7  296   4  2   9.7   5.3 |   0.3  32.5  273   6  3   9.8   5.4
 13500   1.8  35.2  298   4  2   9.7   5.3 |   1.8  35.2  274   5  3   9.8   5.4
 13000   3.3  37.9  300   4  2   9.7   5.3 |   3.2  37.8  276   5  3   9.6   5.3
 12500   4.7  40.5  301   3  2   9.7   5.3 |   4.6  40.3  279   4  2   9.6   5.3
 12000   6.2  43.2  303   3  2   9.8   5.4 |   6.0  42.8  286   3  2   9.4   5.1
 11750   6.9  44.4  306   3  2   9.8   5.4 |   6.7  44.1  293   2  1   9.2   5.1
 11500   7.7  45.9  308   3  1   9.8   5.4 |   7.4  45.3  305   2  1   9.3   5.1
 11250   8.4  47.1  311   3  1   9.8   5.4 |   8.1  46.6  324   2  1   9.2   5.1
 11000   9.1  48.4  313   3  1   9.9   5.5 |   8.8  47.8  348   1  1   9.3   5.1
 10750   9.9  49.8  315   2  1  10.1   5.5 |   9.5  49.1  005   2  1   9.4   5.2
 10500  10.6  51.1  317   2  1  10.0   5.5 |  10.2  50.4  017   2  1   9.4   5.2
 10250  11.3  52.3  320   2  1  10.0   5.5 |  11.6  52.9  029   3  2   9.6   5.3
 10000  12.1  53.8  322   2  1  10.0   5.5 |  12.3  54.1  030   3  2   9.8   5.4
  9750  12.8  55.0  327   2  1  10.0   5.5 |  13.0  55.4  031   4  2   9.8   5.4
  9500  14.3  57.7  338   2  1  10.0   5.5 |  13.8  56.8  032   4  2   9.8   5.4
  9250  15.0  59.0  343   2  1   9.7   5.3 |  14.5  58.1  032   4  2   9.6   5.3
  9000  15.8  60.4  345   2  1   9.5   5.2 |  15.2  59.4  033   4  2   9.6   5.2
  8750  16.5  61.7  348   2  1   9.4   5.1 |  15.9  60.6  034   4  2   9.5   5.2
  8500  17.2  63.0  351   2  1  10.1   5.5 |  16.6  61.9  035   4  2   9.7   5.3
  8250  18.0  64.4  003   2  1  13.6   7.4 |  17.4  63.3  036   4  2  10.6   5.8
  8000  19.1  66.4  036   2  1  17.1   9.4 |  18.1  64.6  040   4  2  11.5   6.3
  7750  20.2  68.4  059   2  1  11.7   6.4 |  18.8  65.8  044   4  2  10.4   5.7
  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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