Soaring Guidance
Issued by NWS Pueblo, CO

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000
UXUS97 KPUB 171135
SRGPUB

SOARING FORECAST
NATIONAL WEATHER SERVICE PUEBLO CO
534 AM MDT FRI MAY 17 2013


EXPERIMENTAL PRODUCT

This forecast is for Friday May 17, 2013:

If the trigger temperature of 66.3 F/19.1 C is reached...then
   Thermal Soaring Index....................... Excellent
   Maximum rate of lift........................ 1835 ft/min (9.3 m/s)
   Maximum height of thermals.................. 26183 ft MSL (18523 ft AGL)

Forecast maximum temperature................... 83.0 F/28.8 C
Time of trigger temperature.................... 0815 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................. 21367 ft MSL (13707 ft AGL)
Thermal soaring outlook for Saturday 05/18..... 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....................... 35772 ft MSL (28112 ft AGL)
Wave soaring outlook for Saturday 05/18........ Poor

Remarks...

Sunrise/Sunset.................... 05:44:47 / 20:06:25 MDT
Total possible sunshine........... 14 hr 21 min 37 sec (861 min 37 sec)
Altitude of sun at 12:55:47 MDT... 70.49 degrees

Upper air data from numerical model forecast valid on 05/17/2013 at 0600 MDT

Freezing level.................. 14202 ft MSL (6542 ft AGL)
Convective condensation level... 18048 ft MSL (10388 ft AGL)
Lifted condensation level....... 21186 ft MSL (13526 ft AGL)
Lifted index.................... -4.3
K index......................... +18.0

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  -61.2 -78.2   248   25   13  -1.0  -0.5   84.5 184.2    33.3      M    M
 45000  -62.4 -80.3   255   31   16   0.7   0.4   59.0 138.3    19.5      M    M
 40000  -61.3 -78.3   248   25   13   0.5   0.3   38.4 101.2     6.9      M    M
 38000  -57.0 -70.6   247   26   14   8.0   4.4   36.0  96.7     5.3      M    M
 36000  -52.1 -61.8   246   28   15   8.0   4.4   34.6  94.4     4.5      M    M
 34000  -47.2 -53.0   246   29   15   8.2   4.5   33.3  92.0     3.7      M    M
 32000  -42.3 -44.1   246   28   15   8.2   4.5   32.1  89.8     2.8      M    M
 30000  -37.4 -35.3   247   27   14   8.2   4.5   30.9  87.6     2.0      M    M
 29000  -35.0 -31.0   248   26   13   8.2   4.5   30.3  86.5     1.5      M    M
 28000  -31.9 -25.4   250   25   13   8.2   4.5   29.6  85.3     1.0      M    M
 27000  -29.5 -21.1   251   25   13   7.8   4.3   28.9  84.0     0.4      M    M
 26000  -27.2 -17.0   252   25   13   7.8   4.3   28.2  82.7    -0.2   1807  9.2
 25000  -24.8 -12.6   254   24   13   7.8   4.3   27.5  81.5    -0.7   1707  8.7
 24000  -22.5  -8.5   254   24   12   7.7   4.2   26.8  80.3    -1.3   1607  8.2
 23000  -20.1  -4.2   254   24   12   7.7   4.2   26.1  78.9    -2.0   1508  7.7
 22000  -17.8  -0.0   254   24   12   7.8   4.3   25.4  77.7    -2.5   1409  7.2
 21000  -15.8   3.6   252   22   11   6.4   3.5   24.4  75.9    -3.5   1318  6.7
 20000  -13.9   7.0   248   20   10   6.4   3.5   23.2  73.8    -4.6   1232  6.3
 19500  -12.9   8.8   245   19   10   6.5   3.5   22.7  72.8    -5.1   1189  6.0
 19000  -12.0  10.4   242   19   10   6.2   3.4   22.2  71.9    -5.6   1146  5.8
 18500  -11.2  11.8   236   17    9   5.7   3.1   21.5  70.7    -6.3   1107  5.6
 18000  -10.4  13.3   229   16    8   5.6   3.0   20.8  69.5    -7.1   1069  5.4
 17500   -9.4  15.1   224   15    8   9.4   5.1   20.4  68.8    -7.5   1023  5.2
 17000   -8.0  17.6   223   15    8   9.3   5.1   20.3  68.6    -7.7    967  4.9
 16500   -6.6  20.1   222   15    8   9.3   5.1   20.3  68.5    -7.8    910  4.6
 16000   -5.2  22.6   223   15    8   9.4   5.1   20.2  68.4    -7.9    853  4.3
 15500   -3.8  25.2   223   15    8   9.4   5.1   20.1  68.3    -8.0    796  4.0
 15000   -2.4  27.7   225   15    8   9.2   5.1   20.1  68.1    -8.1    740  3.8
 14500   -1.0  30.2   226   15    8   9.3   5.1   20.0  68.0    -8.2    683  3.5
 14000    0.4  32.7   228   15    8   9.2   5.1   19.9  67.8    -8.3    627  3.2
 13500    1.7  35.1   230   15    8   9.2   5.1   19.8  67.7    -8.4    571  2.9
 13000    3.1  37.6   232   15    8   9.4   5.2   19.8  67.6    -8.6    514  2.6
 12500    4.6  40.3   235   15    8   9.5   5.2   19.7  67.5    -8.6    456  2.3
 12000    6.0  42.8   238   15    8   9.2   5.1   19.7  67.4    -8.7    399  2.0
 11750    6.7  44.1   239   15    8   9.1   5.0   19.6  67.3    -8.8    371  1.9
 11500    7.3  45.1   240   15    8   9.1   5.0   19.6  67.2    -8.9    344  1.7
 11250    8.0  46.4   241   15    8   9.1   5.0   19.5  67.1    -9.0    316  1.6
 11000    8.7  47.7   241   15    8   8.9   4.9   19.5  67.0    -9.0    288  1.5
 10750    9.3  48.7   240   14    7   8.8   4.8   19.4  66.9    -9.2    261  1.3
 10500   10.0  50.0   238   13    7   8.8   4.8   19.3  66.8    -9.3    235  1.2
 10250   10.6  51.1   236   13    7   8.8   4.8   19.2  66.6    -9.4    208  1.1
 10000   11.9  53.4   230   11    6   8.0   4.4   19.0  66.3    -9.7    156  0.8
  9750   12.4  54.3   226   11    5   8.1   4.4   18.9  66.0    -9.8    131  0.7
  9500   13.0  55.4   221   10    5   8.0   4.4   18.8  65.8   -10.0    107  0.5
  9250   13.6  56.5   218    9    5   7.2   4.0   18.6  65.5   -10.2     82  0.4
  9000   14.0  57.2   220   10    5   6.1   3.3   18.4  65.1   -10.5     61  0.3
  8750   14.5  58.1   223   10    5   8.2   4.5   18.1  64.7   -10.8     40  0.2
  8500   15.0  59.0   225   10    5   1.1   0.6   17.9  64.2   -11.1     19  0.1
  8250   14.2  57.6   229   10    5 -22.7 -12.5   16.4  61.5   -12.7     35  0.2
  8000   11.6  52.9   234    8    4 -40.5 -22.2   13.2  55.7   -16.0    105  0.5
  7750    9.0  48.2   245    6    3 -15.2  -8.3    9.9  49.9   -19.3    175  0.9
  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 * * * * * *

           05/17/2013 at 0900 MDT          |       05/17/2013 at 1200 MDT
                                           |
K index... +0.7                            | K index... -0.4
                                           |
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 -61.3 -78.3  249  26 13  -0.9  -0.5 | -61.5 -78.7  240  24 13  -1.4  -0.7
 45000 -62.3 -80.1  243  28 15   0.9   0.5 | -63.0 -81.4  231  35 18   1.2   0.7
 40000 -60.9 -77.6  228  28 14   0.4   0.2 | -61.1 -78.0  231  34 18   0.7   0.4
 38000 -56.9 -70.4  229  26 14   7.5   4.1 | -57.1 -70.8  230  34 17   7.6   4.2
 36000 -52.4 -62.3  231  25 13   7.5   4.1 | -52.0 -61.6  230  33 17   7.6   4.2
 34000 -47.8 -54.0  233  24 13   8.0   4.4 | -47.3 -53.1  230  31 16   8.0   4.4
 32000 -42.9 -45.2  235  24 12   8.0   4.4 | -42.5 -44.5  230  30 15   8.0   4.4
 30000 -38.0 -36.4  236  24 12   8.3   4.5 | -37.7 -35.9  233  29 15   7.9   4.4
 29000 -34.9 -30.8  236  25 13   8.3   4.5 | -35.4 -31.7  236  28 15   7.9   4.4
 28000 -32.5 -26.5  236  26 13   8.3   4.6 | -33.0 -27.4  238  28 15   7.9   4.4
 27000 -30.1 -22.2  237  26 14   7.6   4.2 | -30.6 -23.1  238  28 15   7.7   4.2
 26000 -27.8 -18.0  239  27 14   7.6   4.2 | -28.3 -18.9  235  29 15   7.7   4.2
 25000 -25.6 -14.1  241  27 14   7.6   4.2 | -26.0 -14.8  233  29 15   7.7   4.2
 24000 -23.1  -9.6  243  27 14   8.5   4.6 | -23.7 -10.7  232  29 15   8.0   4.4
 23000 -20.6  -5.1  246  27 14   8.5   4.7 | -20.7  -5.3  231  27 14   8.0   4.4
 22000 -18.0  -0.4  248  26 13   8.5   4.7 | -18.3  -0.9  230  25 13   8.0   4.4
 21000 -15.5   4.1  246  25 13   8.5   4.6 | -15.9   3.4  230  24 13   7.9   4.3
 20000 -13.0   8.6  240  24 13   8.4   4.6 | -13.6   7.5  232  24 12   7.9   4.3
 19500 -11.7  10.9  237  24 12   8.4   4.6 | -12.4   9.7  233  24 12   7.9   4.3
 19000 -10.4  13.3  234  24 12   7.1   3.9 | -11.2  11.8  234  24 12   8.2   4.5
 18500  -9.6  14.7  231  23 12   5.6   3.1 | -10.0  14.0  235  24 12   8.3   4.6
 18000  -8.8  16.2  227  23 12   5.4   3.0 |  -8.7  16.3  237  23 12   8.4   4.6
 17500  -7.9  17.8  225  22 11   6.5   3.6 |  -7.6  18.3  239  22 11   7.0   3.8
 17000  -7.0  19.4  226  20 10   6.6   3.6 |  -6.6  20.1  240  21 11   7.2   3.9
 16500  -6.0  21.2  227  18  9   7.2   3.9 |  -5.5  22.1  241  19 10   7.4   4.0
 16000  -4.9  23.2  225  17  8   7.7   4.2 |  -4.5  23.9  239  16  8   7.6   4.2
 15500  -3.8  25.2  223  15  8   8.0   4.4 |  -3.4  25.9  235  13  7   8.3   4.5
 15000  -2.5  27.5  221  14  7   9.4   5.1 |  -2.1  28.2  232  11  6   9.4   5.2
 14500  -1.1  30.0  219  13  7   9.3   5.1 |  -0.7  30.7  229  10  5   9.4   5.2
 14000   0.2  32.4  219  13  6   9.0   4.9 |   0.7  33.3  226   9  5   9.6   5.3
 13500   1.5  34.7  222  12  6   9.0   5.0 |   2.1  35.8  226   9  5   9.6   5.3
 13000   2.9  37.2  226  12  6   8.5   4.6 |   3.5  38.3  224   9  5  10.0   5.5
 12500   4.1  39.4  234  12  6   8.4   4.6 |   5.0  41.0  222   9  4  10.0   5.5
 12000   5.4  41.7  241  13  7   8.8   4.8 |   6.5  43.7  220   8  4   9.9   5.4
 11750   6.0  42.8  244  13  7   9.0   4.9 |   7.2  45.0  220   8  4   9.9   5.4
 11500   6.7  44.1  246  13  7   9.0   4.9 |   8.0  46.4  219   8  4   9.9   5.4
 11250   7.4  45.3  249  13  7   9.0   4.9 |   8.7  47.7  219   8  4   9.9   5.4
 11000   8.1  46.6  251  13  7   9.2   5.0 |   9.4  48.9  218   8  4   9.9   5.4
 10750   8.7  47.7  252  13  7   9.3   5.1 |  10.2  50.4  217   8  4   9.9   5.5
 10500  10.1  50.2  253  13  7   9.3   5.1 |  10.9  51.6  216   8  4   9.9   5.5
 10250  10.8  51.4  254  13  7   9.3   5.1 |  11.7  53.1  215   8  4   9.9   5.5
 10000  11.5  52.7  253  12  6   9.3   5.1 |  12.4  54.3  214   8  4   9.9   5.4
  9750  12.2  54.0  253  12  6   9.4   5.1 |  13.1  55.6  213   7  4   9.9   5.4
  9500  12.9  55.2  252  12  6   9.2   5.1 |  14.6  58.3  210   7  4   9.9   5.4
  9250  13.5  56.3  252  12  6   8.2   4.5 |  15.4  59.7  209   7  4  10.0   5.5
  9000  14.1  57.4  253  12  6   7.8   4.3 |  16.1  61.0  208   7  4  10.2   5.6
  8750  14.6  58.3  253  12  6   7.5   4.1 |  16.8  62.2  207   7  4   9.4   5.2
  8500  15.1  59.2  254  12  6   9.4   5.1 |  17.6  63.7  206   7  3  12.2   6.7
  8250  16.0  60.8  253  11  6  13.8   7.6 |  18.7  65.7  204   6  3  19.2  10.5
  8000  17.0  62.6  252   9  5  15.5   8.5 |  20.3  68.5  201   6  3  22.3  12.2
  7750  18.1  64.6  250   7  4  14.3   7.9 |  21.8  71.2  197   5  3  19.5  10.7
  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

           05/17/2013 at 1500 MDT          |       05/17/2013 at 1800 MDT
                                           |
K index... +13.6                           | K index... +12.1
                                           |
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 -61.3 -78.3  253  26 13  -1.4  -0.7 | -59.9 -75.8  265  25 13  -0.5  -0.3
 45000 -62.9 -81.2  245  38 19   0.8   0.5 | -60.6 -77.1  261  35 18  -0.5  -0.3
 40000 -61.6 -78.9  235  42 22   0.4   0.2 | -61.4 -78.5  234  38 20  -1.0  -0.5
 38000 -57.7 -71.9  238  42 21   7.7   4.2 | -57.2 -71.0  232  39 20   7.6   4.1
 36000 -52.4 -62.3  242  41 21   7.7   4.2 | -52.7 -62.9  232  39 20   7.6   4.1
 34000 -47.6 -53.7  243  39 20   8.4   4.6 | -47.9 -54.2  233  39 20   8.2   4.5
 32000 -42.6 -44.7  242  37 19   8.4   4.6 | -43.0 -45.4  234  39 20   8.2   4.5
 30000 -37.6 -35.7  237  35 18   8.3   4.5 | -38.0 -36.4  235  37 19   8.7   4.8
 29000 -35.1 -31.2  233  35 18   8.3   4.6 | -35.3 -31.5  236  36 19   8.7   4.8
 28000 -32.6 -26.7  230  35 18   8.3   4.6 | -32.7 -26.9  236  35 18   8.7   4.8
 27000 -30.2 -22.4  227  35 18   7.7   4.2 | -30.2 -22.4  237  34 18   8.0   4.4
 26000 -27.9 -18.2  224  35 18   7.7   4.2 | -27.8 -18.0  238  33 17   8.0   4.4
 25000 -25.6 -14.1  222  35 18   7.7   4.2 | -25.4 -13.7  240  32 17   7.9   4.4
 24000 -23.4 -10.1  221  35 18   6.7   3.7 | -22.7  -8.9  241  31 16   6.7   3.7
 23000 -20.8  -5.4  225  32 17   6.8   3.7 | -20.7  -5.3  243  30 15   6.7   3.7
 22000 -18.8  -1.8  228  31 16   6.7   3.7 | -18.7  -1.7  245  29 15   6.6   3.6
 21000 -16.5   2.3  232  28 14   8.2   4.5 | -16.4   2.5  245  26 13   8.1   4.4
 20000 -14.1   6.6  237  24 12   8.3   4.5 | -14.0   6.8  244  23 12   8.2   4.5
 19500 -12.9   8.8  240  23 12   8.3   4.6 | -12.8   9.0  243  22 11   8.3   4.5
 19000 -11.6  11.1  243  21 11   8.9   4.9 | -11.6  11.1  242  20 11   8.9   4.9
 18500 -10.3  13.5  244  19 10   9.2   5.1 | -10.3  13.5  241  21 11   9.2   5.1
 18000  -8.9  16.0  245  17  9   9.3   5.1 |  -8.9  16.0  240  21 11   9.3   5.1
 17500  -7.6  18.3  246  16  8   9.1   5.0 |  -7.6  18.3  239  21 11   9.1   5.0
 17000  -6.2  20.8  245  15  8   9.1   5.0 |  -6.2  20.8  237  21 11   9.1   5.0
 16500  -4.9  23.2  245  14  7   9.5   5.2 |  -4.9  23.2  236  22 11   9.3   5.1
 16000  -3.4  25.9  243  13  7   9.6   5.3 |  -3.5  25.7  235  22 11   9.4   5.2
 15500  -2.0  28.4  241  13  6   9.5   5.2 |  -2.1  28.2  233  22 11   9.5   5.2
 15000  -0.6  30.9  236  12  6   9.3   5.1 |  -0.6  30.9  232  22 11   9.9   5.4
 14500   0.7  33.3  230  11  6   9.2   5.1 |   0.9  33.6  231  22 12   9.9   5.4
 14000   2.1  35.8  223  11  6   9.6   5.3 |   2.3  36.1  229  22 12   9.6   5.3
 13500   3.6  38.5  217  11  6   9.6   5.3 |   3.8  38.8  228  23 12   9.7   5.3
 13000   5.0  41.0  211  11  6   9.8   5.4 |   5.2  41.4  226  23 12   9.6   5.2
 12500   6.5  43.7  206  11  6   9.8   5.4 |   6.6  43.9  224  23 12   9.6   5.2
 12000   7.9  46.2  201  12  6   9.8   5.4 |   8.1  46.6  222  23 12   9.9   5.4
 11750   8.6  47.5  198  12  6   9.7   5.3 |   8.8  47.8  221  23 12  10.0   5.5
 11500   9.4  48.9  196  12  6   9.8   5.4 |   9.5  49.1  220  23 12  10.0   5.5
 11250  10.1  50.2  193  12  6   9.8   5.4 |  10.3  50.5  219  23 12  10.0   5.5
 11000  10.8  51.4  191  13  6   9.9   5.4 |  11.0  51.8  217  23 12   9.7   5.3
 10750  11.6  52.9  190  13  7  10.0   5.5 |  11.7  53.1  216  22 12   9.5   5.2
 10500  12.3  54.1  189  13  7  10.0   5.5 |  12.4  54.3  214  22 11   9.5   5.2
 10250  13.0  55.4  188  13  7  10.0   5.5 |  13.1  55.6  212  22 11   9.5   5.2
 10000  13.8  56.8  186  13  7  10.0   5.5 |  13.9  57.0  211  22 11   9.7   5.3
  9750  15.3  59.5  184  13  7  10.1   5.5 |  15.3  59.5  207  22 11   9.8   5.4
  9500  16.0  60.8  183  13  7  10.1   5.5 |  16.0  60.8  205  22 11   9.8   5.4
  9250  16.8  62.2  182  13  7  10.0   5.5 |  16.8  62.2  204  21 11   9.8   5.4
  9000  17.5  63.5  181  13  7  10.1   5.6 |  17.5  63.5  203  21 11   9.9   5.4
  8750  18.3  64.9  180  13  7   9.8   5.4 |  18.3  64.9  201  21 11   9.7   5.3
  8500  19.0  66.2  179  13  7  11.2   6.1 |  19.0  66.2  200  21 11  10.2   5.6
  8250  20.1  68.2  178  13  7  17.9   9.8 |  19.8  67.6  199  20 10  12.7   7.0
  8000  21.6  70.9  176  12  6  24.6  13.5 |  20.8  69.4  199  17  9  15.3   8.4
  7750  23.2  73.8  173  11  5  14.2   7.8 |  21.8  71.2  198  14  7  11.4   6.2
  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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