Soaring Guidance
Issued by NWS Pueblo, CO

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000
UXUS97 KPUB 211114
SRGPUB

SOARING FORECAST
NATIONAL WEATHER SERVICE PUEBLO CO
514 AM MDT TUE MAY 21 2013


EXPERIMENTAL PRODUCT

This forecast is for Tuesday May 21, 2013:

If the trigger temperature of 47.6 F/8.7 C is reached...then
   Thermal Soaring Index....................... Excellent
   Maximum rate of lift........................ 1039 ft/min (5.3 m/s)
   Maximum height of thermals.................. 19555 ft MSL (11893 ft AGL)

Forecast maximum temperature................... 64.0 F/18.2 C
Time of trigger temperature.................... 0800 MDT
Time of overdevelopment........................ 1400 MDT
Middle/high clouds during soaring window....... None
Surface winds during soaring window............ 20 mph or less
Height of the -3 thermal index................. 16803 ft MSL (9141 ft AGL)
Thermal soaring outlook for Wednesday 05/22.... Excellent

Wave Soaring Index............................. Poor
Wave Soaring Index trend (to 1800 MDT)......... Same
Height of stable layer (12-18K ft MSL)......... None
Weak PVA/NVA (through 1800 MDT)................ Weak PVA
Potential height of wave....................... 17501 ft MSL (9839 ft AGL)
Wave soaring outlook for Wednesday 05/22....... Poor

Remarks...

Sunrise/Sunset.................... 05:41:43 / 20:09:55 MDT
Total possible sunshine........... 14 hr 28 min 11 sec (868 min 11 sec)
Altitude of sun at 12:56:01 MDT... 71.33 degrees

Upper air data from numerical model forecast valid on 05/21/2013 at 0600 MDT

Freezing level.................. 10295 ft MSL (2633 ft AGL)
Convective condensation level... 15392 ft MSL (7730 ft AGL)
Lifted condensation level....... 17580 ft MSL (9918 ft AGL)
Lifted index.................... -1.6
K index......................... +8.4

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  -54.9 -66.8   257   10    5   3.3   1.8   94.7 202.4    45.6      M    M
 45000  -50.1 -58.2   286   17    9   1.4   0.8   80.2 176.3    39.4      M    M
 40000  -47.7 -53.9   293   17    9   1.5   0.8   60.3 140.5    28.7      M    M
 38000  -49.0 -56.2   295   15    7  -4.0  -2.2   49.7 121.5    22.2      M    M
 36000  -51.4 -60.5   296   10    5  -4.0  -2.2   38.0 100.4    14.4      M    M
 34000  -52.2 -62.0   295    8    4   6.4   3.5   29.1  84.3     8.3      M    M
 32000  -48.2 -54.8   280    9    5   6.6   3.6   26.4  79.5     6.5      M    M
 30000  -43.9 -47.0   274   11    6   8.7   4.8   24.5  76.1     5.2      M    M
 29000  -41.3 -42.3   277   12    6   8.7   4.8   24.0  75.2     4.9      M    M
 28000  -38.7 -37.7   280   14    7   8.7   4.8   23.7  74.6     4.6      M    M
 27000  -36.1 -33.0   283   16    8   8.2   4.5   23.4  74.1     4.5      M    M
 26000  -33.7 -28.7   290   17    9   7.8   4.3   22.6  72.6     3.9      M    M
 25000  -30.8 -23.4   298   19   10   7.8   4.3   21.7  71.1     3.2      M    M
 24000  -28.4 -19.1   304   21   11   8.1   4.4   21.1  70.0     2.7      M    M
 23000  -26.0 -14.8   310   22   11   8.1   4.4   20.4  68.8     2.2      M    M
 22000  -23.6 -10.5   316   24   12   8.1   4.5   19.9  67.8     1.8      M    M
 21000  -21.2  -6.2   320   26   13   6.9   3.8   19.2  66.6     1.2      M    M
 20000  -19.2  -2.6   324   28   14   7.0   3.8   18.2  64.8     0.3      M    M
 19500  -18.1  -0.6   326   29   15   7.0   3.8   17.8  64.0    -0.1   1031  5.2
 19000  -17.1   1.2   328   30   16   7.1   3.9   17.3  63.2    -0.5    985  5.0
 18500  -16.1   3.0   329   31   16   6.1   3.3   16.8  62.3    -0.9    941  4.8
 18000  -15.2   4.6   329   32   16   6.1   3.3   16.2  61.2    -1.5    900  4.6
 17500  -14.3   6.3   330   33   17   6.0   3.3   15.6  60.1    -2.1    859  4.4
 17000  -13.5   7.7   330   33   17   6.0   3.3   15.0  58.9    -2.7    818  4.2
 16500  -12.6   9.3   330   33   17   6.1   3.3   14.3  57.8    -3.4    777  3.9
 16000  -11.8  10.8   330   34   17   5.7   3.1   13.7  56.7    -4.0    737  3.7
 15500  -11.0  12.2   330   34   18   5.8   3.2   13.0  55.5    -4.7    698  3.5
 15000  -10.1  13.8   331   35   18   5.8   3.2   12.4  54.3    -5.3    658  3.3
 14500   -9.3  15.3   331   35   18   5.8   3.2   11.8  53.2    -6.0    618  3.1
 14000   -8.4  16.9   331   35   18   6.3   3.4   11.1  52.1    -6.6    577  2.9
 13500   -7.4  18.7   331   36   18   6.6   3.6   10.6  51.1    -7.1    533  2.7
 13000   -6.5  20.3   331   36   19   7.0   3.8   10.1  50.2    -7.6    489  2.5
 12500   -5.3  22.5   331   36   18   7.5   4.1    9.8  49.6    -8.0    441  2.2
 12000   -4.2  24.4   331   36   18   7.6   4.2    9.4  49.0    -8.4    392  2.0
 11750   -3.7  25.3   331   36   18   7.6   4.2    9.3  48.7    -8.6    368  1.9
 11500   -3.1  26.4   331   35   18   7.6   4.2    9.1  48.4    -8.8    343  1.7
 11250   -2.5  27.5   331   35   18   7.6   4.2    8.9  48.1    -9.0    319  1.6
 11000   -2.0  28.4   331   35   18   7.8   4.3    8.8  47.8    -9.1    295  1.5
 10750   -1.4  29.5   331   34   17   8.0   4.4    8.6  47.5    -9.3    270  1.4
 10500   -0.8  30.6   331   32   17   8.0   4.4    8.5  47.3    -9.5    245  1.2
 10250   -0.2  31.6   331   31   16   8.0   4.4    8.4  47.0    -9.6    219  1.1
 10000    0.4  32.7   331   30   15   8.2   4.5    8.2  46.8    -9.8    194  1.0
  9750    1.6  34.9   331   27   14   8.4   4.6    8.0  46.4   -10.1    143  0.7
  9500    2.3  36.1   331   25   13   8.4   4.6    7.9  46.2   -10.2    117  0.6
  9250    2.9  37.2   330   24   12   8.0   4.4    7.8  46.0   -10.4     91  0.5
  9000    3.4  38.1   328   22   11   7.1   3.9    7.6  45.7   -10.6     68  0.3
  8750    3.9  39.0   325   20   10   8.8   4.8    7.5  45.4   -10.8     44  0.2
  8500    4.5  40.1   322   18    9   3.1   1.7    7.3  45.1   -11.0     20  0.1
  8250    4.1  39.4   317   15    8 -11.9  -6.5    6.2  43.2   -12.1     24  0.1
  8000    2.8  37.0   306   11    5 -19.7 -10.8    4.2  39.6   -14.2     56  0.3
  7750    1.5  34.7   283    7    4 -10.9  -6.0    2.2  36.0   -16.3     87  0.4
  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 * * * * * *

           05/21/2013 at 0900 MDT          |       05/21/2013 at 1200 MDT
                                           |
K index... +9.9                            | K index... +18.7
                                           |
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 -55.2 -67.4  255  12  6   4.1   2.2 | -55.7 -68.3  257  11  6   3.6   2.0
 45000 -49.4 -56.9  273  12  6   1.1   0.6 | -50.5 -58.9  262  14  7   1.3   0.7
 40000 -47.6 -53.7  295  16  8   1.2   0.6 | -48.4 -55.1  298  16  8   1.3   0.7
 38000 -48.8 -55.8  298  16  8  -3.8  -2.1 | -48.8 -55.8  304  18  9  -1.6  -0.9
 36000 -51.1 -60.0  299  13  7  -3.8  -2.1 | -49.8 -57.6  308  19 10  -1.6  -0.9
 34000 -51.8 -61.2  297  12  6   6.4   3.5 | -49.7 -57.5  308  19 10   5.1   2.8
 32000 -47.8 -54.0  279  12  6   6.7   3.7 | -46.5 -51.7  299  16  8   5.3   2.9
 30000 -43.6 -46.5  271  14  7   8.0   4.4 | -43.1 -45.6  292  16  8   6.9   3.8
 29000 -41.2 -42.2  276  16  8   8.1   4.4 | -41.0 -41.8  294  18  9   6.9   3.8
 28000 -38.7 -37.7  280  19 10   8.1   4.4 | -38.9 -38.0  295  21 11   6.9   3.8
 27000 -36.3 -33.3  283  21 11   7.9   4.3 | -36.9 -34.4  296  24 12   7.4   4.1
 26000 -34.0 -29.2  289  24 12   7.7   4.2 | -34.5 -30.1  297  26 13   7.9   4.3
 25000 -31.1 -24.0  294  28 14   7.7   4.2 | -31.6 -24.9  298  28 15   7.9   4.3
 24000 -28.8 -19.8  297  30 16   8.0   4.4 | -29.2 -20.6  298  30 16   8.2   4.5
 23000 -26.4 -15.5  295  30 15   8.0   4.4 | -26.7 -16.1  298  31 16   8.2   4.5
 22000 -24.0 -11.2  293  29 15   8.0   4.4 | -24.3 -11.7  298  33 17   8.2   4.5
 21000 -21.6  -6.9  294  29 15   8.1   4.4 | -21.9  -7.4  299  33 17   7.6   4.2
 20000 -19.2  -2.6  301  29 15   8.1   4.5 | -19.6  -3.3  303  34 17   7.7   4.2
 19500 -18.0  -0.4  304  29 15   8.2   4.5 | -18.4  -1.1  305  34 17   7.7   4.2
 19000 -16.8   1.8  307  30 15   8.3   4.6 | -17.3   0.9  307  34 18   7.9   4.4
 18500 -15.7   3.7  311  30 16   6.4   3.5 | -16.3   2.7  308  34 18   5.5   3.0
 18000 -14.8   5.4  314  31 16   6.3   3.5 | -15.5   4.1  310  34 18   5.6   3.1
 17500 -13.8   7.2  318  32 17   5.8   3.2 | -14.7   5.5  312  35 18   5.9   3.2
 17000 -13.1   8.4  320  33 17   4.9   2.7 | -13.8   7.2  312  34 18   6.2   3.4
 16500 -12.4   9.7  322  34 18   5.0   2.7 | -12.9   8.8  312  34 17   6.2   3.4
 16000 -11.7  10.9  323  35 18   4.7   2.6 | -11.9  10.6  311  32 17   7.6   4.2
 15500 -11.0  12.2  324  36 19   4.7   2.6 | -10.8  12.6  309  31 16   7.4   4.1
 15000 -10.4  13.3  325  37 19   4.8   2.7 |  -9.7  14.5  306  30 15   8.4   4.6
 14500  -9.7  14.5  325  37 19   4.9   2.7 |  -8.4  16.9  303  28 14   8.5   4.6
 14000  -8.9  16.0  326  37 19   5.9   3.3 |  -7.2  19.0  299  26 13   8.4   4.6
 13500  -7.9  17.8  326  36 19   6.6   3.6 |  -6.0  21.2  295  23 12   8.4   4.6
 13000  -7.0  19.4  325  36 18   7.1   3.9 |  -4.7  23.5  290  21 11   8.5   4.7
 12500  -5.9  21.4  325  34 17   7.6   4.1 |  -3.5  25.7  289  18  9   8.6   4.7
 12000  -4.7  23.5  324  32 16   7.8   4.3 |  -2.2  28.0  287  15  7   9.0   4.9
 11750  -4.1  24.6  323  30 16   8.1   4.4 |  -1.5  29.3  288  13  7   9.7   5.3
 11500  -3.5  25.7  323  29 15   8.1   4.4 |  -0.8  30.6  291  12  6   9.6   5.3
 11250  -3.0  26.6  323  27 14   7.9   4.4 |  -0.1  31.8  294  11  6   9.6   5.3
 11000  -2.4  27.7  322  26 13   8.5   4.6 |   0.6  33.1  297  10  5   9.8   5.4
 10750  -1.7  28.9  323  24 12   9.1   5.0 |   1.4  34.5  300   9  5  10.1   5.6
 10500  -1.0  30.2  324  22 11   9.1   5.0 |   2.1  35.8  303   9  4  10.1   5.6
 10250  -0.4  31.3  325  20 10   9.0   4.9 |   2.9  37.2  306   8  4  10.1   5.6
 10000   1.0  33.8  327  17  9  10.1   5.5 |   3.7  38.7  309   8  4  10.1   5.5
  9750   1.8  35.2  328  16  8  10.0   5.5 |   5.1  41.2  313   8  4  10.0   5.5
  9500   2.5  36.5  330  14  7  10.0   5.5 |   5.9  42.6  316   8  4  10.0   5.5
  9250   3.2  37.8  332  14  7  10.0   5.5 |   6.6  43.9  318   8  4  10.0   5.5
  9000   4.0  39.2  333  13  7  10.1   5.6 |   7.4  45.3  321   7  4  10.2   5.6
  8750   4.7  40.5  333  13  7   9.6   5.2 |   8.1  46.6  323   7  4   9.7   5.3
  8500   5.5  41.9  334  13  7  11.6   6.4 |   8.9  48.0  326   7  4  11.7   6.4
  8250   6.5  43.7  335  12  6  16.5   9.1 |  10.0  50.0  329   7  3  19.5  10.7
  8000   7.8  46.0  335  11  5  18.4  10.1 |  11.8  53.2  333   6  3  26.5  14.5
  7750   9.1  48.4  336   9  5  17.1   9.4 |  13.5  56.3  338   5  3  16.0   8.8
  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

           05/21/2013 at 1500 MDT          |       05/21/2013 at 1800 MDT
                                           |
K index... +20.0                           | K index... +21.2
                                           |
Height Temperature  Wnd WndSpd  Lapse Rate | Temperature  Wnd WndSpd  Lapse Rate
ft MSL deg C deg F  Dir kt m/s  C/km F/kft | deg C deg F  Dir kt m/s  C/km F/kft
--------------------------------------------------------------------------------
 50000 -56.0 -68.8  263  14  7   3.1   1.7 | -56.6 -69.9  259  14  7   3.1   1.7
 45000 -51.6 -60.9  271  21 11   1.2   0.7 | -52.3 -62.1  276  18 10  -0.1  -0.0
 40000 -49.7 -57.5  307  19 10   1.2   0.6 | -52.4 -62.3  318  36 18  -0.0  -0.0
 38000 -49.8 -57.6  317  24 12  -0.8  -0.5 | -52.0 -61.6  322  44 23   1.0   0.5
 36000 -50.3 -58.5  322  30 16  -0.8  -0.5 | -51.4 -60.5  324  53 27   1.0   0.5
 34000 -49.5 -57.1  324  33 17   6.5   3.6 | -49.5 -57.1  325  56 29   7.3   4.0
 32000 -45.5 -49.9  325  28 14   6.6   3.6 | -45.1 -49.2  325  49 25   7.3   4.0
 30000 -41.6 -42.9  324  24 12   6.3   3.5 | -40.7 -41.3  325  42 22   7.7   4.2
 29000 -39.7 -39.5  320  24 12   6.3   3.5 | -38.4 -37.1  325  40 21   7.7   4.2
 28000 -37.8 -36.0  317  24 13   6.3   3.5 | -36.1 -33.0  326  38 19   7.7   4.2
 27000 -35.9 -32.6  314  25 13   6.8   3.8 | -33.8 -28.8  326  36 18   6.9   3.8
 26000 -33.2 -27.8  313  26 13   7.2   3.9 | -31.8 -25.2  325  35 18   6.7   3.7
 25000 -31.1 -24.0  312  27 14   7.2   4.0 | -29.3 -20.7  323  34 17   6.7   3.7
 24000 -28.9 -20.0  312  28 14   7.5   4.1 | -27.3 -17.1  322  33 17   6.5   3.6
 23000 -26.7 -16.1  313  30 16   7.5   4.1 | -25.3 -13.5  322  32 17   6.5   3.6
 22000 -24.4 -11.9  313  32 17   7.5   4.1 | -23.4 -10.1  322  32 16   6.6   3.6
 21000 -22.2  -8.0  314  34 17   7.6   4.2 | -21.4  -6.5  320  31 16   7.1   3.9
 20000 -19.9  -3.8  314  33 17   7.6   4.2 | -19.3  -2.7  315  30 16   7.1   3.9
 19500 -18.8  -1.8  314  33 17   7.6   4.2 | -18.2  -0.8  313  30 15   7.1   3.9
 19000 -17.7   0.1  314  33 17   7.7   4.2 | -17.2   1.0  311  30 15   7.2   3.9
 18500 -16.6   2.1  313  32 16   7.4   4.0 | -16.1   3.0  307  29 15   7.6   4.2
 18000 -15.5   4.1  311  31 16   7.4   4.1 | -15.0   5.0  303  28 14   7.7   4.2
 17500 -14.4   6.1  308  30 15   7.4   4.1 | -13.9   7.0  298  26 14   8.2   4.5
 17000 -13.3   8.1  304  28 14   7.5   4.1 | -12.7   9.1  294  25 13   8.6   4.7
 16500 -12.2  10.0  299  26 14   7.5   4.1 | -11.5  11.3  289  23 12   8.7   4.8
 16000 -11.1  12.0  295  24 12   7.9   4.4 | -10.2  13.6  286  21 11   8.9   4.9
 15500 -10.0  14.0  290  21 11   7.9   4.3 |  -8.9  16.0  285  19 10   8.9   4.9
 15000  -8.7  16.3  285  18  9   9.1   5.0 |  -7.6  18.3  284  16  8   8.8   4.8
 14500  -7.4  18.7  284  15  8   9.1   5.0 |  -6.3  20.7  285  14  7   8.7   4.8
 14000  -6.1  21.0  283  12  6   9.6   5.3 |  -5.0  23.0  287  11  6   9.6   5.3
 13500  -4.6  23.7  285  11  6   9.8   5.4 |  -3.5  25.7  287  10  5   9.8   5.4
 13000  -3.1  26.4  286  10  5   9.9   5.4 |  -2.1  28.2  288   9  5   9.4   5.2
 12500  -1.7  28.9  288  10  5   9.9   5.4 |  -0.7  30.7  292   7  3   9.1   5.0
 12000  -0.2  31.6  290  10  5   9.8   5.4 |   0.6  33.1  299   5  2   9.3   5.1
 11750   0.5  32.9  291   9  5   9.7   5.3 |   1.3  34.3  305   4  2   9.6   5.3
 11500   1.3  34.3  292   9  5   9.7   5.3 |   2.1  35.8  312   4  2   9.5   5.2
 11250   2.0  35.6  293   9  5   9.7   5.3 |   2.8  37.0  322   3  2   9.5   5.2
 11000   2.7  36.9  294   9  4   9.8   5.4 |   3.5  38.3  334   3  2   9.6   5.3
 10750   3.4  38.1  295   8  4  10.0   5.5 |   4.2  39.6  340   3  2   9.7   5.3
 10500   4.2  39.6  296   8  4   9.9   5.5 |   4.9  40.8  345   3  2   9.7   5.3
 10250   4.9  40.8  298   8  4  10.0   5.5 |   5.6  42.1  350   3  2   9.7   5.3
 10000   6.4  43.5  300   8  4   9.7   5.3 |   6.4  43.5  355   3  2   9.7   5.3
  9750   7.1  44.8  302   7  4   9.7   5.3 |   7.8  46.0  004   3  2   9.8   5.4
  9500   7.9  46.2  303   7  4   9.7   5.3 |   8.6  47.5  007   3  2   9.8   5.4
  9250   8.6  47.5  304   7  4   9.8   5.4 |   9.3  48.7  011   3  2   9.7   5.3
  9000   9.3  48.7  306   7  3  10.0   5.5 |  10.0  50.0  014   3  2   9.5   5.2
  8750  10.1  50.2  307   6  3   9.8   5.4 |  10.7  51.3  016   4  2   9.5   5.2
  8500  10.8  51.4  309   6  3  10.4   5.7 |  11.4  52.5  019   4  2   9.8   5.4
  8250  11.7  53.1  312   6  3  13.8   7.6 |  12.2  54.0  023   4  2  11.9   6.5
  8000  12.8  55.0  321   5  2  17.6   9.7 |  13.2  55.8  031   3  2  14.5   7.9
  7750  14.0  57.2  333   4  2  11.4   6.2 |  14.2  57.6  040   3  2  10.3   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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