Soaring Guidance
Issued by NWS Pueblo, CO

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000
UXUS97 KPUB 191014
SRGPUB

SOARING FORECAST
NATIONAL WEATHER SERVICE PUEBLO CO
414 AM MDT WED JUN 19 2013


EXPERIMENTAL PRODUCT

This forecast is for Wednesday June 19, 2013:

If the trigger temperature of 73.5 F/23.1 C is reached...then
   Thermal Soaring Index....................... Good
   Maximum rate of lift........................ 2172 ft/min (11.0 m/s)
   Maximum height of thermals.................. 28710 ft MSL (21051 ft AGL)

Forecast maximum temperature................... 88.0 F/31.6 C
Time of trigger temperature.................... 1000 MDT
Time of overdevelopment........................ None
Middle/high clouds during soaring window....... None
Surface winds during soaring window............ Between 20 mph and 30 mph
Height of the -3 thermal index................. 23284 ft MSL (15625 ft AGL)
Thermal soaring outlook for Thursday 06/20..... Excellent

Wave Soaring Index............................. Poor
Wave Soaring Index trend (to 1800 MDT)......... Neutral
Height of stable layer (12-18K ft MSL)......... None
Weak PVA/NVA (through 1800 MDT)................ Neither
Potential height of wave....................... 27871 ft MSL (20212 ft AGL)
Wave soaring outlook for Thursday 06/20........ Poor

Remarks...

Sunrise/Sunset.................... 05:33:46 / 20:27:34 MDT
Total possible sunshine........... 14 hr 53 min 49 sec (893 min 49 sec)
Altitude of sun at 13:00:47 MDT... 74.42 degrees

Upper air data from numerical model forecast valid on 06/19/2013 at 0600 MDT

Freezing level.................. 15541 ft MSL (7882 ft AGL)
Convective condensation level... 19387 ft MSL (11728 ft AGL)
Lifted condensation level....... 21695 ft MSL (14036 ft AGL)
Lifted index.................... -5.7
K index......................... +5.2

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  -61.6 -78.9   244   31   16   1.9   1.0   81.5 178.7    30.1      M    M
 45000  -58.5 -73.3   248   47   24   2.2   1.2   62.8 145.0    20.3      M    M
 40000  -55.1 -67.2   261   49   25   4.4   2.4   46.3 115.3    10.4      M    M
 38000  -52.1 -61.8   260   46   24   5.0   2.7   41.7 107.0     7.4      M    M
 36000  -49.1 -56.4   260   42   22   5.0   2.7   37.9 100.2     4.9      M    M
 34000  -45.0 -49.0   260   39   20   7.9   4.3   35.5  95.8     3.2      M    M
 32000  -40.2 -40.4   261   37   19   7.9   4.3   34.1  93.3     2.2      M    M
 30000  -35.7 -32.3   263   38   19   7.4   4.1   32.3  90.2     1.0      M    M
 29000  -33.5 -28.3   263   39   20   7.4   4.1   31.4  88.6     0.3      M    M
 28000  -31.2 -24.2   264   40   20   7.3   4.0   30.7  87.2    -0.4   2114 10.7
 27000  -28.2 -18.8   263   41   21   8.2   4.5   29.8  85.6    -1.1   1987 10.1
 26000  -25.8 -14.4   262   42   22   8.2   4.5   29.2  84.6    -1.6   1883  9.6
 25000  -23.3  -9.9   262   43   22   8.3   4.5   28.7  83.7    -2.0   1780  9.0
 24000  -20.9  -5.6   261   41   21   7.9   4.3   28.1  82.5    -2.6   1678  8.5
 23000  -18.5  -1.3   261   38   20   7.9   4.3   27.4  81.3    -3.2   1578  8.0
 22000  -16.2   2.8   261   35   18   7.9   4.3   26.8  80.2    -3.8   1478  7.5
 21000  -13.7   7.3   261   34   17   8.5   4.7   26.3  79.3    -4.3   1373  7.0
 20000  -11.1  12.0   260   32   17   8.5   4.7   25.9  78.5    -4.7   1267  6.4
 19500   -9.9  14.2   260   32   16   8.6   4.7   25.7  78.2    -4.9   1214  6.2
 19000   -8.6  16.5   259   31   16   7.8   4.3   25.5  77.9    -5.1   1162  5.9
 18500   -7.5  18.5   258   30   15   7.7   4.2   25.1  77.2    -5.5   1114  5.7
 18000   -6.4  20.5   257   29   15   7.8   4.3   24.8  76.6    -5.9   1065  5.4
 17500   -5.2  22.6   257   28   14   8.4   4.6   24.5  76.1    -6.2   1015  5.2
 17000   -4.0  24.8   258   27   14   8.4   4.6   24.3  75.7    -6.4    963  4.9
 16500   -2.7  27.1   260   26   13   8.8   4.8   24.1  75.4    -6.7    910  4.6
 16000   -1.4  29.5   263   25   13   8.9   4.9   23.9  75.1    -6.8    855  4.3
 15500   -0.0  32.0   266   25   13   9.0   4.9   23.8  74.9    -7.0    800  4.1
 15000    1.3  34.3   268   24   13   9.0   5.0   23.7  74.6    -7.1    745  3.8
 14500    2.7  36.9   271   24   12   9.1   5.0   23.6  74.4    -7.3    689  3.5
 14000    4.1  39.4   272   24   12   9.7   5.3   23.5  74.3    -7.4    632  3.2
 13500    5.5  41.9   272   23   12   9.6   5.3   23.5  74.3    -7.4    574  2.9
 13000    7.0  44.6   271   23   12   9.5   5.2   23.5  74.2    -7.5    516  2.6
 12500    8.4  47.1   270   22   11   9.5   5.2   23.4  74.2    -7.6    459  2.3
 12000    9.8  49.6   268   21   11   9.7   5.3   23.4  74.1    -7.7    401  2.0
 11750   10.6  51.1   267   21   11   9.7   5.3   23.4  74.1    -7.7    372  1.9
 11500   11.3  52.3   266   20   11   9.8   5.4   23.4  74.1    -7.7    343  1.7
 11250   12.0  53.6   265   20   10   9.6   5.3   23.4  74.1    -7.8    314  1.6
 11000   12.7  54.9   263   19   10   8.6   4.7   23.4  74.0    -7.8    287  1.5
 10750   13.2  55.8   260   18    9   8.2   4.5   23.2  73.8    -8.0    262  1.3
 10500   13.8  56.8   256   17    9   8.4   4.6   23.1  73.6    -8.2    237  1.2
 10250   14.4  57.9   253   16    8   8.2   4.5   23.0  73.4    -8.3    212  1.1
 10000   15.2  59.4   243   15    8   4.8   2.6   22.5  72.5    -9.1    173  0.9
  9750   15.5  59.9   236   14    7   5.5   3.0   22.1  71.8    -9.5    156  0.8
  9500   15.8  60.4   230   13    7   4.8   2.6   21.8  71.2   -10.0    139  0.7
  9250   16.0  60.8   224   13    7   1.1   0.6   21.3  70.3   -10.6    128  0.6
  9000   15.8  60.4   222   13    7  -1.5  -0.8   20.5  68.9   -11.5    125  0.6
  8750   15.7  60.3   220   14    7   1.3   0.7   19.7  67.5   -12.4    122  0.6
  8500   15.5  59.9   218   14    7  -6.2  -3.4   19.0  66.1   -13.3    119  0.6
  8250   14.3  57.7   219   12    6 -24.9 -13.7   17.0  62.7   -15.3    150  0.8
  8000   12.0  53.6   223    9    5 -33.4 -18.3   14.0  57.2   -18.4    212  1.1
  7750    9.6  49.3   233    6    3 -25.0 -13.7   11.0  51.8   -21.5    274  1.4
  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 * * * * * *

           06/19/2013 at 0900 MDT          |       06/19/2013 at 1200 MDT
                                           |
K index... -1.6                            | K index... +2.1
                                           |
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 -60.8 -77.4  232  32 16   1.9   1.1 | -60.9 -77.6  222  34 17   2.0   1.1
 45000 -58.4 -73.1  245  44 23   0.1   0.1 | -58.6 -73.5  242  45 23  -0.4  -0.2
 40000 -57.9 -72.2  265  38 20   5.5   3.0 | -58.9 -74.0  259  36 19   6.3   3.4
 38000 -53.9 -65.0  268  35 18   6.6   3.6 | -54.4 -65.9  257  33 17   7.4   4.1
 36000 -49.9 -57.8  272  33 17   6.6   3.6 | -50.0 -58.0  255  31 16   7.4   4.1
 34000 -45.2 -49.4  272  31 16   8.4   4.6 | -45.1 -49.2  254  29 15   8.4   4.6
 32000 -40.2 -40.4  270  30 16   8.4   4.6 | -40.0 -40.0  254  27 14   8.4   4.6
 30000 -35.2 -31.4  268  30 15   8.4   4.6 | -34.9 -30.8  254  28 15   8.4   4.6
 29000 -32.7 -26.9  266  30 15   8.4   4.6 | -32.4 -26.3  255  30 15   8.4   4.6
 28000 -29.5 -21.1  265  29 15   8.1   4.4 | -29.3 -20.7  255  31 16   8.1   4.4
 27000 -27.2 -17.0  264  31 16   7.6   4.2 | -27.0 -16.6  256  33 17   7.7   4.2
 26000 -24.9 -12.8  264  32 17   7.6   4.2 | -24.7 -12.5  256  34 18   7.7   4.2
 25000 -22.7  -8.9  263  33 17   7.6   4.1 | -22.3  -8.1  257  36 18   7.7   4.2
 24000 -20.3  -4.5  262  33 17   8.0   4.4 | -19.9  -3.8  257  36 18   8.3   4.6
 23000 -17.9  -0.2  261  33 17   8.0   4.4 | -17.4   0.7  256  35 18   8.3   4.5
 22000 -15.5   4.1  260  33 17   8.1   4.4 | -14.9   5.2  255  35 18   8.3   4.5
 21000 -12.9   8.8  257  32 17   8.7   4.8 | -12.6   9.3  255  34 18   7.7   4.2
 20000 -10.3  13.5  254  32 17   8.7   4.8 | -10.3  13.5  255  33 17   7.7   4.2
 19500  -9.0  15.8  253  32 17   8.8   4.8 |  -9.2  15.4  255  33 17   7.7   4.2
 19000  -7.7  18.1  251  32 17   7.7   4.2 |  -8.0  17.6  256  33 17   7.7   4.2
 18500  -6.6  20.1  249  33 17   7.5   4.1 |  -6.9  19.6  256  32 17   7.7   4.2
 18000  -5.5  22.1  247  34 17   7.4   4.0 |  -5.7  21.7  256  32 17   7.8   4.3
 17500  -4.5  23.9  245  33 17   6.6   3.6 |  -4.5  23.9  256  31 16   8.3   4.6
 17000  -3.6  25.5  242  32 16   6.6   3.6 |  -3.3  26.1  255  29 15   8.3   4.6
 16500  -2.5  27.5  239  30 15   8.7   4.8 |  -2.1  28.2  253  27 14   8.3   4.6
 16000  -1.2  29.8  238  27 14   9.0   4.9 |  -0.9  30.4  250  24 13   8.4   4.6
 15500   0.1  32.2  236  25 13   8.9   4.9 |   0.3  32.5  246  22 11   8.7   4.8
 15000   1.4  34.5  235  23 12   8.7   4.8 |   1.6  34.9  244  21 11   9.0   4.9
 14500   2.7  36.9  233  21 11   8.7   4.8 |   3.0  37.4  242  20 10   9.0   5.0
 14000   4.1  39.4  235  19 10   8.8   4.8 |   4.3  39.7  239  18  9   9.1   5.0
 13500   5.4  41.7  239  18  9   8.8   4.8 |   5.6  42.1  235  17  9   9.1   5.0
 13000   6.7  44.1  243  17  9   8.8   4.8 |   7.0  44.6  231  16  8   9.3   5.1
 12500   8.0  46.4  246  16  8   8.7   4.8 |   8.4  47.1  226  15  8   9.3   5.1
 12000   9.4  48.9  248  16  8   9.9   5.4 |   9.8  49.6  221  14  7   9.6   5.2
 11750  10.2  50.4  248  16  8  10.0   5.5 |  10.5  50.9  218  14  7   9.6   5.3
 11500  10.9  51.6  247  16  8  10.0   5.5 |  11.2  52.2  215  14  7   9.6   5.3
 11250  11.6  52.9  247  16  8   9.8   5.4 |  11.9  53.4  212  14  7   9.7   5.3
 11000  12.4  54.3  246  15  8   9.3   5.1 |  12.6  54.7  210  14  7   9.9   5.4
 10750  13.0  55.4  245  15  8   9.1   5.0 |  13.4  56.1  208  14  7  10.0   5.5
 10500  13.7  56.7  244  15  8   9.2   5.1 |  14.1  57.4  205  14  7   9.9   5.5
 10250  15.1  59.2  242  14  7   8.4   4.6 |  15.6  60.1  201  14  7   9.9   5.4
 10000  15.6  60.1  240  13  7   8.0   4.4 |  16.3  61.3  199  14  7   9.8   5.4
  9750  16.2  61.2  237  12  6   8.3   4.6 |  17.0  62.6  197  14  7   9.8   5.4
  9500  16.8  62.2  235  11  6   7.6   4.2 |  17.8  64.0  194  14  7   9.9   5.4
  9250  17.2  63.0  232  11  6   5.3   2.9 |  18.5  65.3  193  14  7  10.0   5.5
  9000  17.5  63.5  231  11  6   4.5   2.5 |  19.2  66.6  191  14  7  10.3   5.6
  8750  17.7  63.9  230  12  6   4.4   2.4 |  20.0  68.0  190  14  7   9.5   5.2
  8500  18.0  64.4  228  12  6   6.9   3.8 |  20.7  69.3  188  14  7  12.4   6.8
  8250  18.6  65.5  226  11  6  12.1   6.6 |  21.9  71.4  187  13  7  19.7  10.8
  8000  19.4  66.9  220   8  4  13.4   7.3 |  23.5  74.3  185  12  6  23.1  12.7
  7750  20.2  68.4  209   6  3  14.2   7.8 |  25.1  77.2  183  11  6  19.9  10.9
  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

           06/19/2013 at 1500 MDT          |       06/19/2013 at 1800 MDT
                                           |
K index... +14.3                           | K index... +10.5
                                           |
Height Temperature  Wnd WndSpd  Lapse Rate | Temperature  Wnd WndSpd  Lapse Rate
ft MSL deg C deg F  Dir kt m/s  C/km F/kft | deg C deg F  Dir kt m/s  C/km F/kft
--------------------------------------------------------------------------------
 50000 -61.1 -78.0  236  37 19   1.6   0.9 | -61.9 -79.4  246  36 19   0.4   0.2
 45000 -59.3 -74.7  247  47 24  -0.4  -0.2 | -61.0 -77.8  257  47 24   1.2   0.7
 40000 -59.4 -74.9  257  41 21   7.7   4.2 | -58.8 -73.8  261  47 24   8.0   4.4
 38000 -54.5 -66.1  258  39 20   8.1   4.5 | -54.1 -65.4  260  43 22   7.9   4.3
 36000 -49.6 -57.3  258  37 19   8.1   4.5 | -49.3 -56.7  258  38 20   7.9   4.3
 34000 -44.7 -48.5  258  35 18   8.4   4.6 | -44.6 -48.3  256  37 19   7.9   4.4
 32000 -39.6 -39.3  258  31 16   8.4   4.6 | -39.8 -39.6  253  36 19   8.0   4.4
 30000 -34.8 -30.6  260  32 16   8.0   4.4 | -34.7 -30.5  254  35 18   8.8   4.8
 29000 -32.3 -26.1  261  33 17   8.0   4.4 | -32.0 -25.6  255  34 17   8.8   4.8
 28000 -29.3 -20.7  262  34 17   7.8   4.3 | -29.4 -20.9  256  33 17   9.0   4.9
 27000 -27.1 -16.8  261  35 18   7.5   4.1 | -26.4 -15.5  258  34 17   7.7   4.2
 26000 -24.8 -12.6  260  37 19   7.5   4.1 | -24.1 -11.4  260  34 18   7.7   4.2
 25000 -22.6  -8.7  260  39 20   7.5   4.1 | -21.8  -7.2  262  35 18   7.7   4.2
 24000 -20.1  -4.2  259  39 20   8.4   4.6 | -19.7  -3.5  262  33 17   7.1   3.9
 23000 -17.6   0.3  258  39 20   8.4   4.6 | -17.6   0.3  262  31 16   7.1   3.9
 22000 -15.1   4.8  258  39 20   8.3   4.6 | -15.5   4.1  261  29 15   7.4   4.1
 21000 -12.7   9.1  258  36 18   8.1   4.4 | -12.9   8.8  257  27 14   8.9   4.9
 20000 -10.3  13.5  257  32 17   8.2   4.5 | -10.3  13.5  251  24 13   9.0   4.9
 19500  -9.1  15.6  257  30 16   8.2   4.5 |  -9.0  15.8  248  23 12   9.0   4.9
 19000  -7.9  17.8  256  29 15   8.6   4.7 |  -7.6  18.3  246  23 12   9.6   5.3
 18500  -6.7  19.9  253  27 14   8.6   4.7 |  -6.2  20.8  245  23 12   9.7   5.3
 18000  -5.4  22.3  250  25 13   8.8   4.9 |  -4.7  23.5  244  23 12   9.7   5.3
 17500  -4.1  24.6  248  24 12   9.3   5.1 |  -3.3  26.1  243  23 12   9.8   5.4
 17000  -2.7  27.1  246  23 12   9.3   5.1 |  -1.8  28.8  241  23 12   9.8   5.4
 16500  -1.3  29.7  243  23 12   9.5   5.2 |  -0.4  31.3  238  23 12   9.5   5.2
 16000   0.1  32.2  240  22 12   9.6   5.2 |   1.1  34.0  235  23 12   9.5   5.2
 15500   1.5  34.7  237  22 11   9.5   5.2 |   2.5  36.5  233  24 12   9.6   5.3
 15000   2.9  37.2  235  22 11   9.5   5.2 |   4.0  39.2  231  24 12   9.7   5.3
 14500   4.4  39.9  233  22 11   9.5   5.2 |   5.4  41.7  230  24 12   9.7   5.3
 14000   5.8  42.4  231  22 11   9.9   5.4 |   6.9  44.4  228  24 12   9.5   5.2
 13500   7.3  45.1  228  22 11   9.9   5.4 |   8.3  46.9  226  24 12   9.5   5.2
 13000   8.7  47.7  225  21 11   9.8   5.4 |   9.7  49.5  224  24 12   9.8   5.4
 12500  10.2  50.4  222  21 11   9.8   5.4 |  11.2  52.2  221  24 12   9.8   5.4
 12000  11.7  53.1  218  21 11   9.7   5.3 |  12.6  54.7  219  24 12   9.8   5.4
 11750  12.4  54.3  216  21 11   9.7   5.3 |  13.4  56.1  218  24 12   9.8   5.4
 11500  13.1  55.6  213  20 11   9.7   5.3 |  14.1  57.4  217  24 12   9.8   5.4
 11250  13.8  56.8  210  20 10   9.7   5.3 |  14.8  58.6  216  23 12   9.8   5.4
 11000  14.6  58.3  208  20 10   9.8   5.4 |  15.5  59.9  214  23 12   9.7   5.3
 10750  15.3  59.5  207  20 10   9.9   5.4 |  16.3  61.3  212  23 12   9.6   5.3
 10500  16.0  60.8  206  20 10   9.8   5.4 |  17.0  62.6  211  23 12   9.7   5.3
 10250  17.5  63.5  203  20 10   9.9   5.4 |  18.4  65.1  207  23 12   9.7   5.3
 10000  18.3  64.9  202  20 10  10.0   5.5 |  19.2  66.6  206  23 12   9.7   5.3
  9750  19.0  66.2  201  20 10   9.9   5.5 |  19.9  67.8  204  22 12   9.7   5.3
  9500  19.8  67.6  200  20 10  10.0   5.5 |  20.6  69.1  203  22 11   9.7   5.3
  9250  20.5  68.9  199  20 10  10.2   5.6 |  21.4  70.5  202  22 11   9.8   5.4
  9000  21.3  70.3  198  20 10  10.5   5.7 |  22.1  71.8  200  22 11   9.9   5.4
  8750  22.0  71.6  197  20 10   9.9   5.4 |  22.8  73.0  199  22 11   9.8   5.4
  8500  22.8  73.0  196  19 10  12.0   6.6 |  23.6  74.5  198  21 11  10.3   5.6
  8250  23.9  75.0  195  19 10  18.8  10.3 |  24.4  75.9  197  20 10  13.0   7.1
  8000  25.5  77.9  194  17  9  23.8  13.1 |  25.4  77.7  197  17  9  15.9   8.7
  7750  27.1  80.8  193  15  8  17.0   9.3 |  26.5  79.7  197  15  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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