Soaring Guidance
Issued by NWS Pueblo, CO

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000
UXUS97 KPUB 131215
SRGPUB

SOARING FORECAST
NATIONAL WEATHER SERVICE PUEBLO CO
615 AM MDT MON MAY 13 2013


EXPERIMENTAL PRODUCT

This forecast is for Monday May 13, 2013:

If the trigger temperature of 65.0 F/18.3 C is reached...then
   Thermal Soaring Index....................... Excellent
   Maximum rate of lift........................ 1538 ft/min (7.8 m/s)
   Maximum height of thermals.................. 24474 ft MSL (16811 ft AGL)

Forecast maximum temperature................... 81.0 F/27.7 C
Time of trigger temperature.................... 0830 MDT
Time of overdevelopment........................ None
Middle/high clouds during soaring window....... Overcast thin high
Surface winds during soaring window............ 20 mph or less
Height of the -3 thermal index................. 19041 ft MSL (11378 ft AGL)
Thermal soaring outlook for Tuesday 05/14...... Excellent

Wave Soaring Index............................. Poor
Wave Soaring Index trend (to 1800 MDT)......... Poor
Height of stable layer (12-18K ft MSL)......... None
Weak PVA/NVA (through 1800 MDT)................ Neither
Potential height of wave....................... 15794 ft MSL (8131 ft AGL)
Wave soaring outlook for Tuesday 05/14......... Poor

Remarks...

Sunrise/Sunset.................... 05:48:17 / 20:02:47 MDT
Total possible sunshine........... 14 hr 14 min 29 sec (854 min 29 sec)
Altitude of sun at 12:55:43 MDT... 69.57 degrees

Upper air data from numerical model forecast valid on 05/13/2013 at 0600 MDT

Freezing level.................. 14147 ft MSL (6484 ft AGL)
Convective condensation level... 19099 ft MSL (11436 ft AGL)
Lifted condensation level....... 20581 ft MSL (12918 ft AGL)
Lifted index.................... -3.8
K index......................... +11.2

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  -65.6 -86.1   008   20   10  -0.8  -0.5   77.7 171.8    29.9      M    M
 45000  -66.2 -87.2   024   31   16   2.8   1.5   54.3 129.7    17.1      M    M
 40000  -61.6 -78.9   026   42   22   6.0   3.3   37.9 100.3     7.3      M    M
 38000  -56.7 -70.1   025   37   19   8.2   4.5   36.2  97.1     6.3      M    M
 36000  -51.7 -61.1   023   32   16   8.2   4.5   35.1  95.2     5.7      M    M
 34000  -46.9 -52.4   020   29   15   7.9   4.3   33.6  92.5     4.7      M    M
 32000  -42.2 -44.0   016   29   15   7.9   4.3   32.2  89.9     3.7      M    M
 30000  -37.4 -35.3   012   26   13   8.2   4.5   30.8  87.5     2.8      M    M
 29000  -34.9 -30.8   010   24   13   8.2   4.5   30.2  86.4     2.3      M    M
 28000  -32.5 -26.5   008   23   12   8.2   4.5   29.7  85.5     1.9      M    M
 27000  -29.5 -21.1   004   20   11   8.0   4.4   28.8  83.9     1.2      M    M
 26000  -27.1 -16.8   359   19   10   8.0   4.4   28.2  82.7     0.7      M    M
 25000  -24.7 -12.5   354   17    9   8.1   4.4   27.6  81.8     0.2      M    M
 24000  -22.4  -8.3   351   16    8   7.8   4.3   26.9  80.4    -0.4   1582  8.0
 23000  -20.0  -4.0   348   16    8   7.8   4.3   26.2  79.2    -1.0   1483  7.5
 22000  -17.7   0.1   345   15    8   7.9   4.4   25.6  78.1    -1.5   1383  7.0
 21000  -15.2   4.6   349   15    8   8.4   4.6   25.0  77.1    -2.1   1280  6.5
 20000  -12.8   9.0   354   15    8   8.4   4.6   24.6  76.2    -2.6   1176  6.0
 19500  -11.5  11.3   357   15    8   8.5   4.7   24.4  75.9    -2.8   1124  5.7
 19000  -10.3  13.5   001   15    8   7.4   4.0   24.1  75.4    -3.0   1073  5.5
 18500   -9.2  15.4   005   15    8   7.4   4.0   23.7  74.6    -3.4   1025  5.2
 18000   -8.1  17.4   010   15    8   7.0   3.8   23.3  73.9    -3.7    976  5.0
 17500   -7.1  19.2   007   16    8   6.4   3.5   22.7  72.9    -4.3    932  4.7
 17000   -6.1  21.0   005   18    9   6.3   3.5   22.2  71.9    -4.8    889  4.5
 16500   -5.2  22.6   001   19   10   6.7   3.7   21.6  71.0    -5.3    845  4.3
 16000   -4.2  24.4   355   20   10   6.7   3.7   21.1  70.1    -5.9    802  4.1
 15500   -3.3  26.1   351   21   11   7.5   4.1   20.7  69.2    -6.4    758  3.9
 15000   -2.2  28.0   350   20   11   7.8   4.3   20.4  68.7    -6.8    710  3.6
 14500   -1.0  30.2   349   20   10   8.1   4.4   20.1  68.1    -7.2    661  3.4
 14000    0.2  32.4   350   19   10   8.4   4.6   19.8  67.7    -7.4    610  3.1
 13500    1.4  34.5   352   17    9   8.4   4.6   19.6  67.3    -7.7    558  2.8
 13000    2.7  36.9   355   16    8   8.6   4.7   19.4  67.0    -7.9    505  2.6
 12500    4.0  39.2   358   15    8   8.6   4.7   19.2  66.6    -8.1    452  2.3
 12000    5.3  41.5   360   14    7   8.8   4.8   19.1  66.3    -8.4    398  2.0
 11750    5.9  42.6   360   14    7   8.7   4.8   19.0  66.2    -8.5    371  1.9
 11500    6.6  43.9   001   14    7   8.8   4.8   18.9  66.1    -8.5    344  1.7
 11250    7.3  45.1   001   13    7   8.7   4.8   18.8  65.9    -8.6    317  1.6
 11000    7.9  46.2   001   13    7   8.7   4.8   18.8  65.8    -8.7    290  1.5
 10750    8.6  47.5   360   13    7   8.7   4.8   18.7  65.6    -8.9    263  1.3
 10500    9.2  48.6   360   13    7   8.7   4.8   18.6  65.5    -9.0    236  1.2
 10250   10.6  51.1   358   12    6   9.5   5.2   18.5  65.3    -9.1    180  0.9
 10000   11.3  52.3   357   12    6   9.4   5.2   18.5  65.3    -9.2    152  0.8
  9750   12.0  53.6   356   12    6   9.3   5.1   18.5  65.2    -9.2    124  0.6
  9500   12.6  54.7   354   12    6   6.4   3.5   18.3  65.0    -9.4     98  0.5
  9250   12.9  55.2   350   12    6   3.9   2.1   18.0  64.3    -9.8     80  0.4
  9000   13.3  55.9   346   12    6   6.2   3.4   17.6  63.6   -10.2     62  0.3
  8750   13.6  56.5   342   13    6  -0.5  -0.3   17.2  62.9   -10.6     45  0.2
  8500   12.8  55.0   334   12    6 -21.2 -11.6   15.7  60.2   -12.1     61  0.3
  8250   10.7  51.3   319   10    5 -31.5 -17.3   12.8  55.0   -15.1    119  0.6
  8000    8.5  47.3   298    9    5 -24.2 -13.3    9.9  49.8   -18.0    177  0.9
  7750    6.3  43.3   277    9    5 -43.0 -23.6    7.1  44.7   -20.9    234  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 * * * * * *

           05/13/2013 at 0900 MDT          |       05/13/2013 at 1200 MDT
                                           |
K index... +16.4                           | K index... +20.2
                                           |
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 -66.4 -87.5  016  14  7  -1.5  -0.8 | -67.6 -89.7  025   8  4  -1.8  -1.0
 45000 -67.3 -89.1  039  26 13   3.9   2.2 | -68.6 -91.5  055  20 10   4.9   2.7
 40000 -61.3 -78.3  046  36 19   6.8   3.7 | -61.3 -78.3  061  27 14   6.8   3.7
 38000 -56.5 -69.7  041  32 16   8.1   4.4 | -56.4 -69.5  058  25 13   8.3   4.5
 36000 -51.6 -60.9  034  28 14   8.1   4.4 | -50.8 -59.4  053  23 12   8.3   4.6
 34000 -46.6 -51.9  027  27 14   8.4   4.6 | -45.7 -50.3  047  22 11   8.5   4.7
 32000 -41.6 -42.9  021  28 14   8.4   4.6 | -40.6 -41.1  040  21 11   8.5   4.7
 30000 -36.6 -33.9  018  25 13   8.1   4.4 | -35.7 -32.3  032  19 10   8.1   4.4
 29000 -34.2 -29.6  016  23 12   8.1   4.4 | -33.3 -27.9  027  18  9   8.1   4.4
 28000 -31.2 -24.2  013  20 10   7.9   4.3 | -30.9 -23.6  021  16  8   8.0   4.4
 27000 -28.9 -20.0  009  18  9   7.6   4.2 | -28.7 -19.7  013  16  8   7.3   4.0
 26000 -26.7 -16.1  003  16  8   7.6   4.2 | -26.5 -15.7  005  15  8   7.3   4.0
 25000 -24.4 -11.9  356  15  8   7.6   4.2 | -24.4 -11.9  356  15  8   7.3   4.0
 24000 -22.2  -8.0  347  14  7   7.3   4.0 | -22.2  -8.0  350  15  8   7.4   4.1
 23000 -20.0  -4.0  338  14  7   7.4   4.0 | -19.5  -3.1  345  16  8   7.4   4.1
 22000 -17.8  -0.0  330  15  8   7.6   4.1 | -17.3   0.9  341  16  8   7.5   4.1
 21000 -15.5   4.1  329  15  8   8.1   4.5 | -15.1   4.8  334  17  9   7.6   4.2
 20000 -13.0   8.6  329  15  8   8.1   4.5 | -12.8   9.0  328  17  9   7.6   4.2
 19500 -11.8  10.8  330  15  7   8.2   4.5 | -11.7  10.9  325  18  9   7.6   4.2
 19000 -10.7  12.7  332  15  8   7.6   4.1 | -10.6  12.9  325  17  9   7.3   4.0
 18500  -9.5  14.9  338  15  8   7.6   4.2 |  -9.5  14.9  328  17  9   7.3   4.0
 18000  -8.4  16.9  343  16  8   7.5   4.1 |  -8.5  16.7  331  16  8   6.2   3.4
 17500  -7.3  18.9  348  17  9   7.5   4.1 |  -7.6  18.3  335  16  8   5.7   3.1
 17000  -6.1  21.0  352  19 10   7.5   4.1 |  -6.8  19.8  340  16  8   6.0   3.3
 16500  -5.1  22.8  352  20 10   6.9   3.8 |  -5.7  21.7  341  15  8   8.4   4.6
 16000  -4.1  24.6  350  20 10   7.0   3.8 |  -4.5  23.9  342  15  7   8.2   4.5
 15500  -3.0  26.6  348  20 10   7.9   4.3 |  -3.3  26.1  342  14  7   8.9   4.9
 15000  -1.8  28.8  346  19 10   8.1   4.4 |  -2.0  28.4  341  12  6   9.0   4.9
 14500  -0.7  30.7  344  17  9   8.1   4.4 |  -0.7  30.7  339  11  6   9.0   4.9
 14000   0.5  32.9  345  16  8   8.1   4.5 |   0.7  33.3  340   9  4   9.1   5.0
 13500   1.7  35.1  346  15  8   8.2   4.5 |   2.0  35.6  341   6  3   9.3   5.1
 13000   3.0  37.4  348  14  7   8.3   4.5 |   3.4  38.1  343   6  3   9.7   5.3
 12500   4.2  39.6  350  13  6   8.3   4.5 |   4.8  40.6  346   5  3   9.8   5.4
 12000   5.4  41.7  352  12  6   8.4   4.6 |   6.3  43.3  347   5  2  10.1   5.5
 11750   6.1  43.0  352  11  6   8.4   4.6 |   7.1  44.8  348   5  2  10.1   5.5
 11500   6.7  44.1  353  11  6   8.4   4.6 |   7.8  46.0  349   5  2  10.1   5.5
 11250   7.4  45.3  353  10  5   8.7   4.8 |   8.6  47.5  349   5  2  10.0   5.5
 11000   8.0  46.4  352  10  5   8.8   4.8 |   9.3  48.7  350   5  2   9.9   5.4
 10750   8.7  47.7  351   9  5   8.8   4.8 |  10.1  50.2  351   5  2   9.9   5.5
 10500   9.3  48.7  350   9  5   8.8   4.8 |  10.8  51.4  352   5  2   9.9   5.4
 10250  10.7  51.3  345   8  4   9.4   5.2 |  11.5  52.7  353   5  2   9.8   5.4
 10000  11.4  52.5  341   8  4   9.4   5.1 |  12.3  54.1  355   5  2   9.8   5.4
  9750  12.1  53.8  337   7  4   9.3   5.1 |  13.7  56.7  357   5  2   9.9   5.4
  9500  12.8  55.0  333   7  4   8.9   4.9 |  14.5  58.1  358   5  2  10.2   5.6
  9250  13.4  56.1  329   7  4   8.8   4.8 |  15.2  59.4  359   5  2  10.5   5.8
  9000  14.0  57.2  325   7  4   8.5   4.7 |  16.0  60.8  359   5  2   9.8   5.4
  8750  14.7  58.5  321   7  4   9.8   5.4 |  16.8  62.2  360   5  2  12.3   6.7
  8500  15.5  59.9  317   7  4  12.5   6.9 |  17.8  64.0  005   4  2  16.5   9.1
  8250  16.4  61.5  311   7  3  13.3   7.3 |  19.1  66.4  012   4  2  17.3   9.5
  8000  17.3  63.1  305   6  3  12.9   7.1 |  20.3  68.5  020   4  2  17.0   9.3
  7750  18.2  64.8  299   6  3  14.0   7.7 |  21.6  70.9  028   4  2  17.8   9.7
  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

           05/13/2013 at 1500 MDT          |       05/13/2013 at 1800 MDT
                                           |
K index... +23.3                           | K index... +24.1
                                           |
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 -68.4 -91.1  031   3  2  -1.8  -1.0 | -67.9 -90.2  360   2  1  -1.7  -1.0
 45000 -69.2 -92.6  066  17  9   5.4   3.0 | -68.7 -91.7  081  15  8   5.4   2.9
 40000 -61.1 -78.0  077  23 12   7.3   4.0 | -60.7 -77.3  092  21 11   7.1   3.9
 38000 -56.1 -69.0  076  20 10   8.4   4.6 | -55.8 -68.4  094  17  9   8.2   4.5
 36000 -50.5 -58.9  073  17  9   8.4   4.6 | -50.3 -58.5  097  12  6   8.2   4.5
 34000 -45.5 -49.9  064  16  8   8.4   4.6 | -45.4 -49.7  085   9  5   8.2   4.5
 32000 -40.5 -40.9  053  15  8   8.4   4.6 | -40.4 -40.7  062   8  4   8.2   4.5
 30000 -35.6 -32.1  041  13  7   8.2   4.5 | -35.5 -31.9  042   7  4   8.2   4.5
 29000 -33.1 -27.6  035  12  6   8.2   4.5 | -33.1 -27.6  033   7  4   8.2   4.5
 28000 -30.7 -23.3  027  11  6   8.1   4.4 | -30.6 -23.1  023   7  4   8.2   4.5
 27000 -28.4 -19.1  018  12  6   7.7   4.2 | -28.3 -18.9  020   8  4   7.9   4.3
 26000 -26.1 -15.0  010  13  7   7.8   4.3 | -25.9 -14.6  018   9  5   7.9   4.4
 25000 -23.8 -10.8  003  14  7   7.8   4.3 | -23.6 -10.5  017  10  5   8.0   4.4
 24000 -21.6  -6.9  001  14  7   7.1   3.9 | -21.4  -6.5  014   9  5   7.1   3.9
 23000 -19.0  -2.2  360  13  7   7.1   3.9 | -18.8  -1.8  010   8  4   7.1   3.9
 22000 -16.9   1.6  360  12  6   7.2   3.9 | -16.7   1.9  005   7  4   7.1   3.9
 21000 -14.8   5.4  344  13  7   7.3   4.0 | -14.6   5.7  349   7  4   7.2   3.9
 20000 -12.7   9.1  330  14  7   7.3   4.0 | -12.5   9.5  334   8  4   7.2   3.9
 19500 -11.6  11.1  324  15  8   7.3   4.0 | -11.4  11.5  328   8  4   7.2   4.0
 19000 -10.5  13.1  321  15  8   6.9   3.8 | -10.4  13.3  322   9  5   7.5   4.1
 18500  -9.5  14.9  318  14  7   6.9   3.8 |  -9.3  15.3  317   9  5   7.5   4.1
 18000  -8.5  16.7  315  13  7   7.1   3.9 |  -8.2  17.2  313  10  5   7.6   4.2
 17500  -7.5  18.5  314  11  6   7.2   3.9 |  -7.1  19.2  314   8  4   7.6   4.2
 17000  -6.5  20.3  314   9  5   7.4   4.0 |  -6.0  21.2  316   6  3   7.7   4.2
 16500  -5.3  22.5  315   7  3   8.7   4.8 |  -4.8  23.4  318   4  2   8.6   4.7
 16000  -4.0  24.8  322   4  2   8.5   4.7 |  -3.5  25.7  324   2  1   8.4   4.6
 15500  -2.7  27.1  333   2  1   9.7   5.3 |  -2.2  28.0  000   0  0   9.5   5.2
 15000  -1.3  29.7  329   2  1   9.8   5.4 |  -0.8  30.6  000   0  0   9.6   5.3
 14500   0.2  32.4  324   2  1   9.7   5.3 |   0.6  33.1  000   0  0   9.6   5.3
 14000   1.6  34.9  328   1  1   9.7   5.3 |   2.0  35.6  108   1  0   9.5   5.2
 13500   3.0  37.4  333   1  1   9.7   5.3 |   3.4  38.1  111   1  0   9.5   5.2
 13000   4.5  40.1  333   1  0   9.7   5.3 |   4.9  40.8  118   1  1   9.5   5.2
 12500   5.9  42.6  333   1  0   9.7   5.3 |   6.3  43.3  123   2  1   9.5   5.2
 12000   7.4  45.3  338   1  0   9.9   5.4 |   7.7  45.9  128   2  1   9.5   5.2
 11750   8.1  46.6  000   0  0   9.9   5.4 |   8.4  47.1  130   2  1   9.5   5.2
 11500   8.9  48.0  000   0  0   9.9   5.4 |   9.1  48.4  132   2  1   9.5   5.2
 11250   9.6  49.3  000   0  0  10.0   5.5 |   9.8  49.6  133   3  1   9.6   5.3
 11000  10.3  50.5  000   0  0  10.0   5.5 |  10.5  50.9  135   3  2   9.7   5.3
 10750  11.1  52.0  000   0  0  10.0   5.5 |  11.2  52.2  136   3  2   9.7   5.3
 10500  11.8  53.2  000   0  0  10.0   5.5 |  12.0  53.6  138   4  2   9.7   5.3
 10250  12.6  54.7  000   0  0   9.9   5.5 |  12.7  54.9  139   4  2   9.8   5.4
 10000  13.3  55.9  082   1  0   9.9   5.4 |  13.4  56.1  139   4  2   9.8   5.4
  9750  14.0  57.2  084   1  0   9.9   5.4 |  14.9  58.8  140   4  2   9.8   5.4
  9500  15.5  59.9  088   1  0   9.9   5.4 |  15.6  60.1  141   4  2   9.6   5.3
  9250  16.2  61.2  092   1  0  10.0   5.5 |  16.3  61.3  140   5  2   9.5   5.2
  9000  17.0  62.6  095   1  1   9.6   5.3 |  17.0  62.6  140   5  2   9.5   5.2
  8750  17.7  63.9  098   1  1  11.1   6.1 |  17.7  63.9  140   5  2   9.7   5.3
  8500  18.7  65.7  107   1  1  14.5   7.9 |  18.4  65.1  139   5  3  10.6   5.8
  8250  19.8  67.6  115   2  1  15.8   8.7 |  19.2  66.6  137   5  3  11.0   6.0
  8000  20.9  69.6  119   3  2  15.0   8.2 |  19.9  67.8  135   5  3  10.8   5.9
  7750  22.0  71.6  121   4  2  17.1   9.4 |  20.7  69.3  133   6  3  11.5   6.3
  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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