Soaring Guidance
Issued by NWS Pueblo, CO

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000
UXUS97 KPUB 151256
SRGPUB

SOARING FORECAST
NATIONAL WEATHER SERVICE PUEBLO CO
656 AM MDT WED MAY 15 2013


EXPERIMENTAL PRODUCT

This forecast is for Wednesday May 15, 2013:

If the trigger temperature of 64.2 F/17.9 C is reached...then
   Thermal Soaring Index....................... Excellent
   Maximum rate of lift........................ 1040 ft/min (5.3 m/s)
   Maximum height of thermals.................. 20401 ft MSL (12740 ft AGL)

Forecast maximum temperature................... 74.0 F/23.8 C
Time of trigger temperature.................... 0845 MDT
Time of overdevelopment........................ 1500 MDT
Middle/high clouds during soaring window....... Overcast opaque high
Surface winds during soaring window............ 20 mph or less
Height of the -3 thermal index................. 16229 ft MSL (8568 ft AGL)
Thermal soaring outlook for Thursday 05/16..... 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)................ Weak PVA
Potential height of wave....................... 14563 ft MSL (6902 ft AGL)
Wave soaring outlook for Thursday 05/16........ Poor

Remarks...

Sunrise/Sunset.................... 05:46:29 / 20:04:37 MDT
Total possible sunshine........... 14 hr 18 min 7 sec (858 min 7 sec)
Altitude of sun at 12:55:44 MDT... 70.04 degrees

Upper air data from numerical model forecast valid on 05/15/2013 at 0600 MDT

Freezing level.................. 14031 ft MSL (6370 ft AGL)
Convective condensation level... 16609 ft MSL (8948 ft AGL)
Lifted condensation level....... 17880 ft MSL (10219 ft AGL)
Lifted index.................... -3.1
K index......................... +22.7

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  -62.7 -80.9   255   13    7  -0.7  -0.4   82.3 180.1    34.9      M    M
 45000  -63.5 -82.3   262    7    4   0.8   0.5   57.5 135.6    21.7      M    M
 40000  -62.3 -80.1   113    4    2   0.7   0.4   37.2  98.9     9.4      M    M
 38000  -57.8 -72.0   069    4    2   8.1   4.5   34.8  94.6     8.0      M    M
 36000  -52.9 -63.2   021    5    3   8.1   4.5   33.6  92.4     7.4      M    M
 34000  -48.0 -54.4   021    7    3   8.5   4.6   32.4  90.3     6.7      M    M
 32000  -42.9 -45.2   037    7    4   8.5   4.7   31.4  88.5     6.1      M    M
 30000  -37.8 -36.0   055    8    4   8.4   4.6   30.4  86.7     5.5      M    M
 29000  -35.3 -31.5   066    8    4   8.4   4.6   29.8  85.7     5.1      M    M
 28000  -32.8 -27.0   077    8    4   8.4   4.6   29.4  85.0     4.8      M    M
 27000  -29.7 -21.5   088    9    4   8.0   4.4   28.7  83.6     4.2      M    M
 26000  -27.3 -17.1   095    9    4   8.1   4.4   28.0  82.4     3.7      M    M
 25000  -25.0 -13.0   102    9    4   8.1   4.4   27.5  81.4     3.3      M    M
 24000  -22.7  -8.9   110    8    4   7.2   3.9   26.7  80.0     2.6      M    M
 23000  -20.6  -5.1   121    6    3   7.2   3.9   25.7  78.3     1.8      M    M
 22000  -18.4  -1.1   142    4    2   7.2   3.9   24.9  76.7     1.1      M    M
 21000  -16.2   2.8   155    3    2   7.6   4.2   24.0  75.2     0.4      M    M
 20000  -13.9   7.0   160    2    1   7.6   4.2   23.3  73.9    -0.3   1199  6.1
 19500  -12.8   9.0   164    2    1   7.6   4.2   22.9  73.2    -0.6   1150  5.8
 19000  -11.7  10.9   170    2    1   7.5   4.1   22.6  72.7    -0.9   1101  5.6
 18500  -10.6  12.9   179    1    0   7.4   4.1   22.2  71.9    -1.3   1055  5.4
 18000   -9.6  14.7   329    1    0   7.5   4.1   21.8  71.2    -1.7   1008  5.1
 17500   -8.5  16.7   333    1    1   7.7   4.2   21.4  70.6    -2.1    961  4.9
 17000   -7.4  18.7   327    2    1   7.7   4.2   21.1  69.9    -2.5    913  4.6
 16500   -6.3  20.7   322    2    1   8.3   4.6   20.8  69.4    -2.9    865  4.4
 16000   -5.0  23.0   300    2    1   8.7   4.8   20.6  69.0    -3.1    812  4.1
 15500   -3.7  25.3   280    3    1   8.6   4.7   20.4  68.8    -3.3    759  3.9
 15000   -2.5  27.5   258    2    1   8.1   4.5   20.2  68.3    -3.5    707  3.6
 14500   -1.3  29.7   227    2    1   8.2   4.5   19.9  67.8    -3.8    656  3.3
 14000   -0.1  31.8   194    2    1   8.1   4.4   19.7  67.4    -4.1    606  3.1
 13500    1.1  34.0   150    2    1   8.1   4.4   19.4  66.9    -4.4    555  2.8
 13000    2.3  36.1   120    3    2   8.3   4.6   19.1  66.4    -4.7    504  2.6
 12500    3.5  38.3   105    5    3   8.3   4.6   18.9  66.0    -4.9    453  2.3
 12000    4.8  40.6   098    7    3   9.1   5.0   18.7  65.7    -5.2    400  2.0
 11750    5.5  41.9   093    7    4   9.4   5.1   18.7  65.6    -5.2    372  1.9
 11500    6.2  43.2   089    8    4   9.3   5.1   18.7  65.6    -5.3    343  1.7
 11250    6.9  44.4   086    8    4   9.3   5.1   18.6  65.5    -5.3    315  1.6
 11000    7.6  45.7   083    9    4   9.6   5.3   18.6  65.5    -5.3    287  1.5
 10750    8.3  46.9   082    9    5   9.7   5.3   18.6  65.5    -5.4    257  1.3
 10500    9.0  48.2   081    9    5   9.7   5.3   18.6  65.5    -5.4    228  1.2
 10250    9.8  49.6   080    9    5   9.7   5.3   18.6  65.5    -5.4    199  1.0
 10000   11.1  52.0   081    9    5   8.6   4.7   18.5  65.3    -5.5    143  0.7
  9750   11.8  53.2   082    8    4   8.8   4.8   18.4  65.1    -5.6    116  0.6
  9500   12.4  54.3   084    8    4   8.5   4.7   18.3  65.0    -5.7     89  0.5
  9250   13.0  55.4   082    7    4   8.1   4.4   18.2  64.8    -5.8     63  0.3
  9000   13.6  56.5   072    5    3   7.0   3.8   18.1  64.5    -6.0     39  0.2
  8750   14.2  57.6   055    4    2   9.9   5.4   17.9  64.2    -6.2     15  0.1
  8500   14.8  58.6   029    4    2  -0.8  -0.4   17.7  63.9    -6.3      M    M
  8250   13.7  56.7   346    3    1 -23.8 -13.0   16.0  60.8    -8.1     14  0.1
  8000   11.5  52.7   296    4    2 -29.6 -16.3   13.1  55.6   -11.1     73  0.4
  7750    9.3  48.7   276    6    3 -28.6 -15.7   10.3  50.5   -14.1    132  0.7
  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 * * * * * *

           05/15/2013 at 0900 MDT          |       05/15/2013 at 1200 MDT
                                           |
K index... +23.6                           | K index... +22.6
                                           |
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 -62.9 -81.2  264  15  8  -0.8  -0.4 | -62.5 -80.5  273  16  8  -0.7  -0.4
 45000 -63.8 -82.8  283   7  3   1.0   0.5 | -63.3 -81.9  265   7  4   0.6   0.3
 40000 -62.3 -80.1  000   0  0   1.2   0.7 | -62.4 -80.3  260   5  3   0.7   0.4
 38000 -57.8 -72.0  352   3  2   8.2   4.5 | -57.9 -72.2  292   6  3   8.3   4.5
 36000 -52.9 -63.2  349   7  4   8.2   4.5 | -52.9 -63.2  311   9  4   8.3   4.5
 34000 -47.8 -54.0  359   7  4   8.6   4.7 | -47.9 -54.2  313   8  4   8.6   4.7
 32000 -42.7 -44.9  027   6  3   8.6   4.7 | -42.7 -44.9  302   4  2   8.6   4.7
 30000 -37.6 -35.7  061   5  3   8.2   4.5 | -37.5 -35.5  258   3  1   8.6   4.7
 29000 -35.2 -31.4  081   6  3   8.2   4.5 | -34.3 -29.7  228   3  2   8.6   4.7
 28000 -32.1 -25.8  101   7  3   8.2   4.5 | -31.7 -25.1  214   4  2   8.7   4.8
 27000 -29.7 -21.5  108   6  3   8.0   4.4 | -29.3 -20.7  218   4  2   7.9   4.3
 26000 -27.3 -17.1  115   6  3   8.1   4.4 | -27.0 -16.6  227   4  2   7.9   4.3
 25000 -25.0 -13.0  122   6  3   8.1   4.4 | -24.6 -12.3  237   4  2   7.9   4.4
 24000 -22.7  -8.9  127   5  2   7.2   3.9 | -22.4  -8.3  245   3  2   7.4   4.0
 23000 -20.6  -5.1  133   3  1   7.2   3.9 | -20.2  -4.4  254   2  1   7.4   4.0
 22000 -18.4  -1.1  163   1  0   7.2   3.9 | -18.0  -0.4  276   1  1   7.4   4.1
 21000 -16.2   2.8  000   0  0   7.5   4.1 | -15.9   3.4  000   0  0   7.0   3.9
 20000 -14.0   6.8  068   1  1   7.5   4.1 | -13.8   7.2  114   3  1   7.1   3.9
 19500 -12.9   8.8  064   2  1   7.5   4.1 | -12.8   9.0  114   4  2   7.1   3.9
 19000 -11.8  10.8  061   2  1   7.3   4.0 | -11.7  10.9  114   5  3   7.0   3.9
 18500 -10.7  12.7  054   3  1   7.3   4.0 | -10.7  12.7  112   6  3   7.0   3.9
 18000  -9.7  14.5  048   3  2   7.3   4.0 |  -9.6  14.7  111   6  3   7.0   3.9
 17500  -8.6  16.5  045   4  2   7.5   4.1 |  -8.6  16.5  110   7  4   7.1   3.9
 17000  -7.6  18.3  044   5  3   7.5   4.1 |  -7.5  18.5  108   8  4   7.1   3.9
 16500  -6.4  20.5  042   6  3   8.6   4.7 |  -6.5  20.3  106   9  5   7.0   3.9
 16000  -5.1  22.8  034   6  3   9.0   4.9 |  -5.5  22.1  103   8  4   7.0   3.8
 15500  -3.8  25.2  027   6  3   8.9   4.9 |  -4.5  23.9  098   6  3   7.3   4.0
 15000  -2.5  27.5  024   5  3   8.5   4.7 |  -3.3  26.1  090   6  3   8.3   4.5
 14500  -1.3  29.7  022   5  3   8.5   4.7 |  -2.2  28.0  080   5  3   8.2   4.5
 14000  -0.0  32.0  028   5  3   8.4   4.6 |  -0.8  30.6  074   5  3  10.0   5.5
 13500   1.2  34.2  040   5  2   8.4   4.6 |   0.6  33.1  072   5  3   9.9   5.4
 13000   2.5  36.5  055   5  2   8.2   4.5 |   2.1  35.8  072   5  3   9.9   5.4
 12500   3.7  38.7  073   5  3   8.2   4.5 |   3.6  38.5  071   5  3   9.9   5.5
 12000   4.9  40.8  082   6  3   8.5   4.7 |   5.1  41.2  071   5  3   9.7   5.3
 11750   5.5  41.9  080   6  3   8.6   4.7 |   5.8  42.4  070   5  3   9.6   5.3
 11500   6.2  43.2  079   6  3   8.5   4.7 |   6.5  43.7  069   5  3   9.7   5.3
 11250   6.8  44.2  077   7  4   8.7   4.8 |   7.2  45.0  068   5  3   9.7   5.3
 11000   7.5  45.5  076   7  4   9.0   5.0 |   8.0  46.4  068   5  3   9.7   5.3
 10750   8.1  46.6  073   8  4   9.2   5.1 |   8.7  47.7  067   5  3   9.8   5.4
 10500   8.8  47.8  071   8  4   9.2   5.0 |   9.4  48.9  067   5  3   9.7   5.3
 10250  10.2  50.4  067   9  4   9.2   5.1 |  10.9  51.6  065   5  3  10.1   5.6
 10000  10.9  51.6  064   9  4   9.3   5.1 |  11.7  53.1  065   5  3  10.3   5.6
  9750  11.6  52.9  061   9  4   9.3   5.1 |  12.4  54.3  065   5  3  10.3   5.6
  9500  12.3  54.1  059   9  5   9.3   5.1 |  13.2  55.8  065   5  3  10.1   5.6
  9250  13.0  55.4  055   8  4   9.1   5.0 |  13.9  57.0  064   5  3   9.7   5.3
  9000  13.6  56.5  049   7  4   9.3   5.1 |  14.6  58.3  063   5  3   9.7   5.3
  8750  14.3  57.7  041   6  3   8.6   4.7 |  15.4  59.7  062   5  3   9.1   5.0
  8500  14.9  58.8  031   6  3  11.2   6.2 |  16.1  61.0  061   5  3  11.7   6.4
  8250  15.9  60.6  027   5  3  15.4   8.4 |  17.1  62.8  061   6  3  16.1   8.8
  8000  17.0  62.6  026   4  2  14.4   7.9 |  18.3  64.9  062   6  3  15.6   8.5
  7750  18.1  64.6  025   4  2  18.5  10.2 |  19.4  66.9  062   6  3  18.9  10.4
  7500     M     M    M   M  M     M     M |     M     M    M   M  M     M     M
  7250     M     M    M   M  M     M     M |     M     M    M   M  M     M     M
  7000     M     M    M   M  M     M     M |     M     M    M   M  M     M     M
  6750     M     M    M   M  M     M     M |     M     M    M   M  M     M     M

           05/15/2013 at 1500 MDT          |       05/15/2013 at 1800 MDT
                                           |
K index... +24.9                           | K index... +25.1
                                           |
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 -62.1 -79.8  265  18  9  -0.1  -0.0 | -63.1 -81.6  279  21 11  -0.3  -0.2
 45000 -62.3 -80.1  262  16  8  -0.1  -0.1 | -63.4 -82.1  270  20 10   0.4   0.2
 40000 -62.5 -80.5  259  10  5  -1.2  -0.7 | -62.8 -81.0  246  18  9   0.8   0.4
 38000 -58.1 -72.6  271  10  5   8.5   4.6 | -58.0 -72.4  249  16  8   8.7   4.8
 36000 -52.4 -62.3  284  12  6   8.5   4.6 | -52.8 -63.0  255  15  8   8.7   4.8
 34000 -47.2 -53.0  280  12  6   8.7   4.8 | -47.5 -53.5  257  16  8   8.7   4.8
 32000 -42.0 -43.6  269  11  6   8.8   4.8 | -42.3 -44.1  257  17  9   8.8   4.8
 30000 -36.8 -34.2  264  11  6   8.7   4.8 | -37.0 -34.6  255  16  8   8.9   4.9
 29000 -34.3 -29.7  263  11  6   8.7   4.8 | -34.4 -29.9  254  15  8   8.9   4.9
 28000 -31.7 -25.1  262  10  5   8.7   4.8 | -31.0 -23.8  252  13  7   9.0   4.9
 27000 -29.3 -20.7  267  10  5   7.8   4.3 | -28.6 -19.5  250  11  6   7.9   4.3
 26000 -26.9 -16.4  275   9  5   7.8   4.3 | -26.3 -15.3  248  10  5   7.9   4.4
 25000 -24.6 -12.3  285   8  4   7.8   4.3 | -23.9 -11.0  245   9  4   8.0   4.4
 24000 -22.4  -8.3  290   7  4   7.1   3.9 | -21.7  -7.1  235   8  4   6.8   3.7
 23000 -19.8  -3.6  280   5  2   7.1   3.9 | -19.7  -3.5  223   9  5   6.8   3.7
 22000 -17.7   0.1  261   3  1   7.2   3.9 | -17.8  -0.0  213  10  5   6.8   3.7
 21000 -15.7   3.7  189   4  2   6.6   3.6 | -15.9   3.4  201  12  6   6.3   3.4
 20000 -13.8   7.2  167   8  4   6.7   3.7 | -14.0   6.8  191  15  8   6.3   3.4
 19500 -12.8   9.0  162  10  5   6.7   3.7 | -13.1   8.4  187  17  9   6.3   3.5
 19000 -11.8  10.8  160  12  6   7.0   3.8 | -12.2  10.0  184  19 10   6.9   3.8
 18500 -10.8  12.6  159  13  7   7.1   3.9 | -11.1  12.0  183  19 10   7.5   4.1
 18000  -9.7  14.5  158  14  7   7.2   3.9 | -10.0  14.0  181  19 10   7.4   4.1
 17500  -8.6  16.5  159  15  8   7.6   4.1 |  -8.8  16.2  180  18  9   8.6   4.7
 17000  -7.5  18.5  160  14  7   7.5   4.1 |  -7.5  18.5  180  16  8   8.5   4.7
 16500  -6.4  20.5  161  13  7   7.8   4.3 |  -6.3  20.7  179  15  8   8.3   4.6
 16000  -5.3  22.5  158  11  6   7.8   4.3 |  -5.1  22.8  176  13  7   8.2   4.5
 15500  -4.2  24.4  154   9  4   8.0   4.4 |  -3.9  25.0  173  11  5   8.3   4.5
 15000  -3.0  26.6  146   7  4   8.4   4.6 |  -2.7  27.1  170   9  5   8.4   4.6
 14500  -1.7  28.9  132   5  3   8.5   4.6 |  -1.4  29.5  167   7  4   8.3   4.5
 14000  -0.4  31.3  122   5  2  10.0   5.5 |  -0.1  31.8  164   6  3   9.7   5.3
 13500   1.1  34.0  117   4  2   9.9   5.4 |   1.3  34.3  163   6  3   9.6   5.3
 13000   2.5  36.5  112   4  2   9.6   5.3 |   2.7  36.9  161   5  3   9.5   5.2
 12500   3.9  39.0  107   4  2   9.6   5.3 |   4.2  39.6  155   3  2   9.5   5.2
 12000   5.4  41.7  102   4  2   9.8   5.4 |   5.6  42.1  141   2  1   9.4   5.2
 11750   6.1  43.0  099   4  2   9.8   5.4 |   6.3  43.3  130   2  1   9.4   5.2
 11500   6.9  44.4  097   3  2   9.8   5.4 |   7.0  44.6  115   2  1   9.4   5.2
 11250   7.6  45.7  094   3  2   9.9   5.4 |   7.7  45.9  096   2  1   9.4   5.2
 11000   8.3  46.9  090   3  2  10.0   5.5 |   8.4  47.1  076   2  1   9.6   5.3
 10750   9.1  48.4  087   3  2  10.0   5.5 |   9.1  48.4  057   2  1   9.7   5.3
 10500   9.8  49.6  083   3  2  10.0   5.5 |   9.8  49.6  044   2  1   9.7   5.3
 10250  10.5  50.9  079   3  2  10.0   5.5 |  11.3  52.3  030   3  2   9.7   5.3
 10000  11.3  52.3  075   3  2   9.9   5.4 |  12.0  53.6  026   4  2   9.8   5.4
  9750  12.0  53.6  071   3  2   9.9   5.4 |  12.7  54.9  024   4  2   9.8   5.4
  9500  13.5  56.3  063   3  2   9.9   5.4 |  13.4  56.1  021   5  3   9.7   5.3
  9250  14.2  57.6  060   3  2   9.8   5.4 |  14.2  57.6  020   5  3   9.6   5.3
  9000  15.0  59.0  058   3  2   9.9   5.4 |  14.9  58.8  020   5  3   9.6   5.3
  8750  15.7  60.3  055   3  2   9.5   5.2 |  15.6  60.1  020   6  3   9.6   5.2
  8500  16.4  61.5  053   3  2  10.9   6.0 |  16.3  61.3  020   6  3   9.9   5.4
  8250  17.3  63.1  055   3  2  13.7   7.5 |  17.0  62.6  022   6  3  10.6   5.8
  8000  18.3  64.9  059   4  2  14.0   7.7 |  17.7  63.9  027   5  3  10.9   6.0
  7750  19.3  66.7  062   4  2  14.9   8.2 |  18.5  65.3  033   5  2  10.8   5.9
  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
________________________________________________________________________________

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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