Soaring Guidance
Issued by NWS Pueblo, CO

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000
UXUS97 KPUB 201041
SRGPUB

SOARING FORECAST
NATIONAL WEATHER SERVICE PUEBLO CO
441 AM MDT MON MAY 20 2013


EXPERIMENTAL PRODUCT

This forecast is for Monday May 20, 2013:

If the trigger temperature of 47.1 F/8.4 C is reached...then
   Thermal Soaring Index....................... Good
   Maximum rate of lift........................ 754 ft/min (3.8 m/s)
   Maximum height of thermals.................. 18262 ft MSL (10600 ft AGL)

Forecast maximum temperature................... 59.0 F/15.5 C
Time of trigger temperature.................... 0800 MDT
Time of overdevelopment........................ 1300 MDT
Middle/high clouds during soaring window....... Broken/overcast thin middle
Surface winds during soaring window............ 20 mph or less
Height of the -3 thermal index................. 15673 ft MSL (8012 ft AGL)
Thermal soaring outlook for Tuesday 05/21...... Good

Wave Soaring Index............................. Poor
Wave Soaring Index trend (to 1800 MDT)......... Increasing
Height of stable layer (12-18K ft MSL)......... None
Weak PVA/NVA (through 1800 MDT)................ Weak PVA
Potential height of wave....................... 15555 ft MSL (7893 ft AGL)
Wave soaring outlook for Tuesday 05/21......... Poor

Remarks...

Sunrise/Sunset.................... 05:42:27 / 20:09:03 MDT
Total possible sunshine........... 14 hr 26 min 37 sec (866 min 37 sec)
Altitude of sun at 12:55:56 MDT... 71.13 degrees

Upper air data from numerical model forecast valid on 05/20/2013 at 0600 MDT

Freezing level.................. 10270 ft MSL (2608 ft AGL)
Convective condensation level... 12730 ft MSL (5068 ft AGL)
Lifted condensation level....... 15195 ft MSL (7533 ft AGL)
Lifted index.................... -3.1
K index......................... +19.6

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  -54.8 -66.6   262   15    8   3.8   2.1   94.4 201.9    47.1      M    M
 45000  -48.8 -55.8   275   25   13   3.8   2.1   80.5 176.9    41.5      M    M
 40000  -43.1 -45.6   268   34   18   3.9   2.1   67.1 152.7    35.2      M    M
 38000  -43.4 -46.1   267   29   15  -3.0  -1.6   58.0 136.4    29.8      M    M
 36000  -45.1 -49.2   267   19   10  -3.8  -1.6   47.1 116.8    22.8      M    M
 34000  -46.6 -51.9   269    8    4   1.5   0.8   37.4  99.3    16.3      M    M
 32000  -45.9 -50.6   087   11    5   1.0   0.6   30.0  86.0    11.2      M    M
 30000  -44.8 -48.6   087   25   13   8.0   4.4   24.0  75.2     6.9      M    M
 29000  -42.6 -44.7   086   20   10   7.3   4.0   22.9  73.3     6.2      M    M
 28000  -39.8 -39.6   083   14    7   7.3   4.0   21.8  71.2     5.4      M    M
 27000  -37.6 -35.7   077    9    5   7.7   4.3   21.0  69.8     4.8      M    M
 26000  -35.2 -31.4   070    5    3   8.0   4.4   20.2  68.4     4.2      M    M
 25000  -32.8 -27.0   037    2    1   8.0   4.4   19.6  67.3     3.7      M    M
 24000  -30.4 -22.7   300    3    2   8.0   4.4   19.1  66.4     3.3      M    M
 23000  -28.0 -18.4   305    4    2   8.1   4.4   18.4  65.1     2.8      M    M
 22000  -25.6 -14.1   309    5    3   8.1   4.4   17.8  64.0     2.3      M    M
 21000  -23.2  -9.8   313    6    3   7.8   4.3   17.3  63.1     1.9      M    M
 20000  -20.9  -5.6   319    5    3   7.8   4.3   16.5  61.7     1.2      M    M
 19500  -19.8  -3.6   323    5    3   7.8   4.3   16.2  61.1     0.9      M    M
 19000  -18.6  -1.5   327    5    3   7.8   4.3   15.9  60.6     0.6      M    M
 18500  -17.5   0.5   330    5    3   6.7   3.7   15.6  60.0     0.3      M    M
 18000  -16.6   2.1   313    6    3   5.9   3.2   14.9  58.8    -0.3    934  4.7
 17500  -15.8   3.6   301    7    4   5.9   3.2   14.3  57.7    -0.9    894  4.5
 17000  -14.9   5.2   297    8    4   6.4   3.5   13.7  56.6    -1.5    852  4.3
 16500  -13.9   7.0   295   10    5   6.4   3.5   13.1  55.6    -2.0    809  4.1
 16000  -13.0   8.6   296   11    5   6.4   3.5   12.5  54.6    -2.6    767  3.9
 15500  -12.1  10.2   300   11    6   6.5   3.5   12.0  53.6    -3.1    724  3.7
 15000  -11.1  12.0   303   12    6   6.7   3.7   11.5  52.6    -3.7    681  3.5
 14500  -10.1  13.8   309   11    6   6.9   3.8   11.0  51.8    -4.2    636  3.2
 14000   -9.1  15.6   316   10    5   7.0   3.8   10.5  50.9    -4.7    592  3.0
 13500   -8.1  17.4   321   10    5   7.2   3.9   10.1  50.2    -5.1    546  2.8
 13000   -7.0  19.4   326   10    5   7.3   4.0    9.7  49.4    -5.6    499  2.5
 12500   -5.9  21.4   330    9    5   8.4   4.6    9.4  48.9    -5.9    449  2.3
 12000   -4.6  23.7   333    9    5   8.4   4.6    9.2  48.5    -6.1    397  2.0
 11750   -4.0  24.8   335    9    5   8.7   4.7    9.1  48.4    -6.2    371  1.9
 11500   -3.4  25.9   337    9    5   8.8   4.8    9.0  48.2    -6.3    344  1.7
 11250   -2.7  27.1   339    9    5   8.8   4.8    8.9  48.1    -6.5    317  1.6
 11000   -2.1  28.2   340    9    5   8.7   4.8    8.9  47.9    -6.5    290  1.5
 10750   -1.4  29.5   343   10    5   8.2   4.5    8.8  47.8    -6.7    264  1.3
 10500   -0.8  30.6   348   10    5   8.0   4.4    8.6  47.5    -6.8    239  1.2
 10250    0.3  32.5   356   11    5   8.0   4.4    8.4  47.1    -7.1    189  1.0
 10000    0.9  33.6   359   11    6   7.7   4.2    8.2  46.8    -7.3    164  0.8
  9750    1.5  34.7   002   11    6   7.6   4.2    8.1  46.5    -7.5    140  0.7
  9500    2.1  35.8   004   11    6   7.7   4.2    7.9  46.2    -7.7    115  0.6
  9250    2.6  36.7   007   11    6   7.5   4.1    7.7  45.9    -7.9     91  0.5
  9000    3.2  37.8   005   11    6   7.4   4.1    7.6  45.6    -8.1     67  0.3
  8750    3.7  38.7   002   12    6   6.9   3.8    7.4  45.3    -8.3     43  0.2
  8500    4.3  39.7   359   13    7   8.6   4.7    7.2  44.9    -8.5     19  0.1
  8250    4.7  40.5   356   13    7  -2.6  -1.4    6.9  44.4    -8.8      M    M
  8000    3.6  38.5   336    9    4 -25.8 -14.1    5.0  41.0   -10.7     25  0.1
  7750    2.5  36.5   295    7    3  16.8   9.2    3.2  37.7   -12.5     51  0.3
  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 * * * * * *

           05/20/2013 at 0900 MDT          |       05/20/2013 at 1200 MDT
                                           |
K index... +20.4                           | K index... +20.4
                                           |
Height Temperature  Wnd WndSpd  Lapse Rate | Temperature  Wnd WndSpd  Lapse Rate
ft MSL deg C deg F  Dir kt m/s  C/km F/kft | deg C deg F  Dir kt m/s  C/km F/kft
--------------------------------------------------------------------------------
 50000 -55.1 -67.2  236  14  7   3.5   1.9 | -55.0 -67.0  253  15  7   3.4   1.9
 45000 -49.9 -57.8  245  18  9   3.4   1.9 | -49.7 -57.5  262  22 11   2.8   1.5
 40000 -44.5 -48.1  271  25 13   3.4   1.9 | -45.5 -49.9  268  22 11   2.8   1.5
 38000 -44.5 -48.1  274  22 11  -1.8  -1.0 | -45.7 -50.3  269  18  9  -1.9  -1.0
 36000 -45.5 -49.9  276  15  8  -1.7  -1.0 | -46.8 -52.2  270  13  7  -1.9  -1.0
 34000 -46.3 -51.3  286   8  4   0.9   0.5 | -47.5 -53.5  273   7  4   2.0   1.1
 32000 -45.9 -50.6  070  10  5   0.7   0.4 | -46.4 -51.5  081   5  3   1.9   1.0
 30000 -44.7 -48.5  077  24 12   9.0   4.9 | -44.5 -48.1  079  15  8   8.8   4.8
 29000 -42.2 -44.0  069  23 12   8.4   4.6 | -41.9 -43.4  063  16  8   8.5   4.7
 28000 -39.7 -39.5  061  22 11   8.4   4.6 | -38.7 -37.7  047  19 10   8.5   4.7
 27000 -36.5 -33.7  051  21 11   7.9   4.3 | -36.2 -33.2  037  21 11   8.3   4.6
 26000 -34.2 -29.6  046  18  9   7.7   4.2 | -33.7 -28.7  031  22 11   8.3   4.6
 25000 -31.9 -25.4  039  16  8   7.7   4.2 | -31.2 -24.2  025  22 11   8.3   4.6
 24000 -29.6 -21.3  029  14  7   7.6   4.2 | -28.8 -19.8  019  23 12   7.7   4.2
 23000 -27.4 -17.3  021  12  6   7.5   4.1 | -26.6 -15.9  013  19 10   7.3   4.0
 22000 -25.1 -13.2  010  10  5   7.5   4.1 | -24.4 -11.9  004  15  8   7.3   4.0
 21000 -22.9  -9.2  359   9  5   7.4   4.1 | -22.3  -8.1  351  13  6   7.0   3.9
 20000 -20.7  -5.3  359   9  5   7.4   4.1 | -20.2  -4.4  340  11  6   7.0   3.9
 19500 -19.6  -3.3  358   8  4   7.5   4.1 | -19.2  -2.6  333  11  5   7.0   3.9
 19000 -18.5  -1.3  358   8  4   7.5   4.1 | -18.1  -0.6  325  10  5   7.1   3.9
 18500 -17.5   0.5  357   8  4   6.7   3.7 | -17.1   1.2  318  10  5   7.0   3.9
 18000 -16.5   2.3  342   8  4   6.3   3.4 | -16.0   3.2  315  11  6   7.0   3.8
 17500 -15.6   3.9  327   8  4   6.2   3.4 | -15.0   5.0  312  11  6   7.0   3.8
 17000 -14.7   5.5  315   9  5   6.6   3.6 | -14.0   6.8  313  12  6   6.8   3.7
 16500 -13.7   7.3  306  10  5   6.6   3.6 | -13.0   8.6  317  13  7   6.9   3.8
 16000 -12.7   9.1  301  12  6   6.9   3.8 | -12.0  10.4  320  14  7   6.3   3.5
 15500 -11.7  10.9  303  13  7   7.0   3.8 | -11.1  12.0  324  14  7   6.3   3.5
 15000 -10.7  12.7  304  14  7   6.8   3.7 | -10.2  13.6  327  15  8   6.5   3.6
 14500  -9.7  14.5  309  15  8   6.7   3.6 |  -9.2  15.4  328  14  7   6.6   3.6
 14000  -8.8  16.2  314  16  8   6.6   3.6 |  -8.3  17.1  329  13  7   6.4   3.5
 13500  -7.8  18.0  316  17  9   6.6   3.6 |  -7.3  18.9  333  12  6   6.2   3.4
 13000  -6.8  19.8  316  18  9   6.6   3.6 |  -6.4  20.5  337  11  6   6.5   3.6
 12500  -5.8  21.6  314  18  9   6.9   3.8 |  -5.4  22.3  340  11  6   7.4   4.1
 12000  -4.8  23.4  311  17  9   6.9   3.8 |  -4.3  24.3  342  11  6   7.5   4.1
 11750  -4.3  24.3  309  17  9   6.9   3.8 |  -3.7  25.3  342  11  6   8.0   4.4
 11500  -3.8  25.2  307  16  8   7.0   3.8 |  -3.1  26.4  339  11  6   8.2   4.5
 11250  -3.3  26.1  305  16  8   6.9   3.8 |  -2.5  27.5  336  11  5   8.1   4.5
 11000  -2.8  27.0  303  16  8   7.1   3.9 |  -2.0  28.4  333  11  5   8.5   4.6
 10750  -2.3  27.9  303  15  8   7.8   4.3 |  -1.3  29.7  330  11  5   9.3   5.1
 10500  -1.7  28.9  306  14  7   8.2   4.5 |  -0.6  30.9  327  10  5   9.7   5.3
 10250  -0.5  31.1  313  12  6   8.5   4.7 |   0.8  33.4  322  10  5   9.7   5.3
 10000   0.1  32.2  316  11  6   9.7   5.3 |   1.6  34.9  321  10  5   9.9   5.5
  9750   0.9  33.6  318  11  6  10.1   5.5 |   2.3  36.1  321  10  5  10.0   5.5
  9500   1.6  34.9  320  11  6  10.0   5.5 |   3.1  37.6  321  10  5  10.0   5.5
  9250   2.4  36.3  323  11  6  10.0   5.5 |   3.8  38.8  321  10  5  10.1   5.5
  9000   3.1  37.6  324  11  5   9.9   5.4 |   4.6  40.3  322  10  5  10.2   5.6
  8750   3.9  39.0  325  10  5  10.0   5.5 |   5.3  41.5  323  10  5  10.2   5.6
  8500   4.6  40.3  327  10  5   9.7   5.3 |   6.1  43.0  323   9  5  10.2   5.6
  8250   5.4  41.7  328  10  5  13.7   7.5 |   7.0  44.6  325   9  5  15.0   8.2
  8000   6.7  44.1  332   9  5  21.4  11.8 |   8.4  47.1  328   8  4  23.0  12.6
  7750   8.0  46.4  337   8  4   7.5   4.1 |   9.8  49.6  333   8  4   8.7   4.8
  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

           05/20/2013 at 1500 MDT          |       05/20/2013 at 1800 MDT
                                           |
K index... +21.9                           | K index... +22.2
                                           |
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 -54.5 -66.1  262  15  8   3.6   2.0 | -54.8 -66.6  265  12  6   3.8   2.1
 45000 -49.3 -56.7  270  23 12   2.7   1.5 | -49.2 -56.6  273  18  9   2.0   1.1
 40000 -45.3 -49.5  262  23 12   2.7   1.5 | -46.2 -51.2  272  19 10   2.0   1.1
 38000 -45.7 -50.3  264  19 10  -2.7  -1.5 | -47.4 -53.3  278  14  7  -4.1  -2.2
 36000 -47.5 -53.5  272  12  6  -2.7  -1.5 | -49.8 -57.6  304   7  4  -4.1  -2.2
 34000 -48.2 -54.8  296   6  3   3.0   1.6 | -50.9 -59.6  006   6  3   6.1   3.3
 32000 -46.3 -51.3  033   4  2   3.1   1.7 | -47.2 -53.0  023   9  5   6.1   3.3
 30000 -43.6 -46.5  052  10  5   8.2   4.5 | -43.2 -45.8  022  12  6   8.3   4.6
 29000 -41.2 -42.2  038  10  5   8.3   4.6 | -40.7 -41.3  010  13  7   8.4   4.6
 28000 -38.7 -37.7  026  12  6   8.3   4.6 | -37.6 -35.7  358  15  8   8.4   4.6
 27000 -36.2 -33.2  018  14  7   8.6   4.7 | -35.1 -31.2  352  17  9   8.4   4.6
 26000 -33.6 -28.5  012  16  8   8.7   4.8 | -32.6 -26.7  351  20 10   8.4   4.6
 25000 -31.0 -23.8  007  19 10   8.7   4.8 | -30.1 -22.2  350  22 11   8.4   4.6
 24000 -28.4 -19.1  004  22 11   8.4   4.6 | -27.6 -17.7  348  24 12   7.3   4.0
 23000 -25.8 -14.4  348  18  9   6.9   3.8 | -25.5 -13.9  336  21 11   7.0   3.8
 22000 -23.7 -10.7  329  17  9   6.9   3.8 | -23.5 -10.3  321  20 10   7.0   3.8
 21000 -21.7  -7.1  315  17  9   7.3   4.0 | -21.4  -6.5  309  20 10   7.0   3.9
 20000 -19.5  -3.1  317  17  9   7.3   4.0 | -19.3  -2.7  310  21 11   7.1   3.9
 19500 -18.5  -1.3  318  17  9   7.3   4.0 | -18.3  -0.9  310  22 11   7.1   3.9
 19000 -17.4   0.7  319  18  9   7.4   4.0 | -17.2   1.0  310  23 12   7.2   3.9
 18500 -16.4   2.5  321  18 10   6.3   3.5 | -16.3   2.7  311  23 12   5.3   2.9
 18000 -15.5   4.1  325  21 11   6.2   3.4 | -15.5   4.1  316  25 13   5.0   2.8
 17500 -14.6   5.7  328  24 12   6.2   3.4 | -14.8   5.4  320  26 14   5.4   2.9
 17000 -13.7   7.3  330  26 14   6.0   3.3 | -13.9   7.0  326  28 14   6.3   3.5
 16500 -12.8   9.0  332  29 15   5.9   3.2 | -13.0   8.6  331  30 15   6.2   3.4
 16000 -11.8  10.8  332  30 16   7.1   3.9 | -12.0  10.4  333  30 16   7.1   3.9
 15500 -10.8  12.6  332  30 15   7.0   3.9 | -11.0  12.2  332  29 15   7.0   3.9
 15000  -9.8  14.4  332  30 15   6.9   3.8 |  -9.9  14.2  331  28 15   7.1   3.9
 14500  -8.8  16.2  332  29 15   6.9   3.8 |  -8.9  16.0  329  27 14   7.2   3.9
 14000  -7.8  18.0  332  28 15   6.9   3.8 |  -7.8  18.0  328  25 13   7.5   4.1
 13500  -6.8  19.8  331  25 13   7.0   3.8 |  -6.7  19.9  329  21 11   7.8   4.3
 13000  -5.8  21.6  328  22 11   7.2   3.9 |  -5.6  21.9  331  18  9   8.1   4.4
 12500  -4.7  23.5  322  18  9   7.6   4.1 |  -4.3  24.3  335  15  8   8.5   4.7
 12000  -3.6  25.5  312  14  7   7.8   4.3 |  -3.1  26.4  342  12  6   8.8   4.8
 11750  -3.0  26.6  306  13  7   8.4   4.6 |  -2.4  27.7  345  11  6   9.6   5.3
 11500  -2.4  27.7  300  12  6   8.6   4.7 |  -1.7  28.9  349  11  6   9.7   5.3
 11250  -1.8  28.8  293  11  6   8.5   4.6 |  -1.0  30.2  352  10  5   9.7   5.3
 11000  -1.2  29.8  285  10  5   8.9   4.9 |  -0.3  31.5  356  10  5   9.7   5.3
 10750  -0.5  31.1  282  10  5   9.8   5.4 |   0.4  32.7  357  10  5   9.7   5.3
 10500   0.2  32.4  281  10  5  10.0   5.5 |   1.1  34.0  358  10  5   9.8   5.4
 10250   1.0  33.8  281  10  5  10.0   5.5 |   2.6  36.7  360  10  5   9.9   5.4
 10000   1.7  35.1  281  10  5   9.9   5.4 |   3.4  38.1  360  10  5  10.1   5.6
  9750   2.4  36.3  280  10  5   9.8   5.4 |   4.1  39.4  001  10  5  10.1   5.6
  9500   3.9  39.0  279  10  5   9.8   5.4 |   4.9  40.8  002  10  5  10.2   5.6
  9250   4.6  40.3  278  10  5   9.9   5.4 |   5.6  42.1  003  10  5   9.9   5.4
  9000   5.4  41.7  277  10  5   9.9   5.5 |   6.4  43.5  003  10  5   9.7   5.3
  8750   6.1  43.0  277   9  5   9.9   5.4 |   7.1  44.8  004  10  5   9.6   5.3
  8500   6.9  44.4  276   9  5  10.0   5.5 |   7.8  46.0  004  10  5  10.0   5.5
  8250   7.7  45.9  276   9  5  14.4   7.9 |   8.6  47.5  006  10  5  13.3   7.3
  8000   9.0  48.2  274   8  4  21.3  11.7 |   9.8  49.6  010   9  5  17.5   9.6
  7750  10.3  50.5  273   7  4   9.2   5.1 |  10.9  51.6  015   8  4  10.5   5.8
  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
________________________________________________________________________________

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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