National Weather Service United States Department of Commerce

Soaring Forecast for Moriarty NM
National Weather Service Albuquerque NM
1510 MST Tuesday February 4 2025

This forecast is for Tuesday, February 4, 2025:

If the trigger temperature of 69.5 F/20.9 C is reached...then
   Thermal Soaring Index....................... Fair
   Maximum rate of lift........................ 342 ft/min (1.7 m/s)
   Maximum height of thermals.................. 10659 ft MSL (4329 ft AGL)

Forecast maximum temperature................... 70.0 F/21.6 C
Time of trigger temperature.................... 1345 MST
Time of overdevelopment........................ None
Middle/high clouds during soaring window....... None
Surface winds during soaring window............ 20 mph or less
Height of the -3 thermal index................. 8212 ft MSL (1882 ft AGL)
Thermal soaring outlook for Wednesday 02/05.... Good


Remarks... 

Sunrise/Sunset.................... 06:59:52 / 17:36:04 MST
Total possible sunshine........... 10 hr 36 min 11 sec (636 min 11 sec)
Altitude of sun at 12:17:58 MST... 38.87 degrees

Upper air data from numerical model forecast valid on 02/04/2025 at 0500 MST

Freezing level.................. 14178 ft MSL (7848 ft AGL)
Convective condensation level... 21978 ft MSL (15648 ft AGL)
Lifted condensation level....... 19120 ft MSL (12790 ft AGL)
Lifted index.................... +5.2
K index......................... -2.8

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  -65.1 -85.2   280   43   22   4.5   2.5   81.9 179.5    35.6      M    M
 45000  -58.8 -73.8   280   55   28   2.5   1.4   69.6 157.2    30.3      M    M
 40000  -54.9 -66.8   260   56   29   2.6   1.4   52.4 126.3    21.0      M    M
 38000  -53.2 -63.8   250   55   29   2.9   1.6   45.8 114.5    17.0      M    M
 36000  -51.4 -60.5   245   55   28   2.9   1.6   40.1 104.2    13.4      M    M
 34000  -47.9 -54.2   240   55   28   8.3   4.6   36.9  98.5    11.5      M    M
 32000  -42.9 -45.2   240   53   27   8.3   4.6   35.8  96.5    10.9      M    M
 30000  -37.3 -35.1   240   50   26   8.3   4.5   34.5  94.2    10.3      M    M
 29000  -34.9 -30.8   240   49   25   8.3   4.5   34.0  93.2    10.0      M    M
 28000  -32.4 -26.3   235   47   24   8.3   4.6   33.5  92.4     9.7      M    M
 27000  -30.0 -22.0   235   46   24   7.8   4.3   32.8  91.0     9.3      M    M
 26000  -27.7 -17.9   235   45   23   7.8   4.3   32.0  89.7     8.8      M    M
 25000  -25.3 -13.5   235   45   23   7.8   4.3   31.4  88.5     8.3      M    M
 24000  -23.0  -9.4   240   44   23   7.8   4.3   30.7  87.3     7.8      M    M
 23000  -20.7  -5.3   240   43   22   7.8   4.3   30.0  85.9     7.3      M    M
 22000  -18.4  -1.1   240   42   22   7.8   4.3   29.3  84.8     6.8      M    M
 21000  -16.1   3.0   240   41   21   7.6   4.2   28.6  83.5     6.3      M    M
 20000  -13.8   7.2   235   39   20   7.6   4.2   27.8  82.1     5.7      M    M
 19500  -12.7   9.1   235   38   20   7.6   4.2   27.5  81.5     5.4      M    M
 19000  -11.5  11.3   230   38   19   7.6   4.2   27.2  80.9     5.1      M    M
 18500  -10.4  13.3   230   36   19   7.5   4.1   26.8  80.2     4.8      M    M
 18000   -9.3  15.3   230   35   18   7.5   4.1   26.4  79.5     4.5      M    M
 17500   -8.2  17.2   230   33   17   7.6   4.2   26.0  78.9     4.2      M    M
 17000   -6.5  20.3   230   32   16   7.6   4.2   25.5  77.9     3.7      M    M
 16500   -5.4  22.3   230   31   16   8.0   4.4   25.2  77.3     3.4      M    M
 16000   -4.2  24.4   230   30   16   7.9   4.3   24.9  76.8     3.2      M    M
 15500   -3.0  26.6   230   30   15   8.0   4.4   24.6  76.2     2.9      M    M
 15000   -1.8  28.8   230   30   15   8.1   4.4   24.3  75.7     2.7      M    M
 14500   -0.6  30.9   230   29   15   7.9   4.4   24.0  75.3     2.4      M    M
 14000    0.6  33.1   230   29   15   7.7   4.2   23.7  74.7     2.1      M    M
 13500    1.7  35.1   230   28   15   7.7   4.2   23.4  74.1     1.8      M    M
 13000    2.9  37.2   230   28   14   7.6   4.2   23.0  73.4     1.5      M    M
 12500    4.0  39.2   230   27   14   7.6   4.2   22.7  72.9     1.3      M    M
 12000    5.2  41.4   230   25   13   7.6   4.2   22.4  72.3     1.0      M    M
 11500    6.3  43.3   230   24   12   7.0   3.9   22.0  71.7     0.7      M    M
 11000    7.4  45.3   230   22   11   7.4   4.1   21.6  70.9     0.3      M    M
 10500    8.5  47.3   230   20   11   7.3   4.0   21.2  70.2    -0.1    327  1.7
 10250    9.0  48.2   230   20   10   7.2   4.0   21.0  69.8    -0.3    303  1.5
 10000    9.5  49.1   230   19   10   7.0   3.8   20.8  69.5    -0.5    280  1.4
  9750   10.0  50.0   230   18    9   6.9   3.8   20.6  69.1    -0.7    257  1.3
  9500   10.5  50.9   230   17    9   7.0   3.8   20.4  68.7    -1.0    235  1.2
  9250   11.0  51.8   230   17    9   6.5   3.6   20.1  68.3    -1.2    213  1.1
  9000   11.4  52.5   230   16    8   5.3   2.9   19.9  67.7    -1.5    193  1.0
  8750   11.8  53.2   230   16    8   4.8   2.7   19.5  67.1    -1.9    175  0.9
  8500   12.1  53.8   230   15    8   4.5   2.5   19.1  66.4    -2.3    158  0.8
  8250   12.4  54.3   230   15    8   2.7   1.5   18.6  65.6    -2.8    143  0.7
  8000   12.5  54.5   230   14    7   1.5   0.8   18.0  64.5    -3.4    133  0.7
  7750   12.5  54.5   235   13    7   1.8   1.0   17.4  63.4    -4.1    123  0.6
  7500   12.6  54.7   235   12    6  -0.7  -0.4   16.8  62.2    -4.8    115  0.6
  7250   12.3  54.1   235   10    5  -4.1  -2.3   15.8  60.5    -5.8    114  0.6
  7000   12.0  53.6   230    8    4  -4.4  -2.4   14.7  58.5    -6.9    118  0.6
  6750   11.6  52.9   230    6    3  -5.6  -3.1   13.7  56.6    -8.0    122  0.6
  6500   10.6  51.1   215    4    2 -24.4 -13.4   12.0  53.6    -9.7    144  0.7
  6250      M     M     M    M    M     M     M      M     M       M      M    M

 * * * * * * Numerical weather prediction model forecast data valid * * * * * * 

           02/04/2025 at 0800 MST          |       02/04/2025 at 1100 MST        
                                           |
CAPE...     0.0    LI...       +5.2        | CAPE...     0.0    LI...       +4.8
CINH...     0.0    K Index...  +1.0        | CINH...     0.0    K Index...  -6.1
                                           |
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 -65.8 -86.4  285  49 25   4.4   2.4 | -65.5 -85.9  280  47 24   3.8   2.1
 45000 -59.0 -74.2  280  59 30   3.9   2.1 | -58.9 -74.0  275  57 29   5.7   3.1
 40000 -53.2 -63.8  265  58 30   3.4   1.9 | -50.4 -58.7  280  62 32   3.9   2.1
 38000 -52.0 -61.6  255  55 28   2.0   1.1 | -50.4 -58.7  260  57 30  -0.2  -0.1
 36000 -50.8 -59.4  240  54 28   2.0   1.1 | -50.5 -58.9  245  58 30  -0.2  -0.1
 34000 -47.8 -54.0  235  54 28   7.6   4.2 | -48.1 -54.6  235  60 31   7.9   4.3
 32000 -42.7 -44.9  240  53 27   7.6   4.2 | -42.8 -45.0  235  58 30   8.0   4.4
 30000 -37.7 -35.9  240  50 26   8.5   4.7 | -38.1 -36.6  240  53 27   7.6   4.2
 29000 -35.2 -31.4  240  48 25   8.5   4.7 | -35.8 -32.4  235  49 25   7.6   4.2
 28000 -32.6 -26.7  235  46 23   8.6   4.7 | -33.6 -28.5  235  45 23   7.5   4.1
 27000 -30.2 -22.4  235  44 23   7.9   4.4 | -31.0 -23.8  235  43 22   8.7   4.8
 26000 -27.8 -18.0  235  43 22   8.0   4.4 | -28.4 -19.1  235  41 21   8.7   4.8
 25000 -25.5 -13.9  235  41 21   8.0   4.4 | -25.8 -14.4  235  40 21   8.7   4.8
 24000 -23.1  -9.6  235  41 21   7.8   4.3 | -23.4 -10.1  235  40 20   7.7   4.2
 23000 -20.8  -5.4  230  41 21   7.8   4.3 | -21.1  -6.0  235  40 21   7.7   4.2
 22000 -18.4  -1.1  230  41 21   7.8   4.3 | -18.8  -1.8  230  41 21   7.7   4.2
 21000 -16.1   3.0  230  41 21   8.2   4.5 | -16.5   2.3  230  41 21   7.8   4.3
 20000 -13.6   7.5  230  41 21   8.2   4.5 | -14.1   6.6  230  41 21   7.8   4.3
 19500 -12.4   9.7  230  41 21   8.2   4.5 | -13.0   8.6  230  42 21   7.8   4.3
 19000 -11.2  11.8  230  41 21   8.0   4.4 | -11.8  10.8  230  42 21   7.9   4.3
 18500 -10.0  14.0  230  41 21   7.8   4.3 | -10.6  12.9  235  42 21   8.0   4.4
 18000  -8.3  17.1  230  40 21   7.7   4.2 |  -8.8  16.2  235  41 21   7.9   4.4
 17500  -7.2  19.0  230  39 20   7.5   4.1 |  -7.6  18.3  235  41 21   7.8   4.3
 17000  -6.0  21.2  230  38 20   7.6   4.2 |  -6.4  20.5  235  41 21   7.8   4.3
 16500  -5.0  23.0  230  37 19   6.8   3.7 |  -5.3  22.5  235  40 21   7.5   4.1
 16000  -3.9  25.0  230  35 18   6.9   3.8 |  -4.1  24.6  235  39 20   7.5   4.1
 15500  -2.9  26.8  230  33 17   6.7   3.7 |  -3.0  26.6  235  39 20   7.1   3.9
 15000  -1.9  28.6  230  31 16   6.6   3.6 |  -2.0  28.4  235  37 19   6.9   3.8
 14500  -1.0  30.2  230  29 15   6.5   3.6 |  -0.9  30.4  230  36 19   6.6   3.6
 14000  -0.0  32.0  230  28 14   6.3   3.5 |  -0.0  32.0  230  34 18   6.2   3.4
 13500   0.9  33.6  230  26 13   6.3   3.5 |   0.9  33.6  230  32 17   6.1   3.4
 13000   1.8  35.2  235  25 13   6.3   3.5 |   1.7  35.1  230  30 15   5.8   3.2
 12500   2.7  36.9  235  24 12   6.3   3.5 |   2.6  36.7  230  28 14   5.9   3.2
 12000   3.7  38.7  240  23 12   7.0   3.9 |   3.4  38.1  230  26 13   6.6   3.6
 11500   4.7  40.5  245  23 12   6.6   3.6 |   4.3  39.7  230  23 12   6.3   3.4
 11000   5.8  42.4  245  22 11   8.2   4.5 |   5.3  41.5  235  21 11   7.6   4.2
 10500   7.0  44.6  245  22 11   8.1   4.4 |   6.4  43.5  240  19 10   7.4   4.1
 10250   7.6  45.7  245  21 11   7.9   4.3 |   6.9  44.4  240  19 10   7.3   4.0
 10000   8.2  46.8  245  21 11   8.1   4.4 |   7.5  45.5  240  18  9   7.7   4.2
  9750   8.8  47.8  245  20 10   8.4   4.6 |   8.1  46.6  240  17  9   8.1   4.4
  9500   9.4  48.9  245  19 10   8.2   4.5 |   8.7  47.7  240  16  8   7.9   4.3
  9250  10.0  50.0  245  18  9   8.2   4.5 |   9.3  48.7  245  15  8   8.5   4.6
  9000  10.6  51.1  245  17  9   6.6   3.6 |   9.9  49.8  240  14  7   7.1   3.9
  8750  11.0  51.8  245  16  8   5.1   2.8 |  10.3  50.5  240  13  7   5.6   3.1
  8500  11.4  52.5  245  14  7   4.5   2.5 |  10.8  51.4  240  13  6   4.8   2.6
  8250  11.6  52.9  245  13  7   2.1   1.1 |  11.0  51.8  240  11  6   2.2   1.2
  8000  11.7  53.1  245  12  6   0.7   0.4 |  11.1  52.0  240  10  5   1.7   0.9
  7750  11.7  53.1  245  11  6   0.1   0.0 |  11.2  52.2  235   8  4   0.9   0.5
  7500  11.6  52.9  245   9  5  -1.7  -0.9 |  11.3  52.3  235   7  3   5.0   2.8
  7250  11.4  52.5  250   8  4  -3.2  -1.8 |  11.9  53.4  235   6  3  10.1   5.6
  7000  11.1  52.0  250   6  3  -2.7  -1.5 |  12.6  54.7  230   5  3   9.5   5.2
  6750  10.9  51.6  255   4  2  -5.0  -2.7 |  13.4  56.1  230   5  3  10.1   5.5
  6500  10.1  50.2  255   1  1 -17.4  -9.5 |  14.2  57.6  225   4  2  12.6   6.9
  6250     M     M    M   M  M     M     M |     M     M    M   M  M     M     M

           02/04/2025 at 1400 MST          |       02/04/2025 at 1700 MST        
                                           |
CAPE...     0.0    LI...       +4.3        | CAPE...     0.0    LI...       +5.0
CINH...    -0.3    K Index... -13.0        | CINH...    -0.4    K Index...  -3.5
                                           |
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 -66.2 -87.2  275  50 26   4.8   2.6 | -65.8 -86.4  290  47 24   5.5   3.0
 45000 -58.5 -73.3  275  61 31   5.4   2.9 | -57.6 -71.7  290  66 34   5.1   2.8
 40000 -50.4 -58.7  275  66 34   4.7   2.6 | -50.0 -58.0  285  76 39   4.9   2.7
 38000 -48.5 -55.3  270  64 33   3.1   1.7 | -47.3 -53.1  275  69 36   4.4   2.4
 36000 -46.7 -52.1  260  62 32   3.1   1.7 | -44.6 -48.3  270  63 32   4.4   2.4
 34000 -44.7 -48.5  250  62 32   3.4   1.9 | -42.7 -44.9  260  57 30   1.6   0.9
 32000 -42.4 -44.3  240  62 32   3.4   1.9 | -41.8 -43.2  245  55 29   1.6   0.9
 30000 -38.7 -37.7  235  59 30   8.3   4.6 | -38.6 -37.5  240  55 28   8.3   4.6
 29000 -36.2 -33.2  240  55 28   8.4   4.6 | -36.1 -33.0  235  54 28   8.3   4.6
 28000 -33.7 -28.7  240  52 27   8.4   4.6 | -33.6 -28.5  235  54 28   8.4   4.6
 27000 -31.2 -24.2  240  49 25   8.3   4.6 | -31.1 -24.0  235  53 27   8.2   4.5
 26000 -28.7 -19.7  235  48 25   8.3   4.6 | -28.6 -19.5  235  51 26   8.2   4.5
 25000 -26.2 -15.2  235  46 24   8.3   4.6 | -26.2 -15.2  235  49 25   8.2   4.5
 24000 -23.8 -10.8  230  45 23   7.5   4.1 | -23.7 -10.7  235  48 25   7.7   4.2
 23000 -21.6  -6.9  230  46 23   7.5   4.1 | -21.4  -6.5  235  48 25   7.7   4.2
 22000 -19.4  -2.9  230  46 24   7.5   4.1 | -19.1  -2.4  235  48 25   7.7   4.2
 21000 -17.1   1.2  230  46 24   7.8   4.3 | -16.8   1.8  235  49 25   7.7   4.2
 20000 -14.7   5.5  230  45 23   7.8   4.3 | -14.5   5.9  235  50 26   7.7   4.2
 19500 -13.6   7.5  230  45 23   7.8   4.3 | -13.4   7.9  235  51 26   7.7   4.2
 19000 -12.4   9.7  235  45 23   7.9   4.3 | -11.7  10.9  235  52 27   8.0   4.4
 18500 -11.2  11.8  235  45 23   8.3   4.6 | -10.4  13.3  240  52 27   8.1   4.4
 18000  -9.3  15.3  235  44 23   8.2   4.5 |  -9.2  15.4  240  52 27   8.1   4.4
 17500  -8.1  17.4  235  44 23   8.0   4.4 |  -8.1  17.4  240  52 27   7.7   4.2
 17000  -6.9  19.6  235  43 22   8.0   4.4 |  -6.9  19.6  240  51 26   7.8   4.3
 16500  -5.7  21.7  235  43 22   7.8   4.3 |  -5.8  21.6  245  50 26   6.5   3.6
 16000  -4.5  23.9  235  42 22   7.8   4.3 |  -4.9  23.2  245  48 25   6.2   3.4
 15500  -3.3  26.1  235  41 21   7.7   4.2 |  -4.0  24.8  245  46 24   5.6   3.1
 15000  -2.2  28.0  235  40 20   7.5   4.1 |  -3.3  26.1  245  43 22   4.8   2.6
 14500  -1.0  30.2  240  39 20   7.2   4.0 |  -2.6  27.3  245  40 21   5.0   2.7
 14000  -0.0  32.0  240  37 19   6.3   3.5 |  -1.7  28.9  245  38 20   7.1   3.9
 13500   0.9  33.6  240  35 18   6.4   3.5 |  -0.7  30.7  240  36 19   6.9   3.8
 13000   1.7  35.1  240  32 17   5.0   2.7 |   0.4  32.7  240  34 18   8.1   4.5
 12500   2.5  36.5  240  29 15   5.3   2.9 |   1.6  34.9  240  32 17   8.0   4.4
 12000   3.2  37.8  240  26 13   6.0   3.3 |   2.8  37.0  235  31 16   8.2   4.5
 11500   4.1  39.4  235  23 12   6.3   3.4 |   4.0  39.2  235  28 15   8.0   4.4
 11000   5.1  41.2  235  21 11   8.7   4.8 |   5.1  41.2  230  26 13   7.7   4.2
 10500   6.4  43.5  230  19 10   8.5   4.7 |   6.3  43.3  230  23 12   7.8   4.3
 10250   7.0  44.6  230  19 10   8.8   4.8 |   6.8  44.2  225  22 11   8.2   4.5
 10000   7.7  45.9  230  18  9   9.4   5.1 |   7.5  45.5  225  21 11   8.7   4.8
  9750   8.4  47.1  230  18  9   9.6   5.2 |   8.1  46.6  225  20 11   8.9   4.9
  9500   9.1  48.4  230  18  9   9.2   5.0 |   8.8  47.8  220  20 10   8.5   4.6
  9250   9.8  49.6  230  18  9  10.7   5.9 |   9.4  48.9  220  19 10   9.9   5.4
  9000  10.6  51.1  230  17  9  10.4   5.7 |  10.2  50.4  220  18  9  10.0   5.5
  8750  11.3  52.3  230  17  9   8.7   4.8 |  10.9  51.6  220  18  9   8.7   4.8
  8500  12.0  53.6  230  17  9   9.1   5.0 |  11.6  52.9  220  17  9   9.0   4.9
  8250  12.7  54.9  230  17  9   9.7   5.3 |  12.2  54.0  220  17  9   9.2   5.0
  8000  13.4  56.1  230  17  9  10.1   5.5 |  12.9  55.2  220  16  8   9.4   5.2
  7750  14.2  57.6  230  17  9   9.8   5.4 |  13.6  56.5  220  16  8   9.4   5.2
  7500  14.9  58.8  230  17  9   9.8   5.4 |  14.3  57.7  220  15  8   9.1   5.0
  7250  15.6  60.1  230  16  8   9.9   5.4 |  15.0  59.0  220  14  7   8.2   4.5
  7000  16.4  61.5  230  16  8  10.1   5.5 |  15.6  60.1  220  13  7   7.6   4.2
  6750  17.1  62.8  225  16  8   9.5   5.2 |  16.1  61.0  220  12  6   8.6   4.7
  6500  17.9  64.2  225  15  8  12.1   6.7 |  16.7  62.1  220  10  5   3.7   2.0
  6250     M     M    M   M  M     M     M |     M     M    M   M  M     M     M
________________________________________________________________________________

This product is issued once per day, at approximately 730 AM local 
time. It is not continuously monitored nor updated after its initial 
issuance. 

The information contained herein is based on numerical weather prediction
model data for the Moriarty Municipal Airport site in Moriarty, New Mexico at

                   North Latitude:  34.9781667 deg
                   West Longitude: 106.0000278 deg
                   Elevation: 6204.2 feet (1891.0 meters)

and may not be representative of other areas along and east of the Sandia
and Manzano 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 are welcome and should be directed
to one of the addresses or phone numbers shown at the bottom of this page.

DEFINITIONS:

CAPE (Convective Available Potential Energy) - An integrated measure of the
     energy available for convective development, also known as the positive 
     area on a thermodynamic diagram.  Units are Joules per kilogram.  Larger
     values are indicative of greater instability and the possibility of 
     stronger convective activity, including thunderstorms.  Values around or
     greater than 1000 suggest the possibility of severe weather should
     convective activity develop.

CINH (Convective Inhibition) - An integrated measure of the amount of energy
     needed to initiate convective activity, also known as the negative area on
     a thermodynamic diagram.  Units are Joules per kilogram.  The more negative
     this number, the more energy is required to initiate convection.  This
     inhibitive energy can be overcome through surface heating, cooling aloft,
     lifting mechanisms (orographic, frontal, gravity waves, etc.)

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 (LI) - 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, cirrostratus, 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.

042613