Astroclimatology |
The method is based on combining satellite current image in the 6.7 and 10.7 microm. channel with wind and temperature profiles forecasted by a prediction center.
Measured |
Ground | Satellite |
Forecast | RMS | MAE | ME | RMS | MAE | ME |
Period 1 | 0.68 | 0.53 | -0.41 | 0.71 | 0.58 | -0.46 |
Period 2 | 1.14 | 0.99 | 0.29 | 0.90 | 0.76 | 0.12 |
Period 3 | 1.06 | 0.78 | 0.31 | 0.92 | 0.69 | -0.13 |
Period 4 | 0.93 | 0.82 | -0.15 | 0.48 | 0.38 | -0.06 |
Summer Periods | 1.11 | 0.92 | 0.3 | 0.91 | 0.73 | 0.04 |
Winter Periods | 0.77 | 0.63 | -0.32 | 0.63 | 0.5 | -0.31 |
All Periods | 1.01 | 0.82 | 0.08 | 0.84 | 0.72 | -0.06 |
Root mean square error (RMS), mean absolute error (MAE) and mean error (ME - measured minus forecasted) between forecasted and measured (by ground monitor and satellite respectively) PWV (mm) at Paranal using the final version (2.5) of the forecasting programme.
In addition, a comparison between the Antofagasta Radiosonde, 6.7 µm Satellite and Paranal Ground monitor measurements of precipitable water vapor (PWV) was also conducted. This comparison showed that there is good agreement between these three different measurement methods.
Some synoptic information on water vapor circulation over the southern Pacific can be found on the H2O flow chart, Demo movies of 24-hour forecast message issued on Nov. 29 1993 at 15h UT for subsequent 3-hourly bins (170kB mpeg), 24-hour of input images on June 14-15, 1993 (480kB mpeg), and 2 weeks of input images on June 14-29, 1993 (4mB mpeg).