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Meteorological Session, Wednesday 14 June
At 13:00 Olivier Liechti, Switzerland startet with his lecture “Verification of Thermal Forecasts with Flight Data”. Post-processing of numerical weather prediction with a regional convection model provides the meteorological information that is crucial to soaring pilots: wind, lift rates,and climb altitude. Regional forecasts are presented by showing the potential flight distance for a standard class glider on a geographical map – a very intuitive form for pilots. Based on the regionalized forecasts specific glider flight tasks can be planned and optimized by applying a software tool named TopTask. The tool allows to specify the best glide ratio and the corresponding glide speed of the glider to be used - be it a paraglider or an open class sailplane. This flight planning technique for gliding has been available for national and international gliding championships such as Swiss Glide 2004 and Viking Glide 2005 . Task speeds obtained from to TopTask were compared to scored speeds for these competitions. Recorded flights were simulated with TopTask in order to compare the forecasted cloud base altitude to the flight altitude and the task speeds of the flights to the forecasts. Finally, flight plans based on different meteorological models like LME-TOPTHERM and HIRLAM were compared to the scored speeds. With the help of TopTask recorded flights can be used to tune the forecasting procedures for convective lift rates and for the depth of the convective boundary layer.This numerical thermal forecasts were used now in this WGC from many teams for their tactical decisions.



After this lecture Beda Sigrist, also from Switzerland presented his paper “Use of topographic radar scans to identify thermal hotspots in Alpine areas”.Thermals are part of the atmospheric energy flow caused by solar irradiation. The question behind this project, called TherMap, has been if variations of the solar irradiance, caused by the local topography, could be a useful predictor of thermals. Using high resolution digital data of the topography the local irradiance was therefore computed. The results, considering the different radiation angles were displayed on maps, leading to first plausible results for the morning hours of mountain areas. In a second step these models were refined to consider the thermal inertia of the soil and the air, the different vegetation factors, as well as the reflection of snow surfaces. For Alpine areas the resulting maps turned out to show a high level of agreement with superimposed flight tracks. For topographically less significant areas, like the Jura, the results were not so good. No conclusive results could be obtained for topologically still smoother landscapes, where other factors are likely to be predominant.



After coffee break Bernt Olofsson, the chief meteorologist of this WGC explained the
“Automatic Thermal Forecasts from the Swedish HIRLAM”. This thermal forecasts for glider pilots are produced automatically from the operational Numerical Weather Prediction model in Sweden and were presented during the daily morning briefing for the pilots.Bernd. Some extra algorithms are used in the postprocessing to calculate the thermal height and mean rate of climb from the forecast temperature profile in every gridpoint. The forecast is visualized in two different charts containing all necessary weather information. It is distributed via internet and is a good and cost effective tool for the pilots´ planning of their soaring activity.



“A system for planning soaring flights in northeastern Colorado USA”, presented from Prof Edward Hindman, USA, showed what is now the present situation about soaring forecasts in the United States. Currently, USA glider pilots do not have an on-line, interactive system to plan flights like their European counterparts. In Europe, a glider pilot interacts with an atmospheric numerical model to determine the most feasible flight for a given day: essentially the pilot "flies" through the predicted weather to plan a flight. This interaction is accomplished through the TopTask algorithm nested in the on-line pilot briefing system called pc_met of the German Weather Service. As a first step in the USA, the Regional Atmospheric Modeling System (RAMS) at the Colorado State University has been coupled to the A & K TopTask Competition (TTC) algorithm. The coupling was accomplished following the Olofsson and Olsson lift-rate procedures. The RAMS-TTC system was tested using 35 Colorado Soaring Association On-line Contest flights. The flights occurred over 15 days in 2004 and 2005 from Owl Canyon Gliderport (OCGP), Wellington CO. On average, the RAMS-TTC system predicted a potential flight distance of 747 km while the actual flight distance was 289 km. The average predicted task speed was 119 kph while the average actual speed was 104 kph. The average thermal top was predicted to be 4600 m MSL while average achieved top was 4400 m MSL. These results demonstrate the significant soaring conditions in northeast Colorado. Closer predicted and actual task speeds are expected from the RAMS-TTC system using results from a competition, as has been shown for Viking Glide 2005 by Liechti using the TTC system in pc-met. Two competitions are planned for OCGP, one in April 2006 and the other in May 2006. These RAMS-TTC results from these competitions were presented.



The last paper “Convergences Mammatus”“ was given by Carsten Lindeman, Germany, who travelled with a motorglider from Berlin to Ekeby. Cloudstreets have been observed by satellite quite often. Radiosoundings are evaluated for wind and temperature profiles for these occasions. A first conclusion is that cloud streets must form at a curved profile of Kuettners theory, but can form with increasing wind velocity with hight also. Secondly convergence lines over the central mountains of Spain are detected, which sometimes can extend into the plain.
Another interesting phenomena “mammatus clouds” were observed and touched during a gliding flight over the Andes.



Hermann Trimmel

Chairman


 
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Meteorological Session, Wednesday 14 June
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Morning, afternoon and... evening shift!
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Evening Shift!
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Evening Shift !
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''Early mornings ''
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Evening shift!
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June 3 2006
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Saturday June 3 2006
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Evening shift!
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Great practise day!
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''A different world''
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''Do you believe it ?''
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Warm welcome in Sweden