<div class="eI0"> <div class="eI1">Model:</div> <div class="eI2"><h2><a href="http://www.meteofrance.fr/" target="_blank" target="_blank">Arpège</a>(Action de Recherche Petite Echelle Grande Echelle) from Meteo France</h2></div> </div> <div class="eI0"> <div class="eI1">Osvježeno:</div> <div class="eI2">4 times per day, from 08:00, 14:00, 20:00, and 00:00 UTC</div> </div> <div class="eI0"> <div class="eI1">Greenwich Mean Time:</div> <div class="eI2">12:00 UTC = 13:00 GMT</div> </div> <div class="eI0"> <div class="eI1">Razlučivost:</div> <div class="eI2">0.1° x 0.1° (Europe)<br> 0.5° x 0.5°</div> </div> <div class="eI0"> <div class="eI1">Parametar:</div> <div class="eI2">Isotachs 10m</div> </div> <div class="eI0"> <div class="eI1">Opis:</div> <div class="eI2"> This map shows isotachs - lines on a given surface connecting points with equal wind speed - together with isobars - the line of equal atmospheric pressure at 10m above the ground. The unit used is kph (kilometers per hour). (<a href="javascript:NeuFenster()">wind-converter</a>)<br> </div> </div> <div class="eI0"> <div class="eI1">Arpège:</div> <div class="eI2"><a href="http://www.cnrm.meteo.fr/spip.php?article121/" target="_blank">Arpège</a> <br> ARPEGE uses a set of primitive equations with a triangular spectral truncation on the horizontal, with a variable horizontal resolution, with a finite elements representation on the vertical and a “sigma-pressure†hybrid vertical coordinate. It also utilizes a temporal two time level semi-implicit semi-lagrangian scheme. The horizontal resolution of the ARPEGE model is around 7.5km over France and 37km over the Antipodes. It has 105 vertical levels, with the first level at 10m above the surface and an upper level at around 70km. Its time step is of 360 seconds.</br> </div></div> <div class="eI0"> <div class="eI1">NWP:</div> <div class="eI2">Numerical weather prediction uses current weather conditions as input into mathematical models of the atmosphere to predict the weather. Although the first efforts to accomplish this were done in the 1920s, it wasn't until the advent of the computer and computer simulation that it was feasible to do in real-time. Manipulating the huge datasets and performing the complex calculations necessary to do this on a resolution fine enough to make the results useful requires the use of some of the most powerful supercomputers in the world. A number of forecast models, both global and regional in scale, are run to help create forecasts for nations worldwide. Use of model ensemble forecasts helps to define the forecast uncertainty and extend weather forecasting farther into the future than would otherwise be possible.<br> <br>Wikipedia, Numerical weather prediction, <a href="http://en.wikipedia.org/wiki/Numerical_weather_prediction" target="_blank">http://en.wikipedia.org/wiki/Numerical_weather_prediction</a>(as of Feb. 9, 2010, 20:50 UTC).<br> </div></div> </div>