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June 4, 2007 The creation of rain is the result of a variety of physical processes. These processes influence each other and play out both at an extremely small scale (several micrometers) and on a very large one (100 kilometers). The spatial scale of weather models is a few kilometers, and physical processes which occur at a smaller scale have to be approximated. Cloud formation is an example of this. The complexity and differences in scale make weather modeling inaccurate in predicting the time and place of a downpour, and the quantity of rain which will ultimately fall. The TU Delft On June 4, TU Delft moved the TARA (Transportable Atmospheric RAdar) atmosphere radar to The TU Delft will also have access to two research aircraft (one French, the other German) which will fly through the clouds to measure their physical properties. These aircraft have been specially assigned to two Delft PhD candidates. Within this international Convective and Orographically-induced Precipitation Study (COPS), TU Delft will be mainly concerned with the question as to how cloud and rain formation is influenced by dust particles in the atmosphere. The influence of the aerosol-cloud interaction on the earth’s radiation balance is also one of the greatest unknowns in climate models. The data collected during COPS will be suitable for improving models describing the relationship between atmospheric dynamics and cloud formation. Schedule - TARA will be transported to
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