Accumulation of cold air

Cold air accumulation is a disturbance of the fresh air supply of a built-up talc. As a result of the fluctuations in the temperature of the day, as well as different buildings and topography, alternating air currents are created between different areas. In summer, in particular, cold, heavier air from higher areas falls into built-up talkbars. This air is required to supply fresh air to the valley. The airflow often takes place in thin layers (only a few meters high).

If this airflow is interrupted by construction measures, this has an effect on the small air, resulting in a cold air jam. Typical interventions in cold-air flows are large-scale or high commercial buildings as well as dams for traffic routes. In the course of the planning such air currents must be considered. SolutionsChoose source text

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