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1.Climate as a Public Interest in Planning and Zoning
2.Characteristics and Forms of the Urban Climate
3.Energy-Conscious Planning and Zoning
4.Methods of Information Acquisition for Planning (Measurements, Wind Tunnels, Numerical Modelling)
4.1Measurements
4.1.1Stationary Measurements
4.1.2Measurements with mobile measurement devices
4.1.3Tracer Experiments
4.1.4Vertical Soundings
4.2Wind Tunnel
4.2.1Overview
4.2.2Operation and Investigation Methods
4.2.2.1Visualization of flows and pollutant dispersion by smoke
4.2.2.2Wind Velocity Measurements
4.2.2.3Measurement of Concentration Distribution in Dispersal Experiments
4.2.3Locations of Wind Tunnels
4.3Numerical Modelling of Flow and Transport Processes
4.3.1The Wind Field Model DIWIMO
4.3.2The Cold-Air Flow Model KALM and KLAM 21
4.3.3The Model STREET for Estimating Traffic-Produced Pollution
4.3.4The Model MLuS-02 for Calculating Pollutant Dispersal
on Roads Without Dense Peripheral Development
4.3.5The Model PROKAS for Calculating Air Pollution on Roads
4.3.6The Micro-Scale Model MISKAM
4.3.7Mesoscale Terrain Climatic Models
4.3.8The Urban Climate Models RayMan , ENVI-met and MUKLIMO_3
5.Climatic and Air Hygiene Maps as Aids for Planning and Zoning (Example: Climate Atlas Federation Region Stuttgart)
6.Recommendations for Planning
7.Bibliography
8.Thematic Websites
Imprint
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METHODS OF INFORMATION ACQUISITION FOR PLANNING (MEASUREMENTS, WIND TUNNELS, NUMERICAL MODELLING)
   
 4.1.3 Tracer Experiments

In order to measure air movements and air transport routes, it is possible to enrich the air with a tracer and follow and measure its motion. The simplest method uses smoke canisters. The smoke, typically colored, mixes with the flowing air and is transported so that e.g. it can be photographically documented and evaluated. Smoke canisters are usually employed to mark cold air flows, since these move relatively slowly and exhibit only minor vertical mixing. Figure 4/5 and Figure 4/5a illustrates the visualisation of a cold-air flow through a smoke bomb.

A more elaborate method includes the use of tracer gases, like sulphur hexafluoride (SF6). The tracer is here released at a selected point and its concentration is then determined at many other points along the presumed flow route (Figure 4/6) by taking air samples at regular time intervals. The concentration of the samples is later determined in a laboratory. Tracer gases should be anthropogenic, chemically stable (inert), non-poisonous and identifiable with standard methods.

 
 
 
Fig. 4/5: Cold air flow, marked by artificial smoke, Source: KUTTLER u. DÜTEMEYER, 2003
 
Fig. 4/5a: Cold air flow, marked by artificial smoke
 
Fig. 4/6: The distribution of the tracer gas SF6 as an average over the total duration of measurement (ppb) during the night of 9-10 August 1996 for determining the cold air flow in Stuttgart; red line: cold air trajectory calculated with KALM (s. a. Chapter 4.3.2) (BAUMBACH et al., 1999)