VDI 3786 BLATT 18
Environmental meteorology - Ground-based remote sensing of temperature - Radio-acoustic sounding systems (RASS)
| Organization: | VDI |
| Publication Date: | 1 May 2010 |
| Status: | active |
| Page Count: | 64 |
| ICS Code (Air quality in general): | 13.040.01 |
| ICS Code (Geology. Meteorology. Hydrology): | 07.060 |
scope:
RASS systems have successfully been used for many years for the remote determination of vertical temperature profiles. They complement conventional instrumentation as they lend themselves to a large number of measurement tasks that cannot be fulfilled adequately with in-situ or point measurement devices or for which masts or towers are not suitable for technical, administrative or economical reasons.
The use of RASS systems is particularly advantageous for
• measurement of temperature in atmospheric layers up to several kilometers height
• determination of the thermal stability of the atmosphere
• pursuit of the development and decay of convective boundary layers (height of the mixing layer)
• determination of the height and structure of stable boundary layers
• determination of the altitude and strength of detached inversions
• measurement of turbulent flows in the atmospheric boundary layer
• measurement of wind profiles in noisy areas or in sites with potentially large radar echoes where the use of sodar and radar systems is restricted
• measurements in heavy weather conditions
The following applications are particularly important:
• routine temperature profiling from aerological stations
• production of data for the use in numerical dispersion models, e. g., in connection with licensing procedures under BImSchG, 9. BImSchV and TA Luft: time series calculation (TA Luft, Annex 3 Clause 1), Monin-Obukhov length (TA Luft, Annex 3 Clause 8. 4), height of the mixing layer (TA Luft, Annex 3 Clause 8.5)
• production of data for site approval certificates for ambient air quality control and environmental compatibility assessment
• flight safety and aviation weather services including the quantitative determination even of extreme ground inversions
• plant monitoring during regular and irregular operations
• investigation of the atmospheric boundary layer
• replacement and complementation of investigations made with meteorological towers, tether balloons and aircrafts
Section 8 gives some examples of applications of RASS in these fields.
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