Stationary measurements are often supplemented
by mobile measurements, which can be taken from an automobile,
bicycle, or on foot. Vehicles for the combined measurement of
climate and air (Figure 4/2a) are often employed
to measure all of the usual meteorological quantities and levels
of air pollution at the same time. The disadvantage of this
approach is that such vehicles are restricted to drivable
streets or paths and thus outlying locations cannot be reached.
The duration of measurement at a location
depends, among other factors, on the response times of the
individual measurement devices. In addition, the duration of
measurement should not be too protracted, otherwise the
measurement run can last too long and the temporal variation of
the measured parameters versus the spatial parameters can become
too large. A correction for uniform time is, however, necessary
in all cases. Figure 4/2b shows the result of temperature
measurement sequences in the area of a large city park and its
surroundings in Stuttgart (KNAPP, 1998). One can recognize the
lower air temperatures in the park and its immediate vicinity. A
deep penetration of cool air is only visible where the relief
supports a cold air flow.
Location-based data can also be obtained
through remote sensing procedures (e.g. IR thermal scans) from
aircraft or satellites. Since these are usually taken at only a
few points in time (see also Chapter 5.2), their representative
accuracy must first be proven.