Geoscience Reference
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Fig. 2.18 Spectral
characteristics of peat
emissivity coef cient under
weighed humidity: 1 45 %;
2 54 %; 3 67 %; 4 78 %
Fig. 2.19 Spectral
characteristics of absorption
coefficient for peat under
weighed humidity: 1
40 %;
2
53 %; 3
63 %; 4
70 %;
5
73 %
Figure 2.22 shows the stability of averaged maximal variations of radio-
brightness temperatures registered in different directions of
flying laboratory traces.
Total error of radio-brightness contrasts is near to 2 K. Results given here show that
microwave radiometers allow the detection of
fl
fire in its beginning with high
probability.
Another important area for the application of microwave radiometry is remote
control of geothermal sources. Microwave monitoring facilitates analyzing the
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