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Application of Raman and Brillouin lidar to measurement of air and water temperature profiles

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Optica Applicata, Vol. X I I I , N o. 4, 1983

Application of Raman and Brillouin lidar to

measurement of air and water

temperature profiles*

Marek Palys

Institute of Quantum Electronics, Military Technical Academy, 00-908 Warszawa-Bemowo, Poland.

In this paper we discuss the measurements of the vertical temperature profiles in the sea and in the atmosphere [1] using backscatter-frequency doubled TA G : ]M 3+ pulsed laser radiation.

Atmospherical experimental lidar system is shown in Fig. 1. Theory: The use of the ideal gas law in the form

P(h) = e (h)T(h)RIM

where: h — altitude, P — pressure, q — density, R — universal gas constant, M — molecular weight, leads to:

AP(h)/P(h) = [ A e ( h ) l e ( h ) ] + [AT(h)IT(h)].

For a fixed altitude h, where the pressure during the measurement can be usually taken as constant

A e (h)le (h) = - AT( h) IT( h) .

For constant pressure (altitude), the signal received by a lidar system measuring Eaman signal backscattered from nitrogen would indicate

ASN2(h)/SN2(h) = —AT{h)jT{h)

where SNi[h) is the backscattered Eaman signal, proportional to eNi(h). Thus, at any altitude, where the partial pressure of nitrogen is approximately constant, the Eaman backscatter gives a direct indication of temperature fluctuations

[2]. The results of experiments are shown in the Table.

Brillouin-Eaman system for monitoring vertical water temperature profiles is presented in Fig. 2.

Measurements of the temperature are to be carried out by using the Eaman effect. In the Eaman effect, unlike the Brillouin'effect, the wavelength of the

* This paper has been, presented at the European Optical Conference (EOC'83),May 30-June 4, 1983, in Rydzyna, Poland.

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422 M. Pa£YS

backscattered light is altered considerably by the interaction of the light with energy levels of the salt and water molecules. Since the population of these levels is temperature dependent, the characteristics of the Eaman spectrum

dep-Fig. 1. Block diagram of lidar system

end on the water temperature. It turns out that both the wavelength and the polarization of the Eaman light are temperature dependent. A recent study by Chang and Young has shown that if the laser light is circularly polarized, the Eaman scattered light will show depolarization which is temperature dependent. This dependence is different from that of the Brillouin effect mentioned above [3-5].

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Application o f Bam an and Brillouin Udar... 423

We have designed an important experiment to test a new method, using backscattered radiation from a laser beam to measure a temperature, Brillouin and Baman scattering all are utilized to evaluate the parameters [6].

h (km) (var T)ll2/T 8 (photon counts)

0 0 0

0.5 2.47 x 10-3 2.90 x10s 1.0 4.05 x 10~s 1.20 x10s 5.0 1.70 x lO -2 6.70 xlO3 10.0 2.90X 10-2 2.30 xlO3

To obtain the information the beam of frequency doubled YAG : Bd"1" pulse laser should be used together with a Fabry-Pérot interferometer and interference filters. The results will be checked by direct measurement.

References

[1] Co o n e t J ., Appl. Opt. 11 (1972), 2374.

[2] Hir s c h b e r g J. G. et al., NASA CR-139184, 1975. [3] Hir s c h f e l d T., Ann. Mtg. Opt. Soc. Am. 1973.

[4 ] La p p M.. Pe n n e y C. M., Go l d m a n L . M., Opt. Commun. 9 (1973), 195.

[5] Maktjhin V. N. et al., Zarubezh. Radioelektr., No. 8 (1977), 83.

[6 ] Pe t r i K ., Sa l ik A., Co o n e y J ., Appl. Opt. 21 (1982),' 1212.

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