Advances in Optical and Photonic Devices 2010
DOI: 10.5772/7142
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Tunable, Narrow Linewidth, High Repetition Frequency Ce:LiCAF Lasers Pumped by the Fourth Harmonic of a Diode-Pumped Nd:YLF Laser for Ozone DIAL Measurements

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“…The structureless nature of the absorption spectrum of ozone in this region allows for a minimum spacing of 2 nm between on and off resonant wavelengths (Milton et al, 1998) for accurate profiling of ozone throughout the free troposphere. Although the wavelengths used with this instrument are spaced further apart (10 nm), they have the advantage of being generated very reliably as opposed to previously used dye laser (Pelon and Mégie, 1982;Browell, 1983;Megie et al, 1985;Kuang et al, 2011), excimer laser (Uchino et al, 1983;de Schoulepnikoff et al, 1997;Veselovskii and Barchunov, 1999), and tunable laser cavity (Fix et al, 2002;Fromzel et al, 2010;Senff et al, 2010) systems. Figure 1, adapted from Malicet et al (1995), illustrates the ozone absorption cross section (σ O 3 ) and the TROPOZ wavelengths that were generated for the 3532 J. T. Sullivan: Tropospheric Ozone DIAL in the Baltimore-Washington, D.C. region large gradient in ozone absorption ( σ O 3 ), which will yield usable atmospheric information.…”
Section: The Differential Absorption Lidar (Dial) Methodsmentioning
confidence: 99%
“…The structureless nature of the absorption spectrum of ozone in this region allows for a minimum spacing of 2 nm between on and off resonant wavelengths (Milton et al, 1998) for accurate profiling of ozone throughout the free troposphere. Although the wavelengths used with this instrument are spaced further apart (10 nm), they have the advantage of being generated very reliably as opposed to previously used dye laser (Pelon and Mégie, 1982;Browell, 1983;Megie et al, 1985;Kuang et al, 2011), excimer laser (Uchino et al, 1983;de Schoulepnikoff et al, 1997;Veselovskii and Barchunov, 1999), and tunable laser cavity (Fix et al, 2002;Fromzel et al, 2010;Senff et al, 2010) systems. Figure 1, adapted from Malicet et al (1995), illustrates the ozone absorption cross section (σ O 3 ) and the TROPOZ wavelengths that were generated for the 3532 J. T. Sullivan: Tropospheric Ozone DIAL in the Baltimore-Washington, D.C. region large gradient in ozone absorption ( σ O 3 ), which will yield usable atmospheric information.…”
Section: The Differential Absorption Lidar (Dial) Methodsmentioning
confidence: 99%