2007
DOI: 10.1002/qj.160
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Characterization of the variability of the humidity and cloud fields as observed from a cluster of ground-based lidar systems

Abstract: Three lidar stations located in Southern Italy were operational during the Italian phase of the EAQUATE campaign in September 2004. With this cluster of instruments, the characterization of water vapour and clouds distribution and evolution with high temporal and vertical resolution is possible. A cirrus cloud episode and the presence of an elevated humid layer in the free troposphere observed at all three stations are analysed in detail. Variability of both cirrus cloud and water vapour fields is studied on d… Show more

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Cited by 22 publications
(17 citation statements)
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“…The means and standard deviations amount to 15.2 ± 0.4 and 12.4 ± 0.6 g kg −1 before and after the major rearrangement in the optical setup on 15 April 2013, 10:06 UTC, respectively. These values correspond to relative errors of 3 and 5 % and are comparable to studies of Mona et al (2007) and Sakai et al (2007). Without any strong rearrangements in the optical setup, the calibration factor is very stable, enabling an operational applicability.…”
Section: Stability Of the Calibration Factorsupporting
confidence: 75%
“…The means and standard deviations amount to 15.2 ± 0.4 and 12.4 ± 0.6 g kg −1 before and after the major rearrangement in the optical setup on 15 April 2013, 10:06 UTC, respectively. These values correspond to relative errors of 3 and 5 % and are comparable to studies of Mona et al (2007) and Sakai et al (2007). Without any strong rearrangements in the optical setup, the calibration factor is very stable, enabling an operational applicability.…”
Section: Stability Of the Calibration Factorsupporting
confidence: 75%
“…Specifically, the water vapour profiles are determined from the Raman backscatter signals at 387 and 407 nm from nitrogen and water vapour molecules, respectively (Melfi et al, 1969;Cooney, 1971;Melfi, 1972). Besides temperature and water vapour, BASIL is capable of providing measurements of particle backscatter at 355, 532 and 1064 nm, particle extinction at 355 and 532 nm and particle depolarization at 355 and 532 nm (Griaznov et al, 2007;Mona et al, 2007;Bhawar et al, 2008;Di Girolamo et al, 2009a). For the purpose of determining particle size and microphysical parameters, measurements of the particle backscattering coefficient at 355, 532 and 1064 nm, of the particle extinction coefficient at 355 and 532 nm and of the depolarization ratio at 355 nm are used (Di Girolamo et al, 2009c).…”
Section: Basilmentioning
confidence: 99%
“…At CIAO large attention has been traditionally paid to the study of aerosol and water vapour using lidar techniques (Pappalardo et al, 2004a(Pappalardo et al, , b, 2010Mona et al, 2006Mona et al, , 2007Mona et al, , 2009). However, since 2004 the facility strengthened its observing capability for the monitoring of clouds through the acquisition of new active and passive microwave profilers, with the main objective to investigate aerosol-clouds interactions using both active and passive remote sensing techniques.…”
Section: The Cnr-imaa Atmospheric Observatory (Ciao)mentioning
confidence: 99%
“…In addition to MUSA and PEARL, CIAO is also equipped with a UV Raman lidar system for water vapour measurements (Mona et al, 2007), operational at CNR-IMAA since July 2002. It performs measurements simultaneously with PEARL.…”
Section: Lidarsmentioning
confidence: 99%
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