2014
DOI: 10.1016/j.jastp.2014.01.006
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Estimation of the mixing layer height over a high altitude site in Central Himalayan region by using Doppler lidar

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Cited by 23 publications
(17 citation statements)
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“…These measurements have been used in many studies (e.g. Hogan et al, 2009;Lothon et al, 2009;Barlow et al, 2011;Shukla et al, 2014). For this measurement, the DL simply points at zenith and continually collects measurements of the vertical velocity w, for which w 2 , spectra of w, and other turbulence statistics of w can be calculated at every range gate over a user-defined time interval.…”
Section: Introductionmentioning
confidence: 99%
“…These measurements have been used in many studies (e.g. Hogan et al, 2009;Lothon et al, 2009;Barlow et al, 2011;Shukla et al, 2014). For this measurement, the DL simply points at zenith and continually collects measurements of the vertical velocity w, for which w 2 , spectra of w, and other turbulence statistics of w can be calculated at every range gate over a user-defined time interval.…”
Section: Introductionmentioning
confidence: 99%
“…We varied the SNR from -15 dB to -25 dB and found the -20 dB to be an appropriate threshold for all scans. Therefore, we applied a threshold of -20 dB for all types of scans (FTP, RHI and PPI) of the DL which can considerably reduce the noise level 12,21,22 .…”
Section: Resultsmentioning
confidence: 99%
“…We have estimated the inversion or mixing layer height by using vertical velocity variance data of DL on 2 December 2011 (Figure 6 e). To estimate the inversion or mixing layer height from the DL signal, we have used the wavelet-covariance transform (WCT) method and detailed description about the WCT can be found elsewhere 22 . The dilation is used 150 m for the 2 December 2011 in WCT.…”
Section: Diurnal Variation Of Snr Vertical Velocity and Attenuated Bmentioning
confidence: 99%
“…Os Ceilometers são instrumentos de sensoriamento remoto do tipo LIDAR, que registram a intensidade do retroespalhamento óptico no infravermelho próximo, por meio da emissão de um pulso de luz na vertical, sendo executado de forma autônoma. E assim, se obtêm a base das nuvens e, por meio desta é estimada à altura da CLP (Shukla et al, 2014). Por se tratar de um instrumento de alta-frequência, possuindo uma taxa amostral da altura da CLP a cada 16 segundos, este é uma ferramenta poderosa para rastreamento da altura da CLP ao longo do seu ciclo diário.…”
Section: Methodsunclassified