2015
DOI: 10.5194/amt-8-1875-2015
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Low-level mixing height detection in coastal locations with a scanning Doppler lidar

Abstract: Abstract. Mixing layer height (MLH) is one of the key parameters in describing lower tropospheric dynamics and capturing its diurnal variability is crucial, especially for interpreting surface observations. In this paper we introduce a method for identifying MLH below the minimum range of a scanning Doppler lidar when operated at vertical. The method we propose is based on velocity variance in lowelevation-angle conical scanning and is applied to measurements in two very different coastal environments: Limasso… Show more

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Cited by 63 publications
(70 citation statements)
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“…Lee AIWs (or orographic waves) are one of the types of AGWs, which arise leeward of obstacles at the stable stratification of an incoming flow (Vel'tishchev and Stepanenko, 2006;Kozhevnikov, 1999;Makarenko and Maltseva, (Pearson et al, 2009). These lidars find expanding applications in studies of ABL (O'Connor et al, 2010;Sathe and Mann, 2012;van Dinther et al, 2015;Päschke et al, 2015;Smalikho and Banakh, 2015a, b;Smalikho et al, 2015a, b, c;Vakkari et al, 2015). The processing of all data measured by the lidar and the analysis of the processed data have revealed several cases of formation of atmospheric internal waves for the period of measurements.…”
Section: Introductionmentioning
confidence: 99%
“…Lee AIWs (or orographic waves) are one of the types of AGWs, which arise leeward of obstacles at the stable stratification of an incoming flow (Vel'tishchev and Stepanenko, 2006;Kozhevnikov, 1999;Makarenko and Maltseva, (Pearson et al, 2009). These lidars find expanding applications in studies of ABL (O'Connor et al, 2010;Sathe and Mann, 2012;van Dinther et al, 2015;Päschke et al, 2015;Smalikho and Banakh, 2015a, b;Smalikho et al, 2015a, b, c;Vakkari et al, 2015). The processing of all data measured by the lidar and the analysis of the processed data have revealed several cases of formation of atmospheric internal waves for the period of measurements.…”
Section: Introductionmentioning
confidence: 99%
“…Turbulent kinetic energy (TKE) dissipation rate was calculated from the Doppler lidar measurements according to the method by O'Connor et al (2010). A VAD-based proxy for turbulent mixing (σ 2 VAD) was calculated from the 30° elevation VAD scan according to the method by Vakkari et al (2015). MLH was determined from the TKE dissipation rate and the VAD scan 30 similar to Vakkari et al (2015).…”
Section: Complementary Measurementsmentioning
confidence: 99%
“…A VAD-based proxy for turbulent mixing (σ 2 VAD) was calculated from the 30° elevation VAD scan according to the method by Vakkari et al (2015). MLH was determined from the TKE dissipation rate and the VAD scan 30 similar to Vakkari et al (2015). Briefly, first a constant threshold of 10 -4 m 2 s -3 was applied to the TKE dissipation rate profile, (Vakkari et al, 2015).…”
Section: Complementary Measurementsmentioning
confidence: 99%
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“…Suomi et al, 2015). However, Doppler lidars can also provide high-resolution turbulent measurements, in both the vertical direction (O'Connor et al, 2010) and, potentially, the horizontal direction (Vakkari et al, 2015).…”
Section: Introductionmentioning
confidence: 99%