2021
DOI: 10.5194/acp-21-517-2021
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Measurement report: Properties of aerosol and gases in the vertical profile during the LAPSE-RATE campaign

Abstract: Abstract. Unmanned aerial systems (UASs) are increasingly being used as observation platforms for atmospheric applications. The Lower Atmospheric Process Studies at Elevation – a Remotely-piloted Aircraft Team Experiment (LAPSE-RATE) in Alamosa, Colorado, USA, on 14–20 July 2018 investigated and validated different UASs, measurement sensors and setup configurations. Flight teams from the Finnish Meteorological Institute (FMI) and Kansas State University (KSU) participated in LAPSE-RATE to measure and investiga… Show more

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Cited by 12 publications
(4 citation statements)
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“…Our explanation for the correlation between the starting time of boundary layer growth and the start of NPF events is that precursor gases from elevated levels are mixed down to the surface and initiate an NPF event at the surface or that the NPF event is initiated aloft, which has been observed by several studies (Größ et al, 2018;Lampilahti et al, 2021;Brus et al, 2021), and the newly formed particles are then measured at the surface once they are entrained within the growing boundary layer.…”
Section: New-particle-formation Eventsmentioning
confidence: 85%
“…Our explanation for the correlation between the starting time of boundary layer growth and the start of NPF events is that precursor gases from elevated levels are mixed down to the surface and initiate an NPF event at the surface or that the NPF event is initiated aloft, which has been observed by several studies (Größ et al, 2018;Lampilahti et al, 2021;Brus et al, 2021), and the newly formed particles are then measured at the surface once they are entrained within the growing boundary layer.…”
Section: New-particle-formation Eventsmentioning
confidence: 85%
“…The performance of this CPC was assessed by Hämeri et al (2002) in laboratory constant-temperature/pressure conditions. Since then, it has been employed in numerous studies where outdoor measurements have been carried out with manned hot-air balloons (e.g., Laakso et al, 2007), unmanned tethered balloons (e.g., Chen et al, 2018;Samad et al, 2020, Brus et al, 2021Creamean et al, 2021), and unmanned aerial vehicles (e.g., Altstädter et al, 2015;Altstädter et al, 2018;Lampert et al, 2020). It should be noted here that the detection efficiency of CPCs can be affected by the measurement conditions as these can in principle affect both the temperature difference/window between the saturator and the condenser (Hermann & Wiedensohler, 2001), as well as the position of this window in the temperature space (Barmpounis et al, 2018).…”
Section: Introductionmentioning
confidence: 99%
“…Three general approaches were used in previous studies of cloud microphysical properties: in situ sampling through airborne measurements by aircraft (e.g., Heymsfield et al, 2011;Craig et al, 2014;Petäjä et al, 2016;Nguyen et al, 2021) and recently by unmanned aerial systems (UASs) (e.g., Girdwood et al, 2020;Brus et al, 2021;Harrison et al, 2021), in situ sampling by using laboratory cloud chambers (e.g., Möhler et al, 2003;Stratmann et al, 2004;Nichman et al, 2017;Doulgeris et al, 2018), and in situ ground-based measurements (e.g., Guyot et al, 2015;Lloyd et al, 2015;Lowenthal et al, 2019;Doulgeris et al, 2020). In situ airborne and ground measurements (Wandinger et al, 2018) using cloud spectrometers are considered fundamental as they offer instrumental access to individual hydrometeors within a sampling volume.…”
Section: Introductionmentioning
confidence: 99%