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Abstract. Accurate airborne aerosol instrumentation is required to determine thespatial distribution of ambient aerosol particles, particularly when dealingwith the complex vertical profiles and horizontal variations of atmosphericaerosols. A versatile water-based condensation particle counter (vWCPC) hasbeen developed to provide aerosol concentration measurements under variousenvironments with the advantage of reducing the health and safety concernsassociated with using butanol or other chemicals as the working fluid.However, the airborne deployment of vWCPCs is relatively limited due to thelack of characterization of vWCPC performance at reduced pressures. Giventhe complex combinations of operating parameters in vWCPCs, modeling studieshave advantages in mapping vWCPC performance. In this work, we thoroughly investigated the performance of a laminar-flowvWCPC using COMSOL Multiphysics® simulation coupled withMATLAB™. We compared it against a modified vWCPC (vWCPC model 3789, TSI,Shoreview, MN, USA). Our simulation determined the performance of particleactivation and droplet growth in the vWCPC growth tube, including thesupersaturation, Dp,kel,0 (smallest size of particle that canbe activated), Dp,kel,50 (particle size activated with 50 %efficiency) profile, and final growth particle size Dd underwide operating temperatures, inlet pressures P (30–101 kPa), and growthtube geometry (diameter D and initiator length Lini). Theeffect of inlet pressure and conditioner temperature on vWCPC 3789performance was also examined and compared with laboratory experiments. TheCOMSOL simulation result showed that increasing the temperature difference(ΔT) between conditioner temperature Tcon andinitiator Tini will reduce Dp,kel,0 and thecut-off size Dp,kel,50 of the vWCPC. In addition, loweringthe temperature midpoint(Tmid=Tcon+Tini2) increasesthe supersaturation and slightly decreases the Dp,kel. Thedroplet size at the end of the growth tube is not significantly dependent onraising or lowering the temperature midpoint but significantly decreases atreduced inlet pressure, which indirectly alters the vWCPC empirical cut-offsize. Our study shows that the current simulated growth tube geometry (D=6.3 mm and Lini=30 mm) is an optimized choice forcurrent vWCPC flow and temperature settings. The current simulation can morerealistically represent the Dp,kel for 7 nm vWCPC and alsoachieved good agreement with the 2 nm setting. Using the new simulationapproach, we provide an optimized operation setting for the 7 nm setting.This study will guide further vWCPC performance optimization forapplications requiring precise particle detection and atmospheric aerosolmonitoring. 

Abstract. A tethered-balloon system (TBS) has been developed and is beingoperated by Sandia National Laboratories (SNL) on behalf of the U.S.Department of Energy's (DOE) Atmospheric Radiation Measurement (ARM) UserFacility in order to collect in situ atmospheric measurements withinmixed-phase Arctic clouds. Periodic tethered-balloon flights have beenconducted since 2015 within restricted airspace at ARM's Advanced MobileFacility 3 (AMF3) in Oliktok Point, Alaska, as part of the AALCO (AerialAssessment of Liquid in Clouds at Oliktok), ERASMUS (Evaluation of RoutineAtmospheric Sounding Measurements using Unmanned Systems), and POPEYE(Profiling at Oliktok Point to Enhance YOPP Experiments) field campaigns. Thetethered-balloon system uses helium-filled 34 m3 helikites and 79 and104 m3 aerostats to suspend instrumentation that is used to measureaerosol particle size distributions, temperature, horizontal wind, pressure,relative humidity, turbulence, and cloud particle properties and tocalibrate ground-based remote sensing instruments. Supercooled liquid water content (SLWC) sondes using the vibrating-wireprinciple, developed by Anasphere Inc., were operated at Oliktok Point atmultiple altitudes on the TBS within mixed-phase clouds for over 200 h.Sonde-collected SLWC data were compared with liquid water content derivedfrom a microwave radiometer, Ka-band ARM zenith radar, and ceilometer at the AMF3, as well as liquid water content derived from AMF3 radiosonde flights. The in situ data collected by the Anasphere sensors were also compared with data collected simultaneously by an alternative SLWC sensor developed at the University of Reading, UK; both vibrating-wire instruments were typically observed to shed their ice quickly upon exiting the cloud or reaching maximum ice loading. Temperature sensing measurements distributed with fiber optic tethered balloons were also compared with AMF3 radiosonde temperature measurements. Combined, the results indicate that TBS-distributedtemperature sensing and supercooled liquid water measurements are inreasonably good agreement with remote sensing and radiosonde-basedmeasurements of both properties. From these measurements and sensorevaluations, tethered-balloon flights are shown to offer an effective methodof collecting data to inform and constrain numerical models, calibrate andvalidate remote sensing instruments, and characterize the flight environmentof unmanned aircraft, circumventing the difficulties of in-cloud unmanned aircraft flights such as limited flight time and in-flight icing. 

Abstract A multi-agency succession of field campaigns was conducted in southeastern Texas during July 2021 through October 2022 to study the complex interactions of aerosols, clouds and air pollution in the coastal urban environment. As part of the Tracking Aerosol Convection interactions Experiment (TRACER), the TRACER- Air Quality (TAQ) campaign the Experiment of Sea Breeze Convection, Aerosols, Precipitation and Environment (ESCAPE) and the Convective Cloud Urban Boundary Layer Experiment (CUBE), a combination of ground-based supersites and mobile laboratories, shipborne measurements and aircraft-based instrumentation were deployed. These diverse platforms collected high-resolution data to characterize the aerosol microphysics and chemistry, cloud and precipitation micro- and macro-physical properties, environmental thermodynamics and air quality-relevant constituents that are being used in follow-on analysis and modeling activities. We present the overall deployment setups, a summary of the campaign conditions and a sampling of early research results related to: (a) aerosol precursors in the urban environment, (b) influences of local meteorology on air pollution, (c) detailed observations of the sea breeze circulation, (d) retrieved supersaturation in convective updrafts, (e) characterizing the convective updraft lifecycle, (f) variability in lightning characteristics of convective storms and (g) urban influences on surface energy fluxes. The work concludes with discussion of future research activities highlighted by the TRACER model-intercomparison project to explore the representation of aerosol-convective interactions in high-resolution simulations. 

Abstract The Cloud, Aerosol, and Complex Terrain Interactions (CACTI) field campaign was designed to improve understanding of orographic cloud life cycles in relation to surrounding atmospheric thermodynamic, flow, and aerosol conditions. The deployment to the Sierras de Córdoba range in north-central Argentina was chosen because of very frequent cumulus congestus, deep convection initiation, and mesoscale convective organization uniquely observable from a fixed site. The C-band Scanning Atmospheric Radiation Measurement (ARM) Precipitation Radar was deployed for the first time with over 50 ARM Mobile Facility atmospheric state, surface, aerosol, radiation, cloud, and precipitation instruments between October 2018 and April 2019. An intensive observing period (IOP) coincident with the RELAMPAGO field campaign was held between 1 November and 15 December during which 22 flights were performed by the ARM Gulfstream-1 aircraft. A multitude of atmospheric processes and cloud conditions were observed over the 7-month campaign, including: numerous orographic cumulus and stratocumulus events; new particle formation and growth producing high aerosol concentrations; drizzle formation in fog and shallow liquid clouds; very low aerosol conditions following wet deposition in heavy rainfall; initiation of ice in congestus clouds across a range of temperatures; extreme deep convection reaching 21-km altitudes; and organization of intense, hail-containing supercells and mesoscale convective systems. These comprehensive datasets include many of the first ever collected in this region and provide new opportunities to study orographic cloud evolution and interactions with meteorological conditions, aerosols, surface conditions, and radiation in mountainous terrain.