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- W2752552421 abstract "A bistatic CCD camera lidar (CLidar) was used at the National Oceanic and Atmospheric Administration’s Mauna LoaObservatory (MLO) to map aerosol light scattering. Laser light from a 532 nm, Nd:YAG laser was vertically transmittedinto the atmosphere and the scatter off clouds, aerosols and air molecules was detected using a CCD camera with wideangle optics and a laser line filter. The intensity of each CCD camera pixel imaging the beam was normalized to amolecular scattering model in an aerosol free region for subtraction of molecular scattering. Aerosol extinction wasderived using a column average aerosol phase function derived from AERONET sun photometer measurements at MLO.The CLidar design allows measurements of aerosol scattering all the way to the ground without an overlap correction.MLO, at 3397 m.a.s.l., typically receives free tropospheric air. During spring months, prevailing winds can occasionallytransport dust from Asian sources with high dust activity over MLO. Aerosol scattering measurements were taken by theCLidar during spring months at MLO and revealed extinction peaks at mid-range altitudes. Back trajectories of airparcels from MLO at the altitudes of these peaks were conducted using NOAA’s Hybrid Single Particle LagrangianIntegrated Trajectory (HYSPLIT) model and it was found that they passed over regions of Eastern Asia known assources of high dust activity. Relative humidity data from radiosondes and the NOAA stratospheric lidar’s water vaporchannel were examined to differentiate aerosol scattering from tenuous cloud scattering. This paper presents aerosolextinction data with observations of Asian dust as measured by the CLidar during spring months at MLO." @default.
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- W2752552421 date "2017-08-30" @default.
- W2752552421 modified "2023-09-28" @default.
- W2752552421 title "Lidar observations of long range dust transport over Mauna Loa Observatory" @default.
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- W2752552421 doi "https://doi.org/10.1117/12.2275723" @default.
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