Geophysical Research Letters · 1974 · 20 citations · 13 references
Natural SciencesEarth SciencesAtmospheric ChemistryAtmospheric ScienceVolcanologyAerosol PhysicsAerosol Remote SensingAtmospheric OpticsAtmospheric ScatteringParticulate MatterAerosol MonitoringAerosol Optical PropertiesAerosol Particle Size DistributionAerosol PropertiesAerosol Size DistributionAtmospheric Aerosol CharacterizationScatteringVolcanic Aerosols
A 4λ nephelometer has been included as part of the aerosol monitoring program at Mauna Loa Observatory, Hawaii. This instrument is capable of measuring the clean air (nighttime downslope wind conditions) aerosol light scattering coefficient of b sp ≃ 3 × 10 −7 m −1 , about 1% of the molecular scattering of air. Typical light scattering values for “dirty” (upslope wind) conditions are of the order of b sp ≃ 5 × 10 −5 m −1 . Although rare, vigorous fountaining at Kilauea Volcano occasionally ejects particulate into the upper air and encroaches upon the clean air at Mauna Loa. However, volcanism does not interfere significantly with the background monitoring program. The aerosol size information obtained from the 4λ nephelometer functions as an indicator of the aerosol source and therefore of possible global trends in aerosol size or concentration.
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Local Wind Circulation on the Slopes of Mauna Loa
B. G. Mendonca · Journal of applied meteorology · 1969 · 115 citations · Full text
Trace constituents emitted to the atmosphere by Hawaiian volcanoes
R. D. Cadle, A. F. Wartburg, W. H. Pollock et al. · Chemosphere · 1973 · 55 citations