A review of atmospheric aerosol measurements
By P. Mcmurry. 2000
856 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/e31d133462c41fbfb451883fd3fcfaae3a326e09
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In Atmospheric Science
In Global and Planetary Change
Citations in the corpus
- Receptor modeling application framework for particle source apportionment. (2002, background): “Collocated continuous monitor sampling: Watson et al. (1998a) and McMurry (2000) describe several continu- ous particle detectors that can obtain mass, mass-surrogates, and chemical- or size-specific concentrations over averaging periods of 1–60 min duration.”
- Ambient nano and ultrafine particles from motor vehicle emissions: Characteristics, ambient processing and implications on human exposure (2008, methodology): “(McMurry 2000).”
- Particle Morphology and Density Characterization by Combined Mobility and Aerodynamic Diameter Measurements. Part 1: Theory (2004, background): “Hand et al. (2002) combined size distribution data from a DMA, an optical particle counter (OPC), and an APS, and used overlap regions to estimate refractive index and (a third definition of) effective density: ρIIeff = ρp χ .”
- Dependence of nucleation rates on sulfuric acid vapor concentration in diverse atmospheric locations (2008, background): “The Nano-SMPS diameter size range was chosen to be small enough to be considered newly formed but large enough to achieve good Poisson counting statistics [ McMurry, 2000 ].”
- Characterization of an Aerodyne Aerosol Mass Spectrometer (AMS): Intercomparison with Other Aerosol Instruments (2005, background): “Recent advances in aerosol measurement techniques have greatly improved our current understanding of aerosol physics and chemistry in the atmosphere (eg, McMurry 2000 ).”
- Modeling the formation and growth of atmospheric molecular clusters: A review (2020, methodology): “Detection of aerosol particles can be performed using Neutral cluster and Air Ion Spectrometers (NAIS) (Kulmala et al., 2007; Manninen et al., 2009) or condensation particle counters (CPC) (McMurry, 2000) with detection thresholds down to around 2–3 nm in diameter (McMurry, 2000).”
- Size and time-resolved growth rate measurements of 1 to 5 nm freshly formed atmospheric nuclei (2012, background): “As aerosol sizing and counting instrumentation have improved since then (McMurry, 2000), particle growth rates have been obtained for even smaller sizes, down to 3 nm – the conventional size detection limit for measuring the total aerosol (Stolzenburg and McMurry, 1991).”