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From:Atmospheric Measurement Techniques (Vol. 15, Issue 5) Peer-ReviewedValidation of remote sensing retrievals of aerosol microphysical and optical properties requires in situ measurements of the same properties. We present here an improved imaging nephelometer for measuring the...
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 19) Peer-ReviewedIn situ measurements of aerosol microphysical, chemical, and optical properties were made during global-scale flights from 2016-2018 as part of the Atmospheric Tomography Mission (ATom). The NASA DC-8 aircraft flew from...
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From:Atmospheric Measurement Techniques (Vol. 11, Issue 1) Peer-Reviewed
Atmospheric aerosol is a key component of the chemistry and climate of the Earth's atmosphere. Accurate measurement of the concentration of atmospheric particles as a function of their size is fundamental to...
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 20) Peer-ReviewedHere we analyze regional-scale data collected on board the NOAA WP-3D aircraft during the 2013 Southeast Nexus (SENEX) campaign to study the aerosol-cloud droplet link and quantify the sensitivity of droplet number to...
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From:Atmospheric Chemistry and Physics (Vol. 18, Issue 16) Peer-Reviewed
Nighttime reaction of nitrate radicals (NO.sub.3) with biogenic volatile organic compounds (BVOC) has been proposed as a potentially important but also highly uncertain source of secondary organic aerosol (SOA). The...
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From:Atmospheric Measurement Techniques (Vol. 12, Issue 11) Peer-ReviewedSingle-particle mass spectrometry (SPMS) instruments characterize the composition of individual aerosol particles in real time. Their fundamental ability to differentiate the externally mixed particle types that...
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From:Atmospheric Measurement Techniques (Vol. 11, Issue 6) Peer-Reviewed
Earth's radiation budget is affected by new particle formation (NPF) and the growth of these nanometre-scale particles to larger sizes where they can directly scatter light or act as cloud condensation nuclei (CCN)....
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 11) Peer-ReviewedThe size of aerosol particles has fundamental effects on their chemistry and radiative effects. We explore those effects using aerosol size and composition data in the lowermost stratosphere along with calculations of...
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From:Atmospheric Measurement Techniques (Vol. 10, Issue 10) Peer-ReviewedAÂ light-scattering module was coupled to an airborne, compact time-of-flight aerosol mass spectrometer (LS-AMS) to investigate collection efficiency (CE) while obtaining nonrefractory aerosol chemical...
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From:Atmospheric Measurement Techniques (Vol. 12, Issue 6) Peer-Reviewed
From 2016 to 2018 a DC-8 aircraft operated by the US National Aeronautics and Space Administration (NASA) made four series of flights, profiling the atmosphere from 180 m to â¼12 km...
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From:Bulletin of the American Meteorological Society (Vol. 95, Issue 12) Peer-ReviewedABSTRACT Given the rapid nature of climate change occurring in the Arctic and the difficulty climate models have in quantitatively reproducing observed changes such as sea ice loss, it is important to improve...
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 23) Peer-ReviewedGlobal observations and model studies indicate that new particle formation (NPF) in the upper troposphere (UT) and subsequent particles supply 40 %-60 % of cloud condensation nuclei (CCN) in the lower troposphere, thus...
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From:Atmospheric Measurement Techniques (Vol. 11, Issue 6) Peer-Reviewed
Earth's radiation budget is affected by new particle formation (NPF) and the growth of these nanometre-scale particles to larger sizes where they can directly scatter light or act as cloud condensation nuclei (CCN)....
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 11) Peer-ReviewedThe details of aerosol processes and size distributions in the stratosphere are important for both heterogeneous chemistry and aerosol-radiation interactions. Using in situ, global-scale measurements of the size...
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 9) Peer-ReviewedBiomass burning aerosol is a major source of PM.sub.2.5, and significantly affects Earth's radiative budget. The magnitude of its radiative effect is poorly quantified due to uncertainty in the optical properties of...
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From:Proceedings of the National Academy of Sciences of the United States (Vol. 117, Issue 9) Peer-ReviewedAbstract Only
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From:Atmospheric Measurement Techniques (Vol. 11, Issue 1) Peer-ReviewedByline: Agnieszka Kupc, Christina Williamson, Nicholas L. Wagner, Mathews Richardson, Charles A. Brock To access, purchase, authenticate, or subscribe to the full-text of this article, please visit this link:...
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From:Atmospheric Measurement Techniques (Vol. 10, Issue 5) Peer-ReviewedThe sum of all reactive nitrogen species (NO.sub.y) includes NO.sub.x (NO.sub.2 + NO) and all of its oxidized forms, and the accurate detection of NO.sub.y is critical to understanding atmospheric nitrogen chemistry....
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 6) Peer-ReviewedByline: Daniel M. Murphy, Karl D. Froyd, Huisheng Bian, Charles A. Brock, Jack E. Dibb, Joshua P. DiGangi, Glenn Diskin, Maximillian Dollner, Agnieszka Kupc, Eric M. Scheuer, Gregory P. Schill, Bernadett Weinzierl,...
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From:Atmospheric Measurement Techniques (Vol. 14, Issue 6) Peer-ReviewedWe evaluate the sensitivity of the size calibrations of two commercially available, high-resolution optical particle sizers to changes in aerosol composition and complex refractive index (RI). The Droplet Measurement...