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Aircraft observations of the upper tropospheric fine particle aerosol in the Northern and Southern Hemispheres at midlatitudes

TLDR
In this paper, two aircraft field campaigns have been performed to study aerosol and cirrus cloud properties of the upper troposphere (UT) in the midlatitudes of the southern hemisphere (SH) and the northern hemisphere (NH).
Abstract
] As part of the project INCA (InterhemisphericDifferences in Cirrus Properties from AnthropogenicEmissions) two aircraft field campaigns have beenperformed to study aerosol and cirrus cloud properties ofthe upper troposphere (UT) in the midlatitudes of thesouthern hemisphere (SH) and the northern hemisphere(NH). This paper focuses on the measurements of UTnumber concentrations and tropospheric vertical profilesof volatile and refractory Aitken as well as totalaccumulation mode particles. The results are discussedwith respect to interhemispheric differences. Aerosolnumber concentrations in the NH are more variable andtypically a factor of 2–3 higher. The SH data considerablyextend the few existing UT in situ aerosol measurementsinthe SH midlatitudes.

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Bounding the role of black carbon in the climate system: A scientific assessment

TL;DR: In this paper, the authors provided an assessment of black-carbon climate forcing that is comprehensive in its inclusion of all known and relevant processes and that is quantitative in providing best estimates and uncertainties of the main forcing terms: direct solar absorption; influence on liquid, mixed phase, and ice clouds; and deposition on snow and ice.
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The aerosol-climate model ECHAM5-HAM

TL;DR: The aerosol-climate modelling system ECHAM5-HAM as mentioned in this paper is based on a flexible microphysical approach and, as the number of externally imposed parameters is minimised, allows the application in a wide range of climate regimes.
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Transport impacts on atmosphere and climate: Aviation

TL;DR: A comprehensive updated assessment of aviation is provided, highlighting the impact of aviation emissions of CO2 on global mean surface temperature last for many hundreds of years (in common with other sources), whilst its non-CO2 effects onTemperature last for decades.
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The global lightning-induced nitrogen oxides source

TL;DR: The best estimate of the annual global LNOx nitrogen oxides nitrogen mass source and its uncertainty range is (5±3) Tg a−1 in this paper, implying larger flash-specific NOx emissions.
References
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Journal ArticleDOI

Formation and cycling of aerosols in the global troposphere

TL;DR: In this article, the authors present an integrated microphysical and dynamical picture of the global tropospher ic aerosol system by reviewing the microphysical processes and those elements of the general circulation that determine the size distribution and chemical composition of the aerosol.
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A Pacific Aerosol Survey. Part I: A Decade of Data on Particle Production, Transport, Evolution, and Mixing in the Troposphere*

TL;DR: In this paper, the authors integrated extensive aerosol data collected during the past decade around the Pacific basin to provide a preliminary assessment of aerosol microphysics for this region and cycling of aerosols in the troposphere.
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Nucleation in the equatorial free troposphere: Favorable environments during PEM‐Tropics

TL;DR: A combination of aerosol and gas phase instrumentation was employed aboard the NASA-P3B as part of the Pacific Exploratory Mission-Tropics (PEM-T) in the eastern equatorial Pacific during August-October 1996 as mentioned in this paper.
Journal ArticleDOI

Vertical and horizontal distributions of the aerosol number concentration and size distribution over the northern Indian Ocean

TL;DR: In this paper, the authors used a combination of back trajectory information and cloud top temperatures retrieved from satellite images to identify the origin of large convective clouds in the Indian Ocean Experiment (INDOEX).
Journal ArticleDOI

Quantitative measurement of the microphysical and optical properties of cirrus clouds with four different in situ probes: Evidence of small ice crystals

TL;DR: In this article, a combination of these four techniques provided a description of particles within a diameter range varying from a few micrometers (typically 3 μm) to 800 μm.
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