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Open AccessJournal ArticleDOI

Measurements of the concentration and composition of nuclei for cirrus formation

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TLDR
Simultaneous measurements of the concentration and composition of tropospheric aerosol particles capable of initiating ice in cold (cirrus) clouds are reported, suggesting a predominant potential impact of these nuclei on cirrus formed by slow, large-scale lifting or small cooling rates, including subvisual cirrus.
Abstract
This article addresses the need for new data on indirect effects of natural and anthropogenic aerosol particles on atmospheric ice clouds. Simultaneous measurements of the concentration and composition of tropospheric aerosol particles capable of initiating ice in cold (cirrus) clouds are reported. Measurements support that cirrus formation occurs both by heterogeneous nucleation by insoluble particles and homogeneous (spontaneous) freezing of particles containing solutions. Heterogeneous ice nuclei concentrations in the cirrus regime depend on temperature, relative humidity, and the concentrations and physical and chemical properties of aerosol particles. The cirrus-active concentrations of heterogeneous nuclei measured in November over the western U.S. were <0.03 cm–3. Considering previous modeling studies, this result suggests a predominant potential impact of these nuclei on cirrus formed by slow, large-scale lifting or small cooling rates, including subvisual cirrus. The most common heterogeneous ice nuclei were identified as relatively pure mineral dusts and metallic particles, some of which may have origin through anthropogenic processes. Homogeneous freezing of large numbers of particles was detected above a critical relative humidity along with a simultaneous transition in nuclei composition toward that of the sulfate-dominated total aerosol population. The temperature and humidity conditions of the homogeneous nucleation transition were reasonably consistent with expectations based on previous theoretical and laboratory studies but were highly variable. The strong presence of certain organic pollutants was particularly noted to be associated with impedance of homogeneous freezing.

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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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Aerosol cloud precipitation interactions. Part 1. The nature and sources of cloud-active aerosols

TL;DR: In this article, the authors discuss the role of chemical composition and particle size in cloud condensation nucleation processes, and the role that the chemical composition plays in the process of cloud droplet and ice nucleation.
Journal ArticleDOI

Review of the vapour pressures of ice and supercooled water for atmospheric applications

TL;DR: In this paper, the vapour pressure of ice and supercooled water is reviewed with an emphasis on atmospheric applications, and various parametrizations are given for the vapor pressure, molar heat capacity, and latent heat of both ice and liquid water.
Journal ArticleDOI

Predicting global atmospheric ice nuclei distributions and their impacts on climate

TL;DR: It is shown that the concentrations of ice nuclei active in mixed-phase cloud conditions can be related to temperature and the number concentrations of particles larger than 0.5 μm in diameter, which reduces unexplained variability in iceuclei concentrations at a given temperature from ∼103 to less than a factor of 10.
References
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Journal ArticleDOI

Climate change 2001: the scientific basis

TL;DR: In this article, the authors present an overview of the climate system and its dynamics, including observed climate variability and change, the carbon cycle, atmospheric chemistry and greenhouse gases, and their direct and indirect effects.
Book

Microphysics of Clouds and Precipitation

TL;DR: In this article, the authors focus on one major aspect of cloud microphysics, which involves the processes that lead to the formation of individual cloud and precipitation particles, and provide an account of the major characteristics of atmospheric aerosol particles.
Journal ArticleDOI

Water activity as the determinant for homogeneous ice nucleation in aqueous solutions

TL;DR: This work shows from experimental data that the homogeneous nucleation of ice from supercooled aqueous solutions is independent of the nature of the solute, but depends only on the water activity of the solution, and presents a thermodynamic theory for homogeneous ice nucleation, which expresses the nucleation rate coefficient as a function of water activity and pressure.
Journal ArticleDOI

Influence of Cirrus Clouds on Weather and Climate Processes: A Global Perspective

TL;DR: In this paper, the authors reviewed and documented the current understanding and knowledge of the composition and structure of cirrus clouds and the radiative properties of clouds as they relate to weather and climate processes.
Journal ArticleDOI

African Dust Aerosols as Atmospheric Ice Nuclei

TL;DR: In this article, the ice nucleating ability of aerosol particles in air masses over Florida having sources from North Africa has been measured, and the concentrations of ice nuclei within dust layers at particle sizes below 1 pn exceeded 1/cu cm.
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