Production of Ice in Tropospheric Clouds: A Review.

By Will H Cantrell, Andrew J. Heymsfield. 2005

408 citations recorded by the source corpus.

Subfields: Aerospace Engineering, Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/df1d4f7379854ff57e3d32285c43f45903b44782

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Aerospace Engineering

1. I. Sölch
2. Bernd Kärcher
3. T. Bartels-Rausch

In Atmospheric Science

1. Markku Kulmala
2. C. Hoose
3. Bernd Kärcher
4. Ulrike Lohmann
5. V. Kerminen
6. K. Lehtinen
7. J. Kristjánsson
8. M. Krämer

In Global and Planetary Change

1. Markku Kulmala
2. C. Hoose
3. Bernd Kärcher
4. Ulrike Lohmann
5. J. Kristjánsson
6. V. Kerminen
7. M. Krämer
8. A. Hazra

Citations in the corpus

• The Zurich Ice Nucleation Chamber (ZINC)-A New Instrument to Investigate Atmospheric Ice Formation (2008, background): “While there is now a good understanding of particle properties that affect CCN activation, there is still a lack of understanding as to which intrinsic properties of aerosol particles determine their ice nucleation capabilities ( Szyrmer and Zawadzki 1997 ; Cantrell and Heymsfield 2005 ).”
• Overview of Ice Nucleating Particles (2017, background): “termining the physical properties of clouds and the chemical composition of the troposphere by exerting enormous influence on physical processes such as radiative transfer, precipitation, and cloud electrification (Cantrell and Heymsfield 2005).”
• Ice structures, patterns, and processes: A view across the icefields (2012, background): “Heterogeneous freezing is traditionally categorized in four ways: deposition (ice deposits directly onto an ice nucleus), condensation (liquid water condenses and subsequently freezes), immersion (a solid particle within a cooling droplet initiates freezing), and contact (surface contact between a l”
• SALSA – a Sectional Aerosol module for Large Scale Applications (2007, background): “Insoluble particles, such as freshly-emitted desert dust particles, do not act as cloud condensation nuclei (CCN) but may instead act as cloud nuclei (e.g. Cantrell and Heymsfield, 2005).”
• Experimental study on the ice nucleation ability of size-selected kaolinite particles in the immersion mode (2010, background): “tant for the understanding of precipitation formation and of cloud radiative properties [e.g., Ansmann et al., 2008; Cantrell and Heymsfield, 2005; Durant and Shaw, 2005].”
• A large‐eddy model for cirrus clouds with explicit aerosol and ice microphysics and Lagrangian ice particle tracking (2010, background): “Knowledge of this pathway in the atmosphere is lacking (Cantrell and Heymsfield, 2005); it can therefore not be adequately quantified and implemented in current models.”
• Deactivation of ice nuclei due to atmospherically relevant surface coatings (2009, background): “Less well studied to date is the process of freezing when an IN contacts a droplet (Cantrell and Heymsfield 2005).”
• Microbiology and atmospheric processes: the role of biological particles in cloud physics (2007, neutral): “Biological particles, including certain bacteria, pollen, and decayed organic material have also been identified as ice nuclei (e.g. reviews by Cantrell and Heymsfield, 2005; Morris et al., 2004; Szyrmer and Zawadzki, 1997).”
• A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and Biological Particles in a Global Climate Model (2010, background): “Ice in tropospheric clouds is important for cloud radiative properties and precipitation formation, but its formation is neither theoretically fully understood nor empirically well constrained (Cantrell and Heymsfield 2005).”