Predicting global atmospheric ice nuclei distributions and their impacts on climate

By P. DeMott, A. Prenni, Xiaohong Liu, S. Kreidenweis, M. Petters, C. Twohy, M. Richardson, T. Eidhammer, D. Rogers. Proceedings of the National Academy of Sciences of the United States of America, 2010

1,246 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/1d9a52ef58780dde3d2a95f19bdf1f0348d4beff

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Citations in the corpus

On the Representation of High-Latitude Boundary Layer Mixed-Phase Cloud in the ECMWF Global Model (2014, background): “Equation (3) based on Meyers et al. (1992) is used here, but there are significant spatial and temporal variations and uncertainties with many proposed alternative parameterizations as a function of temperature and supersaturation (Cooper 1986; Prenni et al. 2007; DeMott et al. 2010).”
Confronting the Challenge of Modeling Cloud and Precipitation Microphysics (2020, background): “…water path, cloud forcing, cloud feedback, and for some even the climate sensitivity were found to depend strongly on the choice of the ice nucleation scheme (e.g., Barahona et al., 2010; DeMott et al., 2010; Garimella et al., 2018; Gettelman et al., 2012; Liu et al., 2012; Storelvmo et al., 2011).”
Resurgence in Ice Nuclei Measurement Research (2011, background): “The majority of the instruments at ICIS-2007 were of continuous flow diffusion chamber design, which has been responsible for most of the aircraft measurements of ice nuclei since the late 1990s (DeMott et al. 2010).”
A New Ice Nucleation Active Site Parameterization for Desert Dust and Soot (2017, background): “More simple descriptions of heterogeneous ice nucleation (e.g., DeMott et al. 2010, 2015) are easier to use in models but, in general, are not applicable to all atmospherically relevant conditions or atmospherically relevant aerosol types.”
Overview of Ice Nucleating Particles (2017, methodology): “Later, DeMott et al. (2010) updated this to a parameterization using the observed particle number concentration larger than 500 nm ( n a .”
Opinion: Cloud-phase climate feedback and the importance of ice-nucleating particles (2020, background): “Many models create ice as a function of temperature but lack the link to aerosol; this has been shown to be inadequate (DeMott et al., 2010; Vergara-Temprado et al., 2018).”
Revisiting ice nucleation from precipitation samples (2015, methodology): “…for different aerosol types [Hoose and Möhler, 2012; Murray et al., 2012] and informed the continuing refinement of INP parameterizations [DeMott et al., 2010; Fletcher, 1962; Georgii and Kleinjung, 1967; Khvorostyanov and Curry, 2004;Meyers et al., 1992; Niemand et al., 2012; Phillips…”
Secondary Ice Production: Current State of the Science and Recommendations for the Future (2016, neutral): “Notwithstanding instrumentation uncertainties in measurements 1 of both ice crystal concentrations and INPs, measurable concentrations of atmospheric INPs can be smaller by orders of magnitude at these temperatures (DeMott et al. 2010, 2016).”
Representation of microphysical processes in cloud‐resolving models: Spectral (bin) microphysics versus bulk parameterization (2015, background): “In light of the uncertainties of ice production processes, different empirically based parameterizations have been developed [e.g.,Meyers et al., 1992; DeMott et al., 2010; Phillips et al., 2013].”
Ice structures, patterns, and processes: A view across the icefields (2012, background): “Each freezing mode is active over a typical range of temperature and relative humidity (RH) (DeMott et al., 2010; Meyers et al., 1992).”
The ice nucleation ability of one of the most abundant types of fungal spores found in the atmosphere (2010, neutral): “This value is a factor of approximately 4 to 800 smaller than the number of IN observed in the atmosphere at temperatures around −15C (DeMott et al., 2010).”
Intercomparison of the cloud water phase among global climate models (2014, methodology): “The changes in the downwelling solar radiation at the surface for these two most sensitive GCMs between Experiment 1 (GCMs default heterogeneous ice nucleation) and Experiment 2 (ice nucleation following DeMott et al. [2010]) are 3Wm 2 for CAM-Oslo and Figure 7.”
Biological residues define the ice nucleation properties of soil dust (2011, background): “It has been suggested that all IN active at temperatures warmer than −10C are of biological origin (Christner et al., 2008; DeMott et al., 2010).”