In Situ Observations of the Microphysical Properties of Wave, Cirrus, and Anvil Clouds. Part II: Cirrus Clouds

By R. P. Lawson, B. Baker, B. Pilson, Q. Mo. 2006

197 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/92dbe62a5b8ede2d8cadb5ea895a03c8c1c7905e

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Citations in the corpus

Heterogeneous freezing of ice on atmospheric aerosols containing ash, soot, and soil (2009, unknown): “This may explain high ice crystal concentrations observed at cloud tops and in downdrafts [ Beard , 1992; Rangno and Hobbs , 1990; Field et al. , 2001; Cotton and Field , 2002; Ansmann et al. , 2005; Baker and Lawson , 2005; Lawson et al. , 2006].”
The 2D-S (Stereo) Probe: Design and Preliminary Tests of a New Airborne, High-Speed, High-Resolution Particle Imaging Probe (2006, background): “The location of the first ice particles encountered in the mixed-phase cloud region is of interest to cloud physicists, because this relates to ice nucleation, a process that is still poorly understood in wave clouds (Baker and Lawson 2006).”
Effects of ice particles shattering on the 2D-S probe (2011, methodology): “The much smaller mass where small ice particles exist and typically dominate the size distribution throughout the depth of cloud (e.g., Lawson et al., 2006b).”
Mixed-Phase Clouds: Progress and Challenges (2017, methodology): “In leewave clouds, mixed-phase conditions form in the upwind section of the cloud as a result of droplet formation, ice initiation on INP, and droplet freezing (Baker and Lawson 2006; Field et al. 2012) (Fig.”
A review of the light scattering properties of cirrus (2009, background): “However, there have been other and more recent cloud and laboratory studies which attempt to classify ice crystal shape as a function of environmental temperature, see for instance [40–42].”
A New Bulk Microphysical Scheme That Includes Riming Intensity and Temperature-Dependent Ice Characteristics (2011, methodology): “We utilize the temperature-dependent A-D relationship derived by Baker and Lawson (2006) and include the effect of Ri to get”
ML-CIRRUS : The airborne experiment on natural cirrus and contrail cirrus with the high-altitude long-range research aircraft HALO (2017, background): “Currently, aircraft-induced condensation trails or contrail cirrus are considered to be responsible for the major part of the aviation climate impact (IPCC 2013), and growth rates in aviation (Lee et al. 2009) suggest future increases.”