Evidence of liquid dependent ice nucleation in high‐latitude stratiform clouds from surface remote sensors
By Gijs de Boer, Hugh Morrison, Matthew Shupe, R. Hildner. 2011
210 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/0ec30b348433f67e8aea01b892ed98fb547bd014
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Jason A. Milbrandt
- Hugh Morrison
- Jennifer E. Kay
- G. Cesana
- Rodanthi-Elisavet Mamouri
- H. Chepfer
- Albert Ansmann
- Gijs de Boer
In Global and Planetary Change
- Jason A. Milbrandt
- Hugh Morrison
- Jennifer E. Kay
- G. Cesana
- Rodanthi-Elisavet Mamouri
- H. Chepfer
- Albert Ansmann
- Gijs de Boer
Citations in the corpus
- Ubiquitous low‐level liquid‐containing Arctic clouds: New observations and climate model constraints from CALIPSO‐GOCCP (2012, result): “[ 9 ] Over the high northern latitude oceans, most liquid-containing clouds occur below 3 km and at temperatures between (cid:5) 25 and 0 (cid:1) C (Figures 2a and 2c), a result that is similar to available ground-based observations [e.g., de Boer et al. , 2011; Shupe , 2011, Figure 3].”
- Parameterization of Cloud Microphysics Based on the Prediction of Bulk Ice Particle Properties. Part I: Scheme Description and Idealized Tests (2015, background): “Given recent evidence for limited deposition nucleation in relatively warm conditions (Ansmann et al. 2009; de Boer et al. 2011), it is limited to conditions with T# 258:15K and ice supersaturation Si $ 5%.”
- Overview of Ice Nucleating Particles (2017, background): “have been proposed (Fletcher 1959) and used (Pruppacher andKlett 1997) but confirmed to be too high by Fletcher (1969). Using deposition mode experiments on kaolinite particles, more recently Welti et al.”
- Potential of polarization lidar to provide profiles of CCN- and INP-relevant aerosol parameters (2015, background): “…radar observations) can be used to continuously monitor the evolution of clouds in their natural environment, at given meteorological conditions with high vertical and temporal reso-60 lution (Illingworth et al., 2007; Shupe, 2007; Ansmann et al., 2009; de Boer et al., 2011; Schmidt et al., 2014).”