Deep convective clouds with sustained supercooled liquid water down to -37.5 °C

By Daniel Rosenfeld, W. Woodley. Nature, 2000

508 citations recorded by the source corpus.

Subfields: Atmospheric Science, Earth-Surface Processes, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/5c48433acce562fbd52c900b8502bebf108c1539

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Citations in the corpus

Aerosol invigoration and restructuring of Atlantic convective clouds (2005, background): “Citation: Koren, I., Y. J. Kaufman, D. Rosenfeld,”
Representation of microphysical processes in cloud‐resolving models: Spectral (bin) microphysics versus bulk parameterization (2015, background): “…in thunderstorm anvils around the level of homogeneous freezing, can intensify hail and graupel riming and foster lightning formation in clouds [Rosenfeld and Woodley, 2000; Heymsfield et al., 2009; Khain et al., 2012], etc. Brenguier and Grabowski [1993] reported the bimodality of DSD caused…”
A technique for quantifying heterogeneous ice nucleation in microlitre supercooled water droplets (2014, background): “Cloud droplets can supercool to temperatures below −37 ◦C (Rosenfeld and Woodley, 2000) but can freeze at much warmer temperatures in the presence of ice-nucleating particles (INPs).”
Global indirect aerosol effects: a review (2004, unknown): “Rosenfeld (1999) and Rosenfeld and Woodley (2000) analyzed aircraft data together with satellite data suggesting that pollution aerosols suppress precipitation by decreasing cloud droplet size.”
Lightning enhancement over major oceanic shipping lanes (2017, background): “…lead to more numerous but smaller cloud drops [Ramanathan et al., 2001], which leads to suppressed or delayed warm rain formation, and thus potentially more water transported to the colder upper atmosphere if continued uplift is sustained by dynamics or thermodynamics [Rosenfeld and Woodley, 2000].”
Notes on state-of-the-art investigations of aerosol effects on precipitation: a critical review (2009, methodology): “As it was shown by Rosenfeld and Woodley (2000), Khain et al (2001), Khain and Pokrovsky (2004) and Khain et al (2008a), the strong atmospheric instability and high AP concentration typical of these clouds lead to the formation of a significant amount of ice crystals by homogeneous freezing.”
Tropospheric water vapor, convection, and climate (2010, background): “Also, freezing nuclei are sufficiently rare in the atmosphere that liquid droplets usually must cool well below 0°C to freeze, sometimes even to −35°C or so, where homogeneous freezing (that in the absence of nuclei) rapidly begins [Rosenfeld and Woodley, 2000].”
The Chisholm firestorm: observed microstructure, precipitation and lightning activity of a pyro-cumulonimbus (2006, background): “Phys., 7, 645–659, 2007 www.atmos-chem-phys.net/7/645/2007/ homogeneous freezing level still in liquid form were already observed in much less extreme convection (Rosenfeld and Woodley, 2000) as well as in severe hailstorms (Rosenfeld et al., 2006).”