Last update: Sat Oct 14 03:06:25 MDT 2017
@Article{Wettlaufer:2000:MBZ,
author = "John S. Wettlaufer and J. Greg Dash",
title = "Melting Below Zero",
journal = j-SCI-AMER,
volume = "282",
number = "2",
pages = "50--53",
month = feb,
year = "2000",
CODEN = "SCAMAC",
DOI = "https://doi.org/10.1038/scientificamerican0200-50",
ISSN = "0036-8733 (print), 1946-7087 (electronic)",
ISSN-L = "0036-8733",
bibdate = "Fri May 17 10:26:11 MDT 2013",
bibsource = "http://www.math.utah.edu/pub/tex/bib/sciam2000.bib;
http://www.sciam.com/2000/0200issue/0200quicksummary.html",
URL = "http://www.nature.com/scientificamerican/journal/v282/n2/pdf/scientificamerican0200-50.pdf",
abstract = "Even well below the freezing point, ice is coated with
a microscopic film of quasiliquid water because of a
process called surface melting. The dynamics of the
water in this film do more than make ice slippery. They
also cause destructive frost heaves and unleash
lightning from the clouds.",
acknowledgement = ack-nhfb,
fjournal = "Scientific American",
journal-URL = "http://www.nature.com/scientificamerican",
}