<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.nonlin-processes-geophys.net/inc/npg/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Nonlinear Processes  in Geophysics</journal_title>
		<journal_url>www.nonlin-processes-geophys.net</journal_url>
		<issn>1023-5809</issn>
		<eissn>1607-7946</eissn>
		<volume_number>3</volume_number>
		<issue_number>1</issue_number>
		<publication_year>1996</publication_year>
	</journal>
	<doi>10.5194/npg-3-23-1996</doi>
	<article_url>http://www.nonlin-processes-geophys.net/3/23/1996/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/3/23/1996/npg-3-23-1996.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/3/23/1996/npg-3-23-1996.pdf</fulltext_pdf>
	<start_page>23</start_page>
	<end_page>28</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">A spectral model for turbulence and microphysics dynamics in an ice cloud</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. J. Palmer</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">NOAA, Environmental Technology Laboratory, 325 Broadway, Boulder, CO 80303, USA</affiliation>
	</affiliations>
	<abstract content_type="html">A  one-dimensional,  nine-mode 
spectral  model  for
          temperature, velocity, and  the mixing ratios of
suspended  and
          precipitating   ice-particle   components  is   shown  
to   be
          consistent   with  ice-cloud   observations.  The 
observations
          include  Doppler radar  time-series  measurements of  a 
single
          winter ice cloud and  direct measurements of mean
particle size
          vs.  icewater content for a  set of ice  clouds. Fitting
of the
          model to  the Doppler vertical-velocity  measurements
allows  a
          prediction to  be  made  of the  vertical  scale and 
turbulent
          Prandtl number  active in the  ice-cloud vertical
motions.  The
          model is  then used to explore  the question  of how
turbulence
          and gravity-wave  motions affect  the microphysical 
properties
          of  an ice  cloud.  The  model predicts  interesting 
dynamical
          effects  on the  mixing  ratios due  to  these motions, 
but no
          significant   effects   on  the   time-averaged  
microphysical
          quantities.</abstract>
	<references>
	</references>
</article>

