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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>7</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-14675-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/14675/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/14675/2007/acpd-7-14675-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/14675/2007/acpd-7-14675-2007.pdf</fulltext_pdf>
	<start_page>14675</start_page>
	<end_page>14706</end_page>
	<publication_date>2007-10-15</publication_date>
	<article_title content_type="html">Introduction of prognostic rain in ECHAM5: design and Single Column Model simulations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. Posselt</name>
			<email>rebekka.posselt@env.ethz.ch</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>U. Lohmann</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute for Atmospheric and Climate Science, ETH Zurich, Universitaetsstrasse 16, 8092 Zurich, Switzerland</affiliation>
	</affiliations>
	<abstract content_type="html">Prognostic equations for the rain mass mixing ratio and the rain drop
number concentration are introduced into the large-scale cloud
microphysics parameterization of the ECHAM5 general circulation model
(ECHAM5-RAIN). For this a rain flux from one level to the next with
the appropriate fall speed is introduced. This maintains rain water
in the atmosphere to be available for the next time step. Rain
formation in ECHAM5-RAIN is, therefore, less dependent on the
autoconversion rate than the standard ECHAM5 but shifts the emphasis
towards the accretion rates in accordance with observations.
ECHAM5-RAIN is tested and evaluated with two cases: the continental
mid-latitude ARM Cloud IOP (shallow frontal cloud case &amp;ndash; March 2000)
and EPIC (a marine stratocumulus study &amp;ndash; October 2001). The prognostic
equations for rain hardly affect the amount and timing of
precipitation at the surface in different Single Column Model (SCM)
simulations for heavy precipitating clouds because heavy rain depends
mainly on the large-scale forcing. In case of thin, drizzling clouds
(i.e., stratocumulus), an increase in surface precipitation is caused
by more sub-time steps used in the prognostic rain scheme until
convergence is reached. Cloud microphysical quantities, such as liquid
and rain water, are more sensitive to the number of sub-time steps for
light precipitation.  This results from the decreasing autoconversion
rate and increasing accretion rate.</abstract>
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