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<!DOCTYPE article SYSTEM "http://www.hydrol-earth-syst-sci.net/inc/hess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences</journal_title>
		<journal_url>www.hydrol-earth-syst-sci.net</journal_url>
		<issn>1027-5606</issn>
		<eissn>1607-7938</eissn>
		<volume_number>13</volume_number>
		<issue_number>11</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/hess-13-2233-2009</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/13/2233/2009/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/13/2233/2009/hess-13-2233-2009.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/13/2233/2009/hess-13-2233-2009.pdf</fulltext_pdf>
	<start_page>2233</start_page>
	<end_page>2240</end_page>
	<publication_date>2009-11-25</publication_date>
	<article_title content_type="html">Extracting statistical parameters of extreme precipitation from a NWP model</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. Eliasson</name>
			<email>jonase@hi.is</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>O. Rögnvaldsson</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>T. Jonsson</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">University of Iceland, Institute of Environmental and Civil Engineering, Iceland</affiliation>
		<affiliation numeration="2" content_type="html">Institute for Meteorological Research, Reykjavik, Iceland</affiliation>
		<affiliation numeration="3" content_type="html">Icelandic Meteorological Office, Iceland</affiliation>
	</affiliations>
	<abstract content_type="html">Precipitation simulations on an 8&amp;times;8 km grid using the PSU/NCAR
Mesoscale Model MM5 are used to estimate the M5 and C&lt;sub&gt;i&lt;/sub&gt; statistical
parameters in order to support the M5 map used for flood estimates by
Icelandic engineers. It is known a priori that especially wind anomalies
occur on a considerably smaller scale than 8 km. The simulation period used
is 1962–2005 and 73 meteorological stations have records long enough in
this period to provide a validation data set. Of these only one station is
in the central highlands, so the highland values of the existing M5 map are
estimates. A comparison between the simulated values and values based on
station observations set shows an M5 average difference
(observed-simulated) of &amp;minus;5 mm/24 h with a standard deviation of 17 mm,
3 outliers excluded. This is within expected limits, computational and
observational errors considered. A suggested correction procedure brings
these values down to 4 mm and 11 mm, respectively.</abstract>
	<references>
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</article>

