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<article language="en">
	<journal>
		<journal_title>Advances in Geosciences</journal_title>
		<journal_url>www.adv-geosci.net</journal_url>
		<issn>1680-7340</issn>
		<eissn>1680-7359</eissn>
		<volume_number>21</volume_number>
		<volume_title>Transdisciplinary concepts and modelling strategies for the assessment of complex environmental systems</volume_title>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/adgeo-21-125-2009</doi>
	<article_url>http://www.adv-geosci.net/21/125/2009/</article_url>
	<abstract_html>http://www.adv-geosci.net/21/125/2009/adgeo-21-125-2009.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/21/125/2009/adgeo-21-125-2009.pdf</fulltext_pdf>
	<start_page>125</start_page>
	<end_page>130</end_page>
	<publication_date>2009-08-12</publication_date>
	<article_title content_type="html">Hydrologic comparison between a lowland catchment (Kielstau, Germany) and a mountainous catchment (XitaoXi, China) using KIDS model in PCRaster</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>X. Zhang</name>
			<email>xzhang@hydrology.uni-kiel.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>G. Hörmann</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>N. Fohrer</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Ecology Centre, Department of Hydrology and Water Resources Management, Christian-Albrechts-University of Kiel, Olshausenstr. 75, 24118 Kiel, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The KIDS model (Kielstau Discharge Simulation model) is a simple
rainfall-runoff model developed originally for the Kielstau catchment. To
extend its range of application we applied it to a completely different
catchment, the XitaoXi catchment in China. Kielstau is a small (51 km&lt;sup&gt;2&lt;/sup&gt;)
lowland basin in Northern Germany, with large proportion of wetland area.
And XitaoXi is a mesoscale (2271 km&lt;sup&gt;2&lt;/sup&gt;) mountainous basin in the south of
China. Both catchments differ greatly in size, topography, landuse, soil
properties, and weather conditions. We compared two catchments in these
features and stress on the analysis how the specific catchment
characteristics could guide the adaptation of KIDS model and the parameter
estimation for streamflow simulation. The Nash and Sutcliffe coefficient was
0.73 for Kielstau and 0.65 for XitaoXi. The results suggest that the
application of KIDS model may require adjustments according to the specific
physical background of the study basin.</abstract>
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</article>

