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<front>
<journal-meta>
<journal-id journal-id-type="publisher">GMDD</journal-id>
<journal-title-group>
<journal-title>Geoscientific Model Development Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">GMDD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1991-962X</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/gmdd-5-1041-2012</article-id>
<title-group>
<article-title>TopoSUB: a tool for efficient large area numerical modelling in complex topography at sub-grid scales</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fiddes</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gruber</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Glaciology, Geomorphodynamics &amp; Geochronology, Department of Geography, University of Zurich, Switzerland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>02</day>
<month>05</month>
<year>2012</year>
</pub-date>
<volume>5</volume>
<issue>2</issue>
<fpage>1041</fpage>
<lpage>1076</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
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<abstract>
<p>Mountain regions are highly sensitive to global climate change. However,
large scale assessments of mountain environments remain problematic due to
the high resolution required of model grids to capture strong lateral
variability. To alleviate this, tools are required to bridge the scale gap
between gridded climate datasets (climate models and re-analyses) and
unresolved (by coarse grids) sub-grid mountain topography. We address this
problem with a sub-grid method. It relies on sampling the most important
aspects of land surface heterogeneity through a lumped scheme, allowing for
the application of numerical land surface models (LSM) over large areas in
mountain regions. This is achieved by including the effect of mountain
topography on these processes at the sub-grid scale using a multidimensional
informed sampling procedure together with a 1-D lumped model that can be
driven by gridded climate datasets. This paper provides a description of this
sub-grid scheme, TopoSUB, as well as assessing its performance against a
distributed model. We demonstrate the ability of TopoSUB to approximate
results simulated by a distributed numerical LSM at around 10&lt;sup&gt;4&lt;/sup&gt; less
computations. These significant gains in computing resources allow for: (1)
numerical modelling of processes at fine grid resolutions over large areas;
(2) extremely efficient statistical descriptions of sub-grid behaviour; (3) a
&quot;sub-grid aware&quot; aggregation of simulated variables to course grids; and (4)
freeing of resources for treatment of uncertainty in the modelling process.</p>
</abstract>
<counts><page-count count="36"/></counts>
</article-meta>
</front>
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