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Titel |
Enhancing the representation of subgrid land surface characteristics in land surface models |
VerfasserIn |
Y. Ke, L. R. Leung, M. Huang, H. Li |
Medientyp |
Artikel
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Sprache |
Englisch
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ISSN |
1991-959X
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Digitales Dokument |
URL |
Erschienen |
In: Geoscientific Model Development ; 6, no. 5 ; Nr. 6, no. 5 (2013-09-27), S.1609-1622 |
Datensatznummer |
250084996
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Publikation (Nr.) |
copernicus.org/gmd-6-1609-2013.pdf |
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Zusammenfassung |
Land surface heterogeneity has long been recognized as important to
represent in the land surface models. In most existing land surface models,
the spatial variability of surface cover is represented as subgrid
composition of multiple surface cover types, although subgrid topography
also has major controls on surface processes. In this study, we developed a
new subgrid classification method (SGC) that accounts for variability of
both topography and vegetation cover. Each model grid cell was represented
with a variable number of elevation classes and each elevation class was
further described by a variable number of vegetation types optimized for
each model grid given a predetermined total number of land response units
(LRUs). The subgrid structure of the Community Land Model (CLM) was used to
illustrate the newly developed method in this study. Although the new method
increases the computational burden in the model simulation compared to the
CLM subgrid vegetation representation, it greatly reduced the variations of
elevation within each subgrid class and is able to explain at least 80%
of the total subgrid plant functional types (PFTs). The new method was also
evaluated against two other subgrid methods (SGC1 and SGC2) that assigned
fixed numbers of elevation and vegetation classes for each model grid (SGC1:
M elevation bands–N PFTs method; SGC2: N PFTs–M elevation bands method). Implemented at
five model resolutions (0.1°, 0.25°, 0.5°,
1.0°and 2.0°) with three maximum-allowed total number
of LRUs (i.e., NLRU of 24, 18 and 12) over North America
(NA), the new method yielded more computationally efficient subgrid
representation compared to SGC1 and SGC2, particularly at coarser model
resolutions and moderate computational intensity (NLRU = 18).
It also explained the most PFTs and elevation variability that is more
homogeneously distributed spatially. The SGC method will be implemented in
CLM over the NA continent to assess its impacts on simulating land surface
processes. |
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