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Ibérica na região de Trás-os-Montes (NE Portugal) - Universidade ...

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Ca<strong>de</strong>rn<strong>os</strong> Lab. Xeolóxico <strong>de</strong> Laxe<br />

Coruña. 2001. Vol. 26, pp. 179-190<br />

ISSN: 0213-4497<br />

Ge<strong>os</strong>tatistical interpolation of<br />

topographical field data in or<strong>de</strong>r to obtain a<br />

DEM of a small forest catchment in<br />

Northwest Spain<br />

Interpolación geoestadística <strong>de</strong> dat<strong>os</strong><br />

topográfic<strong>os</strong> para obtener un MED <strong>de</strong> u<strong>na</strong><br />

pequeña cuenca forestal en el noroeste <strong>de</strong><br />

España<br />

A B S T R A C T<br />

THONON, I. 1 & CACHEIRO POSE, M. 2<br />

This article gives an example of the elaboration of a digital elevation mo<strong>de</strong>l (DEM) with<br />

the aid of ge<strong>os</strong>tatistics, using the case of a small experimental catchment near Arc<strong>os</strong> <strong>de</strong><br />

la Con<strong>de</strong>sa in Galicia, Spain. A DEM is a necessary tool in present-day er<strong>os</strong>ion and landscape<br />

mo<strong>de</strong>lling. The ge<strong>os</strong>tatistical method of DEM construction involves six steps, starting<br />

with the removal of the drift and ending with the fi<strong>na</strong>l interpolation. The drift was<br />

alm<strong>os</strong>t completely elimi<strong>na</strong>ted by a first or<strong>de</strong>r trend surface. After it had been confirmed<br />

that no heter<strong>os</strong>cedacity is present in the data set, the resulting experimental variogram<br />

was fitted by an anisotropic Gaussian variogram mo<strong>de</strong>l, which is the variogram mo<strong>de</strong>l<br />

that is generally used for DEM interpolation. Cr<strong>os</strong>s validation was used to <strong>de</strong>termine the<br />

optimal number of data points to be used in interpolation. The interpolation results<br />

were found to be satisfactory and the interpolation standard <strong>de</strong>viations are below the<br />

data set standard <strong>de</strong>viation. It is yet noted that this uncertainty in the DEM – although<br />

small – may influence its <strong>de</strong>rivatives and subsequent mo<strong>de</strong>l results. However, when

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