Methods for Scaling Gridded Data

Scaling or change of scale is important for information transfer across scales, wherever analysis, modeling, or applications are performed on scales different from those of the given datasets, models, or problem domains (Gelfand et al. 2001; Hufkens et al. 2008). As in previous chapters, we focus on...

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Bibliographic Details
Published inScale in Spatial Information and Analysis pp. 143 - 160
Main Authors Zhang, Jingxiong, Atkinson, Peter, Goodchild, Michael F.
Format Book Chapter
LanguageEnglish
Published United States CRC Press 2014
Taylor & Francis Group
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Online AccessGet full text
ISBN9781439829370
1439829373
DOI10.1201/b16751-11

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Summary:Scaling or change of scale is important for information transfer across scales, wherever analysis, modeling, or applications are performed on scales different from those of the given datasets, models, or problem domains (Gelfand et al. 2001; Hufkens et al. 2008). As in previous chapters, we focus on methods for (spatial) scaling of spatial data. Chapter 6 described geostatistical approaches to change of scale: upscaling can be performed through block kriging, whereas downscaling can be implemented using block-to-point (or larger support-to-smaller support) kriging, respectively. For downscaling, geostatistical inverse modeling approaches may be usefully explored and provide a motivation for this chapter, as both are explicitly oriented to gridded data, such as images and raster data. Below, we review briefly the geostatistical methods for scaling before moving to the cases of gridded lattice data, highlighting the complementarity of methods covered in Chapters 6 and 7.
ISBN:9781439829370
1439829373
DOI:10.1201/b16751-11