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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| Published in | Scale in Spatial Information and Analysis pp. 143 - 160 |
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| Main Authors | , , |
| Format | Book Chapter |
| Language | English |
| Published |
United States
CRC Press
2014
Taylor & Francis Group |
| Subjects | |
| Online Access | Get full text |
| ISBN | 9781439829370 1439829373 |
| DOI | 10.1201/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. |
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| ISBN: | 9781439829370 1439829373 |
| DOI: | 10.1201/b16751-11 |