2010
DOI: 10.1111/j.1538-4632.2009.00780.x
|View full text |Cite
|
Sign up to set email alerts
|

Geography, Spatial Data Analysis, and Geostatistics: An Overview. 地理学、空间数据分析及地统计学:综述

Abstract: Geostatistics is a distinctive methodology within the field of spatial statistics. In the past, it has been linked to particular problems (e.g., spatial interpolation by kriging) and types of spatial data (attributes defined on continuous space). It has been used more by physical than human geographers because of the nature of their types of data. The approach taken by geostatisticians has several features that distinguish it from the methods typically used by human geographers for analyzing spatial variation … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
41
0
3

Year Published

2011
2011
2020
2020

Publication Types

Select...
5
4
1

Relationship

0
10

Authors

Journals

citations
Cited by 65 publications
(44 citation statements)
references
References 108 publications
0
41
0
3
Order By: Relevance
“…Visual and geomorphometric landform analysis both implicate continuity between elevation data points, inevitably ignoring the DEM's fractal characteristics. This is feasible because terrain height also possesses a high level of positive autocorrelation for small distances, sufficiently reflecting the assumption of continuity (Hunter and Goodchild, 1997;Ehlschlaeger, 1998;Gallay, 2009;Haining et al, 2010). According to the Nyquist-Shannon sampling theorem, the intrinsic resolution of a raster DEM is twice the sampling distance of the height values actually measured for DEM generation, whereas the double of the DEM posting represents the nominal resolution (Robinson, 1994;Florinsky, 1998;Fisher and Tate, 2006;Arrell et al, 2008).…”
Section: Introductionmentioning
confidence: 97%
“…Visual and geomorphometric landform analysis both implicate continuity between elevation data points, inevitably ignoring the DEM's fractal characteristics. This is feasible because terrain height also possesses a high level of positive autocorrelation for small distances, sufficiently reflecting the assumption of continuity (Hunter and Goodchild, 1997;Ehlschlaeger, 1998;Gallay, 2009;Haining et al, 2010). According to the Nyquist-Shannon sampling theorem, the intrinsic resolution of a raster DEM is twice the sampling distance of the height values actually measured for DEM generation, whereas the double of the DEM posting represents the nominal resolution (Robinson, 1994;Florinsky, 1998;Fisher and Tate, 2006;Arrell et al, 2008).…”
Section: Introductionmentioning
confidence: 97%
“…The kriging interpolation method (Haining et al, 2010) was chosen as it allows to estimate the empirical semivariogram according to the values, distance and reliability of surrounding points until an established maximum distance from the starting point. The distribution of input data, as represented in the histogram, was at first normalized using the arcsin function in order to obtain a regular Gaussian distribution.…”
Section: Representativeness Area Assessmentmentioning
confidence: 99%
“…Ordinary kriging (OK) was employed to generate rainfall maps, because it is the simplest and most straightforward method that accounts for the local variability of the stochastic process, rainfall in this case (Cressie, 1990;Haining et al, 2010). Kriging is ideally suited for interpolation of highly irregularly spaced data points.…”
Section: Rainfall Mapsmentioning
confidence: 99%