scholarly journals Geographically Weighted Area-to-Point Regression Kriging for Spatial Downscaling in Remote Sensing

2018 ◽  
Vol 10 (4) ◽  
pp. 579 ◽  
Author(s):  
Yan Jin ◽  
Yong Ge ◽  
Jianghao Wang ◽  
Gerard Heuvelink ◽  
Le Wang
CATENA ◽  
2018 ◽  
Vol 163 ◽  
pp. 111-122 ◽  
Author(s):  
Yiming Xu ◽  
Scot E. Smith ◽  
Sabine Grunwald ◽  
Amr Abd-Elrahman ◽  
Suhas P. Wani ◽  
...  

2017 ◽  
Vol 20 (1) ◽  
pp. 61-70 ◽  
Author(s):  
Arun Mondal ◽  
Deepak Khare ◽  
Sananda Kundu ◽  
Surajit Mondal ◽  
Sandip Mukherjee ◽  
...  

2021 ◽  
Vol 09 (06) ◽  
pp. 191-202
Author(s):  
Nuan Wang ◽  
Jie Yu ◽  
Lin Zhu ◽  
Yanbing Wang ◽  
Zhengyang He

2018 ◽  
Vol 46 (5) ◽  
pp. 705-716 ◽  
Author(s):  
Navneet Kumar ◽  
Ayyamperumal Velmurugan ◽  
Nicholas A. S. Hamm ◽  
Vinay Kumar Dadhwal

Author(s):  
Q. Wang ◽  
V. Rodriguez-Galiano ◽  
P. M. Atkinson

Remotely sensed land surface temperature (LST) downscaling is an important issue in remote sensing. Geostatistical methods have shown their applicability in downscaling multi/hyperspectral images. In this paper, four geostatistical solutions, including regression kriging (RK), downscaling cokriging (DSCK), kriging with external drift (KED) and area-to-point regression kriging (ATPRK), are applied for downscaling remotely sensed LST. Their differences are analyzed theoretically and the performances are compared experimentally using a Landsat 7 ETM+ dataset. They are also compared to the classical TsHARP method.


2008 ◽  
Vol 2 (No. 4) ◽  
pp. 123-134 ◽  
Author(s):  
J. Balkovič ◽  
G. Čemanová ◽  
J. Kollár ◽  
M. Kromka ◽  
K. Harnová

The paper introduces a method of digital mapping of spatial distribution of soil typological units. It implements fuzzy k-means to classify the soil profile data (study area from the Považsk&yacute; Inovec Mountains, Slovakia) and regression-kriging with the selected digital terrain and remote sensing data to draw membership maps of soil typological units. Totally three soil typological units were identified: Haplic Cambisols (Skeletic, Dystric), Albic Stagnic Luvisols, and Haplic Stagnosols (Albic, Dystric). We analysed the membership values to these units with respect to terrain and remote sensing data. The membership values appeared as spatially smoothly dependant on the terrain gradients (linearly or exponentially) whereas the residua showed spatial autocorrelation. Based on regression and kriging analyses, the regression-kriging model was successfully deployed to draw raster membership maps. These maps yield coefficients of determination between R<sup>2</sup> = 56% (Albic Stagnic Luvisols) to R<sup>2</sup>= 79% (Haplic Cambisols (Skeletic, Dystric)) when evaluated by cross validation. The grid-based continuous soil map represents an alternative to the classical polygon soil maps and can offer a wide range of interpretations for landscape studies.


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