DocumentCode :
441066
Title :
Further validation for the scaling rule of the spatial independent variables on the basis of the image assimilation and the simultaneous experiment
Author :
Tian, Jing ; Sun, Xiao-Min ; Zhang, Ren-Hua ; Zhu, Zhi-Lin ; Zhou, Yan-Lian ; Xu, Jin-Ping ; Li, Zhao-Liang
Author_Institution :
Inst. of Geophys. Sci. & Natural Resources Res., Chinese Acad. of Sci., Beijing, China
Volume :
1
fYear :
2005
fDate :
25-29 July 2005
Abstract :
In the article, one universal formula presented by RH Zhang (2004) is validated based on the TM image assimilation and the surface simultaneous experiment data which was measured in remote sensing experimental field of Xiaotangshan of Beijing. Several scales was used to study: the first is the experimental field (2 m × 2 m), another is a 30 m × 30 m TM image validated by the experiment data, the others are images degraded using the Landsat TM image. The scaling rule of independent variables defined as those surface parameters whose values are not affected by its neighboring pixels but depend on the characteristics of the pixel itself, such as NDVI, albedo, LAI, surface emissivity and apparent thermal inertia (ATI). They are investigated using the areas composed by farmland, the areas of the same size but different water area fractions, within which the difference of the surface characteristics are obvious. Generally, the independent variables can be expressed as the form of x/y. Therefore, when degrading these parameters, the scaling rule have close relationship with the numerator x and the denominator y. In terms of our analysis, when the denominator yi is the same for the aggregated pixels, there is no scaling difference. However, when yi is variable, the scaling difference is affected by the magnitude of x and y, and the variance of xi (varx) and yi (vary) divided by the average xi (meanx) and yi (meany) can reduce this effect; for a moderate heterogeneous surface, the scaling difference of NDVI, LAI, emissivity and ATI can be ignored, however, for obvious contrasting surface, the scaling difference can lead to large errors; when the meanx, meany, varx and vary are in the same magnitude, it can be considered that there is the same scaling difference regardless of resolution.
Keywords :
data assimilation; geophysical signal processing; image processing; terrain mapping; vegetation mapping; Beijing; China; Landsat TM image; NDVI; Xiaotangshan; albedo; apparent thermal inertia; image assimilation; image resolution; remote sensing; scaling rule; spatial independent variables; surface emissivity; surface parameters; surface simultaneous experiment data; water area fractions; Geophysical measurements; Image processing; Remote sensing; Satellites; Spatial resolution; Sun; Technological innovation; Thermal degradation; Uncertainty; Water;
fLanguage :
English
Publisher :
ieee
Conference_Titel :
Geoscience and Remote Sensing Symposium, 2005. IGARSS '05. Proceedings. 2005 IEEE International
Print_ISBN :
0-7803-9050-4
Type :
conf
DOI :
10.1109/IGARSS.2005.1526265
Filename :
1526265
Link To Document :
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