isprsarchives XL 7 W3 871 2015
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In consideration of the spatial resolution of these sensors and the size of the target, with the aid of data measured with optical sensor onboard GF-1
The goal of this paper is to compare the utility of Multi-Track HDS-InSAR permafrost surface deformation monitoring using C- and X-band SAR data both
(2012) to calculate the annual average shoreline on dynamic beaches through information provided by the Landsat satellite data, and comparing the results with those
These are the land use map, the map soil morphology and sand cover map (extracted from the map of land) that constitute the basic maps that will serve to establish
Some examples are provided on the infor- mation extracted from satellite data by the GHSL project, includ- ing preliminary results obtained from the processing of the global
KEY WORDS: Small Satellite Constellation, Infrared Instruments, High Temperature Events, impact on the climatic processes, Bi- Spectral Method, Advanced On Board
of the Terra/Aqua satellite (“MODIS lines”). The system in eq. 2 is over determined, thus it can be solved by a least-square technique. The geocentric Cartesian coordinates of
In the M 4 Land system, SLC is configured to use spectral configurations and acquisition parameters from the used satellite sensors (in this case RapidEye),
