[PDF] Top 20 isprs archives XLII 3 W1 205 2017
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isprs archives XLII 3 W1 205 2017
... 3.3 Possible analog site: Tarim Bain, Xinjiang, China We found landforms similar to Figure 8 in Tarim Basin in Xinjiang, China, where the environment is currently extremely arid and cold. Figure 10A is a sub image of ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 69 2017
... Kirk 2017) and BAE has recently delivered the source code for a CSM version ...of 2017 and are working with BAE to open source the CSM code in early ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 77 2017
... There are two types of lunar domes: mare (ordinary) domes and silicic domes. Mare dome are gentler swells, with elevation difference of about 300 m above the plane surface, often have flank slopes <7°. While domes ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 85 2017
... The k values (Fig.4) of all endmembers were first obtained based on section 3.2. Then the single-scattering albedos of all the minerals were calculated for different particle sizes. Thus, an endmember library including ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 91 2017
... SAfS techniques depend largely on the understanding of reflectance models which describe the relationship between surface orientation and energy response. This research has been long studied and various practical models ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 99 2017
... Besides introducing the classical Root-mean-square height method and Morphological Surface Roughness MSR algorithm, this paper takes the area of the Jurassic mountain uplift in the Sinus[r] ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 105 2017
... Within the D ISTILLATION processes (Figure 2) the core issues are the abstraction of data, the (carto)graphic visualization, and GIS-based management of derived data. We identify three major tasks that are necessary to ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 35 2017
... (Figure 3) that has less thermal inertias, high reflectivity and thick ...Region 3 (Black polygon in the right) is C-level, thus Region 2 and 3 are ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 23 2017
... 20 m fraction, or ~70 Ma, Fassett and Thomson, 2014). Given that the event is estimated at ~110 Ma (Arvidson et al. 1976), the crater count should have approached the background level by now. This discrepancy raises ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 29 2017
... The global adjustment of the multi-mission image and laser altimetry network is based on a combined photogrammetric solution. Three types of tie points (intra-strip tie point linking the stereo images of the same strip, ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 41 2017
... In order to introduce the basic principle of our method in detail, image matching on the third pyramid level of the HRSC Level-3 images was performed with SIFT. The results are presented in Figure 2. The HRSC ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 55 2017
... Liu, 2017), even after precise offline ground calibration in laboratory environment, which further conflicts with a unified camera ...International Archives of the Photogrammetry, Remote Sensing and Spatial ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 49 2017
... Mode Observer, Luenberger observer, Backstepping observer, etc. Attitude determination algorithm obtains satellite attitude information based on observation vectors of star sensor. The attitude determination method does ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 63 2017
... Scambos, T. A., Dutkiewicz, M. J., Wilson, J. C., & Bindschadler, R. A. 1992. Application of image cross- correlation to the measurement of glacier velocity using satellite image data. Remote sensing of environment, ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 213 2017
... average point space (that is to say NPS) is about 3 mm. With regard to the computing the slope index and roughness index, it is vital to consider the number of sampled point lied in each reference grid. Normally ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 177 2017
... With various radiometric pre-processing techniques being pro- posed and developed (Kashani et al., 2015), LiDAR data users reap the benefits of using the monochromatic laser intensity data for surface classification and ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 171 2017
... In order to validate the spatial distribution of minerals, scatterplots of CRISM index values(BD1300, LCPINDEX, OLINDEX)(Viviano-Beck et al., 2014) versus derived major mineral abundance were produced to evaluate the ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 183 2017
... images, which describes the local shape information of impact crater in the optical image and calculate morphological factors mainly including slope and aspect using DEM data and then the multi-scale frequency histograms ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 199 2017
... Crater-detection approaches can be divided into four categories: manual recognition, shape-profile fitting algorithms, machine-learning methods and geological information-based analysis using terrain and spectral data. ... Lihat dokumen lengkap
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isprs archives XLII 3 W1 191 2017
... The realization of the method: The IIM and LROC images are divided into small image blocks, and the manually selected control points are also divided into the corresponding image blocks,[r] ... Lihat dokumen lengkap
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