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Field Data Introduction to Remote Sensing Instructor: Dr. Cheng-Chien LiuCheng-Chien Liu Department of Earth Sciences National Cheng Kung University Last updated: 27 October 2004 Chapter 5
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Outline Introduction Information of field data Field radiometry Tutorial/demonstration of handheld spectroradiometer Basic radiometric quantities and definitions Location information Tutorial/demonstration of handheld GPS Geographic sampling
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Introduction Field data Necessary for remote sensing Establish relationship between ground truth and imagery Validation Evaluation Expensive Purpose-oriented Content Method
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Information of field data Attributes/measurements of ground conditions Nominal data e.g. crop identification, land use, … Biophysical data Moisture content, Leaf area index (LAI), … Radiometry data Location and size Time and date Ancillary data Weather, illumination, calibration of instrument, persons who collect data
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Field radiometry Handheld spectroradiometer Constitution (Fig 1.14a or see Campbell 2002 Fig 12-4) Pointing device Fiber-optical cable Measuring unit Detector Filter Display unit Data log Measurement Radiance Reflectance
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Tutorial/demonstration of handheld spectroradiometer Software installation Hardware installation Calibration Data log Data processing Implementation (Fig 1.14b and Fig 1.15, or see Campbell 2002 Fig 12-9)
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Basic radiometric quantities and definitions Spherical coordinate Spherical coordinate Spherical coordinate Measurement of radiance L Definition of L Measurement of planar irradiance E Definition of E Measurement of scalar irradiance E 0 Definition of E 0 Definition of reflectance R = E u /E d Definition of remote sensing reflectance R rs =L u /E d
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Locational information Observations need locational information Method Reference to distinctive landmarks Valid for well-mapped regions Global Positioning System (GPS)
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Global Positioning System Satellite Orbit Working principle Receiver Accuracy Selective availability (SA)
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Geographic sampling Terminology Observation Sample Three considerations Number of observations Sampling pattern Spacing of observations
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Geographic sampling (cont.) Number of observations The larger the sample size, the closer to the actual values Minimum number assigned to each class Sampling pattern Simple random sampling pattern Stratified random pattern Systematic patterns Systematic stratified unaligned pattern Cluster sampling Spacing of observations
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Homework We are going to employ the handheld spectroradiometer and GPS receiver to collect field data of vegetation in the watershed of Chen-Yo-Lan River. Please help us to integrate these instruments on (1) Shoulder (2) Suzuki grand Vitara (3) unmanned helicopter
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Homework (cont.) The reflectance of a standard white board is given in Table 1. The field measurements of the standard white board and the sample are shown in Table 2, respectively. Please use this information to calculate the reflectance of the sample. Wavelength (nm)400.26450.33500550.23600.21650.19700.04 White board352.265838.2652607.9522902.2652397.9521751.9521015.265 Sample12.93429.93484.929254.934124.92956.92991.934 Wavelength (nm)400450500550600650700 Reflectance0.455 0.4580.4610.4640.4670.471 Table 1 Table 2
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Source
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Fig. 2.3.1 Definition of the polar coordinates ( , ) and of the upward ( u ) and downward ( d ) hemispheres of directions. Reprint from Figure 1.3 in (Mobley 1994). Fig 2.3.1
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Fig. 2.3.2 Fig. 2.3.2 Schematic design of an instrument for measuring un-polarized spectral radiance. Reprint from Figure 1.5 in (Mobley 1994).
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2.3 Basic radiometric quantities and definitions (cont.) Radiance L:
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Fig. 2.3.3 Fig. 2.3.3 Schematic design of an instrument for measuring un-polarized spectral downwelling planar irradiance. Reprint from Figure 1.6 in (Mobley 1994).
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2.3 Basic radiometric quantities and definitions (cont.) Downwelling planar irradiance E d :
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Fig. 2.3.4 Fig. 2.3.4 Schematic design of an instrument for measuring un-polarized spectral downwelling scalar irradiance. Reprint from Figure 1.7 in (Mobley 1994).
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2.3 Basic radiometric quantities and definitions (cont.) Downwelling scalar irradiance E 0d :
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