611 research outputs found

    Effects of atmospheric, topographic, and BRDF correction on imaging spectroscopy-derived data products

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    Surface reflectance is an important data product in imaging spectroscopy for obtaining surface information. The complex retrieval of surface reflectance, however, critically relies on accurate knowledge of atmospheric absorption and scattering, and the compensation of these effects. Furthermore, illumination and observation geometry in combination with surface reflectance anisotropy determine dynamics in retrieved surface reflectance not related to surface absorption properties. To the best of authorsโ€™ knowledge, no comprehensive assessment of the impact of atmospheric, topographic, and anisotropy effects on derived surface information is available so far.This study systematically evaluates the impact of these effects on reflectance, albedo, and vegetation products. Using three well-established processing schemes (ATCOR F., ATCOR R., and BREFCOR), high-resolution APEX imaging spectroscopy data, covering a large gradient of illumination and observation angles, are brought to several processing states, varyingly affected by mentioned effects. Pixel-wise differences of surface reflectance, albedo, and spectral indices of neighboring flight lines are quantitatively analyzed in their respective overlapping area. We found that compensation of atmospheric effects reveals actual anisotropy-related dynamics in surface reflectance and derived albedo, related to an increase in pixel-wise relative reflectance and albedo differences of more than 40%. Subsequent anisotropy compensation allows us to successfully reduce apparent relative reflectance and albedo differences by up to 20%. In contrast, spectral indices are less affected by atmospheric and anisotropy effects, showing relative differences of 3% to 10% in overlapping regions of flight lines.We recommend to base decisions on the use of appropriate processing schemes on individual use cases considering envisioned data products

    A STUDY ON THE EFFECTS OF VIEWING ANGLE VARIATION IN SUGARCANE RADIOMETRIC MEASURES

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    Remote Sensing techniques, such as field spectroscopy provide information with a large level of detail about spectral characteristics of plants enabling the monitoring of crops. The aim of this study is to analyze the influence of viewing angle in estimating the Bidirectional Reflectance Distribution Function (BRDF) for the case of sugarcane. The study on the variation of the spectral reflectance profile can help the improvement of algorithms for correction of BRDF in remote sensing images. Therefore, spectral measurements acquired on nadir and different off-nadir view angle directions were considered in the experiments. Change both anisotropy factor and anisotropy index was determined in order to evaluate the BRDF variability in the spectral data of sugarcane. BRDF correction was applied using the Walthall model, thus reducing the BRDF effects. From the results obtained in the experiments, the spectral signatures showed a similar spectral pattern varying mainly in intensity. The anisotropy factor which showed a similar pattern in all wavelengths. The visual analysis of the spectral reflectance profile of sugarcane showed variation mainly in intensity at different angles. The use of Walthall model reduced the BRDF effects and brought the spectral reflectance profiles acquired on different viewing geometry close to nadir viewing. Therefore, BRDF effects on remote sensing data of vegetation cover can be minimized by applying this model. This conclusion contributes to developing suitable algorithms to produce radiometrically calibrated mosaics with remote sensing images taken by aerial platforms

    Impact of multiangular information on empirical models to estimate canopy nitrogen concentration in mixed forest

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    Directional effects in remotely sensed reflectance data can influence the retrieval of plant biophysical and biochemical estimates. Previous studies have demonstrated that directional measurements contain added information that may increase the accuracy of estimated plant structural parameters. Because accurate biochemistry mapping is linked to vegetation structure, also models to estimate canopy nitrogen concentration (CN) may be improved indirectly from using multiangular data. Hyperspectral imagery with five different viewing zenith angles was acquired by the spaceborne CHRIS sensor over a forest study site in Switzerland. Fifteen canopy reflectance spectra corresponding to subplots of field-sampled trees were extracted from the preprocessed CHRIS images and subsequently two-term models were developed by regressing CN on four datasets comprising either original or continuum-removed reflectances. Consideration is given to the directional sensitivity of the CN estimation by generating regression models based on various combinations (n=15) of observation angles. The results of this study show that estimating canopy CN with only nadir data is not optimal irrespective of spectral data processing. Moreover adding multiangular information improves significantly the regression model fits and thus the retrieval of forest canopy biochemistry. These findings support the potential of multiangular Earth observations also for application-oriented ecological monitoring

    NASA's surface biology and geology designated observable: A perspective on surface imaging algorithms

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    The 2017โ€“2027 National Academies' Decadal Survey, Thriving on Our Changing Planet, recommended Surface Biology and Geology (SBG) as a โ€œDesignated Targeted Observableโ€ (DO). The SBG DO is based on the need for capabilities to acquire global, high spatial resolution, visible to shortwave infrared (VSWIR; 380โ€“2500 nm; ~30 m pixel resolution) hyperspectral (imaging spectroscopy) and multispectral midwave and thermal infrared (MWIR: 3โ€“5 ฮผm; TIR: 8โ€“12 ฮผm; ~60 m pixel resolution) measurements with sub-monthly temporal revisits over terrestrial, freshwater, and coastal marine habitats. To address the various mission design needs, an SBG Algorithms Working Group of multidisciplinary researchers has been formed to review and evaluate the algorithms applicable to the SBG DO across a wide range of Earth science disciplines, including terrestrial and aquatic ecology, atmospheric science, geology, and hydrology. Here, we summarize current state-of-the-practice VSWIR and TIR algorithms that use airborne or orbital spectral imaging observations to address the SBG DO priorities identified by the Decadal Survey: (i) terrestrial vegetation physiology, functional traits, and health; (ii) inland and coastal aquatic ecosystems physiology, functional traits, and health; (iii) snow and ice accumulation, melting, and albedo; (iv) active surface composition (eruptions, landslides, evolving landscapes, hazard risks); (v) effects of changing land use on surface energy, water, momentum, and carbon fluxes; and (vi) managing agriculture, natural habitats, water use/quality, and urban development. We review existing algorithms in the following categories: snow/ice, aquatic environments, geology, and terrestrial vegetation, and summarize the community-state-of-practice in each category. This effort synthesizes the findings of more than 130 scientists

    Scaling Estimates of Vegetation Structure in Amazonian Tropical Forests Using Multi-Angle MODIS Observations

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    Detailed knowledge of vegetation structure is required for accurate modelling of terrestrial ecosystems, but direct measurements of the three dimensional distribution of canopy elements, for instance from LiDAR, are not widely available. We investigate the potential for modelling vegetation roughness, a key parameter for climatological models, from directional scattering of visible and near-infrared (NIR) reflectance acquired from NASA's Moderate Resolution Imaging Spectroradiometer (MODIS). We compare our estimates across different tropical forest types to independent measures obtained from: (1) airborne laser scanning (ALS), (2) spaceborne Geoscience Laser Altimeter System (GLAS)/ICESat, and (3) the spaceborne SeaWinds/QSCAT. Our results showed linear correlation between MODIS-derived anisotropy to ALS-derived entropy (r(exp 2)= 0.54, RMSE= 0.11), even in high biomass regions. Significant relationships were also obtained between MODIS-derived anisotropy and GLAS-derived entropy(0.52 less than or equal to r(exp 2) less than or equal to 0.61; p less than 0.05), with similar slopes and offsets found throughout the season, and RMSE between 0.26 and 0.30 (units of entropy). The relationships between the MODIS-derived anisotropy and backscattering measurements (sigma(sup 0)) from SeaWinds/QuikSCAT presented an r(exp 2) of 0.59 and a RMSE of 0.11. We conclude that multi-angular MODIS observations are suitable to extrapolate measures of canopy entropy across different forest types, providing additional estimates of vegetation structure in the Amazon

    a Berlin case study

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    Durch den Prozess der Urbanisierung verรคndert die Menschheit die Erdoberflรคche in groรŸem AusmaรŸ und auf unwiederbringliche Weise. Die optische Fernerkundung ist eine Art der Erdbeobachtung, die das Verstรคndnis dieses dynamischen Prozesses und seiner Auswirkungen erweitern kann. Die vorliegende Arbeit untersucht, inwiefern hyperspektrale Daten Informationen รผber Versiegelung liefern kรถnnen, die der integrierten Analyse urbaner Mensch-Umwelt-Beziehungen dienen. Hierzu wird die Verarbeitungskette von Vorverarbeitung der Rohdaten bis zur Erstellung referenzierter Karten zu Landbedeckung und Versiegelung am Beispiel von Hyperspectral Mapper Daten von Berlin ganzheitlich untersucht. Die traditionelle Verarbeitungskette wird mehrmals erweitert bzw. abgewandelt. So wird die radiometrische Vorverarbeitung um die Normalisierung von Helligkeitsgradienten erweitert, welche durch die direktionellen Reflexionseigenschaften urbaner Oberflรคchen entstehen. Die Klassifikation in fรผnf spektral komplexe Landnutzungsklassen wird mit Support Vector Maschinen ohne zusรคtzliche Merkmalsextraktion oder Differenzierung von Subklassen durchgefรผhrt...thesi

    ๋“œ๋ก ์„ ํ™œ์šฉํ•œ ์œ„์„ฑ ์ง€ํ‘œ๋ฐ˜์‚ฌ๋„ ์‚ฐ์ถœ๋ฌผ ๊ณต๊ฐ„ ํŒจํ„ด ๋ถ„์„

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    ํ•™์œ„๋…ผ๋ฌธ(์„์‚ฌ) -- ์„œ์šธ๋Œ€ํ•™๊ต๋Œ€ํ•™์› : ๋†์—…์ƒ๋ช…๊ณผํ•™๋Œ€ํ•™ ์ƒํƒœ์กฐ๊ฒฝยท์ง€์—ญ์‹œ์Šคํ…œ๊ณตํ•™๋ถ€(์ƒํƒœ์กฐ๊ฒฝํ•™), 2021.8. ์กฐ๋Œ€์†”.High-resolution satellites are assigned to monitor land surface in detail. The reliable surface reflectance (SR) is the fundamental in terrestrial ecosystem modeling so the temporal and spatial validation is essential. Usually based on multiple ground control points (GCPs), field spectroscopy guarantees the temporal continuity. Due to limited sampling, however, it hardly illustrates the spatial pattern. As a map, the pixelwise spatial variability of SR products is not well-documented. In this study, we introduced drone-based hyperspectral image (HSI) as a reference and compared the map with Sentinel 2 and Landsat 8 SR products on a heterogeneous rice paddy landscape. First, HSI was validated by field spectroscopy and swath overlapping, which assured qualitative radiometric accuracy within the viewing geometry. Second, HSI was matched to the satellite SRs. It involves spectral and spatial aggregation, co-registration and nadir bidirectional reflectance distribution function (BRDF)-adjusted reflectance (NBAR) conversion. Then, we 1) quantified the spatial variability of the satellite SRs and the vegetation indices (VIs) including NDVI and NIRv by APU matrix, 2) qualified them pixelwise by theoretical error budget and 3) examined the improvement by BRDF normalization. Sentinel 2 SR exhibits overall good agreement with drone HSI while the two NIRs are biased up to 10%. Despite the bias in NIR, the NDVI shows a good match on vegetated areas and the NIRv only displays the discrepancy on built-in areas. Landsat 8 SR was biased over the VIS bands (-9 ~ -7.6%). BRDF normalization just contributed to a minor improvement. Our results demonstrate the potential of drone HSI to replace in-situ observation and evaluate SR or atmospheric correction algorithms over the flat terrain. Future researches should replicate the results over the complex terrain and canopy structure (i.e. forest).์›๊ฒฉํƒ์‚ฌ์—์„œ ์ง€ํ‘œ ๋ฐ˜์‚ฌ๋„(SR)๋Š” ์ง€ํ‘œ์ •๋ณด๋ฅผ ๋น„ํŒŒ๊ดด์ ์ด๊ณ  ์ฆ‰๊ฐ์ ์ธ ๋ฐฉ๋ฒ•์œผ๋กœ ์ „๋‹ฌํ•ด์ฃผ๋Š” ๋งค๊ฐœ์ฒด ์—ญํ• ์„ ํ•œ๋‹ค. ์‹ ๋ขฐํ•  ์ˆ˜ ์žˆ๋Š” SR์€ ์œก์ƒ ์ƒํƒœ๊ณ„ ๋ชจ๋ธ๋ง์˜ ๊ธฐ๋ณธ์ด๊ณ , ์ด์— ๋”ฐ๋ผ SR์˜ ์‹œ๊ณต๊ฐ„์  ๊ฒ€์ฆ์ด ์š”๊ตฌ๋œ๋‹ค. ์ผ๋ฐ˜์ ์œผ๋กœ SR์€ ์—ฌ๋Ÿฌ ์ง€์ƒ ๊ธฐ์ค€์ (GCP)์„ ๊ธฐ๋ฐ˜์œผ๋กœ ํ•˜๋Š” ํ˜„์žฅ ๋ถ„๊ด‘๋ฒ•์„ ํ†ตํ•ด์„œ ์‹œ๊ฐ„์  ์—ฐ์†์„ฑ์ด ๋ณด์žฅ๋œ๋‹ค. ๊ทธ๋Ÿฌ๋‚˜ ํ˜„์žฅ ๋ถ„๊ด‘๋ฒ•์€ ์ œํ•œ์ ์ธ ์ƒ˜ํ”Œ๋ง์œผ๋กœ ๊ณต๊ฐ„ ํŒจํ„ด์„ ๊ฑฐ์˜ ๋ณด์—ฌ์ฃผ์ง€ ์•Š์•„, ์œ„์„ฑ SR์˜ ํ”ฝ์…€ ๋ณ„ ๊ณต๊ฐ„ ๋ณ€๋™์„ฑ์€ ์ž˜ ๋ถ„์„๋˜์ง€ ์•Š์•˜๋‹ค. ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ๋“œ๋ก  ๊ธฐ๋ฐ˜์˜ ์ดˆ๋ถ„๊ด‘ ์˜์ƒ(HSI)์„ ์ฐธ๊ณ ์ž๋ฃŒ๋กœ ๋„์ž…ํ•˜์—ฌ, ์ด๋ฅผ ์ด์งˆ์ ์ธ ๋…ผ ๊ฒฝ๊ด€์—์„œ Sentinel 2 ๋ฐ Landsat 8 SR๊ณผ ๋น„๊ตํ•˜์˜€๋‹ค. ์šฐ์„ , ๋“œ๋ก  HSI๋Š” ํ˜„์žฅ ๋ถ„๊ด‘๋ฒ• ๋ฐ ๊ฒฝ๋กœ ์ค‘์ฒฉ์„ ํ†ตํ•ด์„œ ๊ด€์ธก๊ฐ๋„ ๋ฒ”์œ„ ๋‚ด์—์„œ ์ •์„ฑ์ ์ธ ๋ฐฉ์‚ฌ ์ธก์ •์„ ๋ณด์žฅํ•œ๋‹ค๊ณ  ๊ฒ€์ฆ๋˜์—ˆ๋‹ค. ์ดํ›„, ๋“œ๋ก  HSI๋Š” ์œ„์„ฑ SR์˜ ๋ถ„๊ด‘๋ฐ˜์‘ํŠน์„ฑ, ๊ณต๊ฐ„ํ•ด์ƒ๋„ ๋ฐ ์ขŒํ‘œ๊ณ„๋ฅผ ๊ธฐ์ค€์œผ๋กœ ๋งž์ถฐ์กŒ๊ณ , ๊ด€์ธก ๊ธฐํ•˜๋ฅผ ํ†ต์ผํ•˜๊ธฐ ์œ„ํ•ด์„œ ๋“œ๋ก  HIS์™€ ์œ„์„ฑ SR์€ ๊ฐ๊ฐ ์–‘๋ฐฉํ–ฅ๋ฐ˜์‚ฌ์œจ๋ถ„ํฌํ•จ์ˆ˜ (BRDF) ์ •๊ทœํ™” ๋ฐ˜์‚ฌ๋„ (NBAR)๋กœ ๋ณ€ํ™˜๋˜์—ˆ๋‹ค. ๋งˆ์ง€๋ง‰์œผ๋กœ, 1) APU ํ–‰๋ ฌ์œผ๋กœ ์œ„์„ฑ SR๊ณผ NDVI, NIRv๋ฅผ ํฌํ•จํ•˜๋Š” ์‹์ƒ์ง€์ˆ˜(VI)์˜ ๊ณต๊ฐ„๋ณ€๋™์„ฑ์„ ์ •๋Ÿ‰ํ™” ํ–ˆ๊ณ , 2) ๋Œ€๊ธฐ๋ณด์ •์˜ ์ด๋ก ์  ์˜ค์ฐจ๋ฅผ ๊ธฐ์ค€์œผ๋กœ SR๊ณผ VI๋ฅผ ํ”ฝ์…€๋ณ„๋กœ ํ‰๊ฐ€ํ–ˆ๊ณ , 3) BRDF ์ •๊ทœํ™”๋ฅผ ํ†ตํ•œ ๊ฐœ์„  ์‚ฌํ•ญ์„ ๊ฒ€ํ† ํ–ˆ๋‹ค. Sentinel 2 SR์€ ๋“œ๋ก  HSI์™€ ์ „๋ฐ˜์ ์œผ๋กœ ์ข‹์€ ์ผ์น˜๋ฅผ ๋ณด์ด๋‚˜, ๋‘ NIR ์ฑ„๋„์€ ์ตœ๋Œ€ 10% ํŽธํ–ฅ๋˜์—ˆ๋‹ค. NIR์˜ ํŽธํ–ฅ์€ ์‹์ƒ์ง€์ˆ˜์—์„œ ํ† ์ง€ ํ”ผ๋ณต์— ๋”ฐ๋ผ ๋‹ค๋ฅธ ์˜ํ–ฅ์„ ๋ฏธ์ณค๋‹ค. NDVI๋Š” ์‹์ƒ์—์„œ๋Š” ๋‚ฎ์€ ํŽธํ–ฅ์„ ๋ณด์—ฌ์คฌ๊ณ , NIRv๋Š” ๋„์‹œ์‹œ์„ค๋ฌผ ์˜์—ญ์—์„œ๋งŒ ๋†’์€ ํŽธํ–ฅ์„ ๋ณด์˜€๋‹ค. Landsat 8 SR์€ VIS ์ฑ„๋„์— ๋Œ€ํ•ด ํŽธํ–ฅ๋˜์—ˆ๋‹ค (-9 ~ -7.6%). BRDF ์ •๊ทœํ™”๋Š” ์œ„์„ฑ SR์˜ ํ’ˆ์งˆ์„ ๊ฐœ์„ ํ–ˆ์ง€๋งŒ, ๊ทธ ์˜ํ–ฅ์€ ๋ถ€์ˆ˜์ ์ด์—ˆ๋‹ค. ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ํ‰ํƒ„ํ•œ ์ง€ํ˜•์—์„œ ๋“œ๋ก  HSI๊ฐ€ ํ˜„์žฅ ๊ด€์ธก์„ ๋Œ€์ฒดํ•  ์ˆ˜ ์žˆ๊ณ , ๋”ฐ๋ผ์„œ ์œ„์„ฑ SR์ด๋‚˜ ๋Œ€๊ธฐ๋ณด์ • ์•Œ๊ณ ๋ฆฌ์ฆ˜์„ ํ‰๊ฐ€ํ•˜๋Š”๋ฐ ํ™œ์šฉ๋  ์ˆ˜ ์žˆ๋‹ค๋Š” ๊ฒƒ์„ ๋ณด์˜€๋‹ค. ํ–ฅํ›„ ์—ฐ๊ตฌ์—์„œ๋Š” ์‚ฐ๋ฆผ์œผ๋กœ ๋Œ€์ƒ์ง€๋ฅผ ํ™•๋Œ€ํ•˜์—ฌ, ์ง€ํ˜•๊ณผ ์บ๋…ธํ”ผ ๊ตฌ์กฐ๊ฐ€ ๋“œ๋ก  HSI ๋ฐ ์œ„์„ฑ SR์— ๋ฏธ์น˜๋Š” ์˜ํ–ฅ์„ ๋ถ„์„ํ•  ํ•„์š”๊ฐ€ ์žˆ๋‹ค.Chapter 1. Introduction 1 1.1 Background 1 Chapter 2. Method 3 2.1 Study Site 3 2.2 Drone campaign 4 2.3 Data processing 4 2.3.1 Sensor calibration 5 2.3.2 Bidirectional reflectance factor (BRF) calculation 7 2.3.3 BRDF correction 7 2.3.4 Orthorectification 8 2.3.5 Spatial Aggregation 9 2.3.6 Co-registration 10 2.4 Satellite dataset 10 2.4.2 Landsat 8 12 Chapter 3. Result and Discussion 12 3.1 Drone BRF map quality assessment 12 3.1.1 Radiometric accuracy 12 3.1.2 BRDF effect 15 3.2 Spatial variability in satellite surface reflectance product 16 3.2.1 Sentinel 2B (10m) 17 3.2.2 Sentinel 2B (20m) 22 3.2.3 Landsat 8 26 Chapter 4. Conclusion 28 Supplemental Materials 30 Bibliography 34 Abstract in Korean 43์„

    Uncertainty Analysis for Input Parameters of the Atmospheric Compensation Process in Airborne Imaging Spectroscopy.

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    In airborne imaging spectroscopy for the Visible Shortwave Infrared (VSWIR) wavelength range the state of the atmosphere can have a large influence on the values detected by optical sensors like APEX or AVIRIS NG. Since the value of interest is the reflectance property of the surface, atmospheric effects need to be compensated for. Atmospheric compensation algorithms like ATCOR-4 use radiance images as input data. In theory, the algorithm would then estimates the hemispherical-directional reflectance factor as a function of radiance intensity minus the influence of atmospheric particles and processes. Assuming the atmospheric parameters to be independent of the radiance intensity, a higher obtained radiance would necessarily lead to a higher estimated reflectance factor. The atmospheric compensation, however, is not a linear function and therefore the resulting images might show errors. This thesis presents an uncertainty analysis for the radiance intensity as one of several independent and non-independent input parameters and variables of ATCOR-4. The analysis is done by modelling the radiance images with factors drawn from a normal probability distribution and simulating the corresponding reflectance factor images with consideration of various other parameters and variables. Generally, the resulting HDRF can be found to have a wavelength dependent standard uncertainty of 0 to 0.15% associated with the radiance intensity. The uncertainty values are put into perspective by showing how other factors like a) the solar reference spectrum, b) the solar azimuth and zenith angle, c) the sensor uncertainty, d) different steps within the atmospheric compensation process, e) the choice of terrain mode in ATCOR-4 and f) the adjacency effect do all have an influence on the HDRF as well
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