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Image-Based Atmospheric Corrections - Revisited and Improved

Authors:
  • Northern Arizona University (retired USGS)

Abstract

A major benefit of multitemporal, remotely sensed images is their applicability to change detection over time.(...) However, to maximize the usefulness of data from multitemporal point of view, an easy-to-use, cost-efective, and accurate radiometric calibration and correction procedure is needed.
... The analysis utilized the Landsat 8 OLI dataset, incorporating seven bands, namely blue, green, red, near-infrared (NIR), short-wave infrared-1 (SWIR1), short-wave infrared-2 (SWIR2), and thermal infrared of band 10. Radiometric correction was carried out employing Chavez's full model correction method (Chavez 1996;Eastman, 2019), as illustrated in Figure 2, which outlines the research methodology. Subsequently, the terrain attribute maps were integrated into the optical image dataset (blue -SWIR plus thermal bands) to serve as input for the multisource classification. ...
... The correction used full atmospheric correction to derive new dataset with 0 − 1.0 range of at surface reflectance. The equation of full atmospheric correction was based on the work of Chavez (1996) as follows: ...
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... While atmospheric transmittances and solar irradiance cancel each other in the ratio, the haze terms should be preliminarily estimated and removed. Path-radiance estimation may follow image-based approaches [30], [31] or rely on radiative transfer models of the atmosphere and its constituents [32], as well as knowledge of acquisition parameters, such as actual Sun-Earth distance, solar zenith angle, and satellite platform observation angle. The haze term is trivially zero for data in surface reflectance format, whenever they are available. ...
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... After preprocessed with georeference, and clipping via boundary in Erdas 9.2, it was performed in ENVI to calculate the radiometric calibration value for each band (Chander and Markham, 2003;Xu, 2015). Then, a COST model was used for atmospheric correction to the image (Chavez, 1996;Xu, 2015). ...
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Exploring how water bodies work on the thermal environment in a real and complex urban context is of great significance to develop urban blue infrastructure (BI) system for climate adaption. Previous studies mainly focused on the water cool island (WCI) effect in the microenvironment, which cannot provide enough evidence for systematic application. This study explored the cooling effect of water bodies on the urban environment in Wuhan, China based on three scenarios in which water bodies was regarded as individual samples, water network system and one landscape category of urban ecosystem, respectively. Results indicate that all detected water bodies expressed WCI effect with the mean WCI intensity of 5.5°C and the range of 1.1°C to 13.3°C. The main factors influencing the cooling effect of urban water body system were Percent of landscape (PLAND_W), Landscape shape index (LSI_W) and Contrast-weighted edge density (CWED_W) of water bodies, which could explain 69.0% of urban LST variation. An urban water body system with relatively larger water area, more regular boundary and simpler surroundings might be more efficient in cooling the urban environment. Nevertheless, when considering the interaction of water bodies with other land covers on thermal environment, the contribution of water bodies to the cooling benefit was depressed. The main factors were Similarity index_mean of Construction land (SIMI_MN_C), Class area of Construction land (CA_C), Total edge contrast index of Water body (TECI_W), Landscape shape index of Water body (LSI_W) and Percent of landscape of Vegetated area (PLAND_V). They combined to explain 71.9% of LST variation in urban areas. Developing an urban BI system by connecting the dispersed water bodies and fragmenting the contiguous construction land in rapidly urbanized areas can be more realistic for mitigating UHI effect and adapting to climate change.
... Atmospheric correction was conducted to obtain the surface reflectance values. The method for removing path radiance in images is the dark object subtraction (DOS) technique developed by Chavez (1996), which is applied to the TOA reflectance of the WorldView-3 image (Equation 1). ...
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