scholarly journals Camera Calibration Using Projective Invariants of Sphere Images

IEEE Access ◽  
2020 ◽  
Vol 8 ◽  
pp. 28324-28336
Author(s):  
Fengli Yang ◽  
Yue Zhao ◽  
Xuechun Wang
Keyword(s):  
Camera Calibration ◽  
Projective Invariants

Fish-eye camera calibration using horizontal and vertical laser planes projected from a laser level

2019 ◽  
Vol 2019 (9) ◽  
pp. 374-1-374-6
Author(s):  
Yen-Chou Tai ◽  
Yu-Hsiang Chiu ◽  
Yi-Yu Hsieh ◽  
Yong-Sheng Chen ◽  
Jen-Hui Chuang
Keyword(s):  
Camera Calibration ◽  
Laser Level ◽  
Fish Eye

Detecting Asymmetric Cropping Based on Camera Calibration

2013 ◽  
Vol 34 (10) ◽  
pp. 2409-2414 ◽  
Author(s):  
Xian-zhe Meng ◽  
Shao-zhang Niu ◽  
Xiao-mei Wu ◽  
Ye-zhou Li
Keyword(s):  
Camera Calibration

scholarly journals Two Independent Light Dilution Corrections for the SO2 Camera Retrieve Comparable Emission Rates at Masaya Volcano, Nicaragua

2021 ◽  
Vol 13 (5) ◽  
pp. 935
Author(s):  
Matthew Varnam ◽  
Mike Burton ◽  
Ben Esse ◽  
Giuseppe Salerno ◽  
Ryunosuke Kazahaya ◽  
...  
Keyword(s):  
Light Scattering ◽  
Optical Depth ◽  
Camera Calibration ◽  
Wind Direction ◽  
Emission Rate ◽  
Emission Rates ◽  
Depth Images ◽  
Masaya Volcano ◽  
Rapid Changes ◽  
Volcanic Emission

SO2 cameras are able to measure rapid changes in volcanic emission rate but require accurate calibrations and corrections to convert optical depth images into slant column densities. We conducted a test at Masaya volcano of two SO2 camera calibration approaches, calibration cells and co-located spectrometer, and corrected both calibrations for light dilution, a process caused by light scattering between the plume and camera. We demonstrate an advancement on the image-based correction that allows the retrieval of the scattering efficiency across a 2D area of an SO2 camera image. When appropriately corrected for the dilution, we show that our two calibration approaches produce final calculated emission rates that agree with simultaneously measured traverse flux data and each other but highlight that the observed distribution of gas within the image is different. We demonstrate that traverses and SO2 camera techniques, when used together, generate better plume speed estimates for traverses and improved knowledge of wind direction for the camera, producing more reliable emission rates. We suggest combining traverses and the SO2 camera should be adopted where possible.

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