The results on development of an original method of atmosphere’s transparency determination in the infrared region are presented. The method is a halfempirical and based on the direct nephelometric and meteorological measurements of the atmosphere’s transparency in the visual region (on λ = 0.55 μ ) with following recalculation to the other spectrum region in diapason from 1 μ to 14 μ . The proposed method provides the possibility of the operative valuation “optical weather” in the atmosphere, especially in full-scale tests thermovision equipment and devices of night vision.
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                    Physics                
                        , 2025, Issue 1, pp. 1–10
        
        
        
            ISSN Online: 0000-0000
        
        
        
            DOI:
                            10.xxxx/example-doi