The structure of the twilight ray in different spectral regions
Bigg's report (Bigg 1959) on his having distinctly detected isolated stratiform cloud, situated at an altitude of 10 km, with the help of twilight observations using 6000-8000 A light is of great interest. In the present article we should like to dis-cuss some questions of twilight phenomena theory, and in particular, to touch on the problem of solar radiation absorption by water vapour in the earth's atmosphere.
How to Cite
Copyright (c) 2021 MAUSAM
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
All articles published by MAUSAM are licensed under the Creative Commons Attribution 4.0 International License. This permits anyone.
Anyone is free:
- To Share - to copy, distribute and transmit the work
- To Remix - to adapt the work.
Under the following conditions:
- Share - copy and redistribute the material in any medium or format
- Adapt - remix, transform, and build upon the material for any purpose, even