Abstract
From the author’s formula for the relative radiation as a function of temperature and humidity conditions in the atmosphere, a formula is deduced for the zenith distance variation of the effective radiation. This formula is compared with observational data and empirical formulae. Finally, the constancy of the representative zenith distance, for which the effective radiation equals the effective radiation integrated over the whole hemisphere, is investigated.
DOI: https://doi.org/10.3402/tellusa.v3i3.8633 | Journal eISSN: 3035-9554
Language: English
Page range: 148 - 153
Published on: Jan 1, 1951
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1951 Olov Lönnqvist, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.