Abstract
Changes in global albedo of the Earth can depend on regional variations in reflectivity. We compare here three regional factors that have been considered capable of causing significant changes in global albedo, representing them approximately by zonal averages. Our calculations suggest that
(1) large latitudinal changes in ice cover will have only a slight effect on the planetary albedo, and
(2) latitudinal shifts in the cloud belts can produce significant changes in the planetary albedo.
DOI: https://doi.org/10.3402/tellusa.v31i2.10422 | Journal eISSN: 3035-9554
Language: English
Page range: 170 - 173
Submitted on: Jul 18, 1978
Published on: Jan 1, 1979
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1979 A. Henderson-Sellers, A. J. Meadows, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.
