Abstract
For many practical purposes, the air of the lower atmosphere can be considered as a mixture of perfect gases; in the present context these may conveniently be assumed to be dry air of constant composition and water vapor.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 1982 Springer Science+Business Media Dordrecht
About this chapter
Cite this chapter
Brutsaert, W. (1982). The Lower Atmosphere. In: Evaporation into the Atmosphere. Environmental Fluid Mechanics, vol 1. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-1497-6_3
Download citation
DOI: https://doi.org/10.1007/978-94-017-1497-6_3
Publisher Name: Springer, Dordrecht
Print ISBN: 978-90-481-8365-4
Online ISBN: 978-94-017-1497-6
eBook Packages: Springer Book Archive