Overview
In arid and semi-arid areas, the main contributions to land surface processes are precipitation, surface evaporation and surface energy balancing. In the close-to-surface layer and root-zone layer, vapor flux is the dominant flux controlling these processes - process which, in turn, influence the local climate pattern and the local ecosystem. The work reported in this thesis attempts to understand how the soil airflow affects the vapor transport during evaporation processes, by using a two-phase heat and mass transfer model. The necessity of including the airflow mechanism in land surface process studies is discussed and highlighted.
Full Product Details
Publisher: Springer
Imprint: Springer
ISBN: 9781283935333
ISBN 10: 1283935333
Pages: 175
Publication Date: 01 January 2013
Audience:
General/trade
,
General
Format: Undefined
Publisher's Status: Active
Availability: Available To Order

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