Diurnal Variation of Soil Heat Flux at an Antarctic Local Area during Warmer Months

Soil heat flux (G) is one term in the energy balance equation, and it can be particularly important in regions with arid, bare, or thinly vegetated soil surfaces. However, in remote areas such as the Antarctic, this measurement is not routinely performed. The analysis of observational data collected...

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Bibliographic Details
Published in:Applied and Environmental Soil Science
Main Authors: Marco Alves, Jacyra Soares
Format: Article in Journal/Newspaper
Language:English
Published: Hindawi Limited 2016
Subjects:
geo
Eta
Online Access:https://doi.org/10.1155/2016/1769203
https://doaj.org/article/86f5fee621ab4d878e3f4e1638d69580