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2012 | OriginalPaper | Buchkapitel

2. Moisture and Heat

verfasst von : Prof. Dr. Ming-ko Woo

Erschienen in: Permafrost Hydrology

Verlag: Springer Berlin Heidelberg

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Abstract

Under a cold climate, water exists in solid, liquid and gaseous states at, above and below the surface. Water can undergo change of state on time scales that vary from hours to days and seasons, to multi-year periods. Phase change involves energy and thus energy balance plays a major role in the detention or the release of water to runoff and river flow. Hinzman et al. (1991) stated that the thermal and moisture regimes are closely related to each other and to the characteristics of the active layer and therefore have a marked influence on permafrost dynamics. This chapter reviews briefly the fundamentals of moisture and heat fluxes at the atmospheric boundary layer and below-ground.

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Titel: Moisture and Heat
verfasst von: Prof. Dr. Ming-ko Woo
Verlag: Springer Berlin Heidelberg
Buch: Permafrost Hydrology
Print ISBN: 978-3-642-23461-3

Electronic ISBN: 978-3-642-23462-0

Copyright-Jahr: 2012
DOI: https://doi.org/10.1007/978-3-642-23462-0_2