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Kadlec, R. H., Williams, R. B., & Scheffe, R. D. (1988). Wetland evapotranspiration in temperate and arid climates. In The Ecology and Management of Wetlands: Volume 1: Ecology of Wetlands (pp. 146–160). New York, NY: Springer US. 
Added by: Christoph Külls (2024-05-29 19:33:05)   
Resource type: Book Article
DOI: 10.1007/978-1-4684-8378-9_12
ID no. (ISBN etc.): 978-1-4684-8378-9
BibTeX citation key: Kadlec1988
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Categories: Ecology, Hydrology
Creators: Kadlec, Scheffe, Williams
Publisher: Springer US (New York, NY)
Collection: The Ecology and Management of Wetlands: Volume 1: Ecology of Wetlands
Views: 122/127
Views index: 93%
Popularity index: 23.25%
Attachments   URLs   https://doi.org/10 ... 8-1-4684-8378-9_12
Water losses to the atmosphere from wetlands are a combination of evaporation and transpiration by emergent macrophytes. Wetland surfaces may be permanently or periodically saturated, with periods of shallow standing water. A variable fraction of the surface area may be occupied by open water. The soil surface may be bare or covered by a litter layer that forms an effective mulch.
Added by: Christoph Külls  
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