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| Title: | Evaporation and the water balance |
| Authors: | Kelliher, Francis M. Jackson, R. Sturman, A.P. Spronken-Smith, R.A. |
| Issue Date: | 2001 |
| Citation: | Kelliher, Francis M. and Jackson, Rick (2001) Evaporation and the water balance. In Sturman, A.P. and Spronken-Smith, R. A. (Ed.). The Physical Environment: A New Zealand Perspective (pp. 113-129). Melbourne: Oxford University Press. |
| Abstract: | In New Zealand most water reaches the land surface as rain. Some rain evaporates
after being caught on the surfaces of plants (a process called interception), but the rest
reaches the ground and usually soaks into the soil. Water in the soil is extracted by
plants through their roots and, after passing through the stems and branches, evaporates
through tiny leaf pores known as stomata, in the process called transpiration.
Water also evaporates from the moist surface of the soil at a rate determined by energy
availability, surface wetness, nature of the vegetation, and the availability of soil
water. |
| Publisher: | Oxford University Press University of Canterbury. Geography |
| Research Fields: | Fields of Research::260000 Earth Sciences Fields of Research::260000 Earth Sciences::260500 Hydrology |
| URI: | http://hdl.handle.net/10092/3770 |
| Rights URI: | http://library.canterbury.ac.nz/ir/rights.shtml |
| Appears in Collections: | Chapters and Books
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