Effects of the introduction of rice on evapotranspiration in seasonal wetlands |
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| Authors: | Tetsuji Suzuki Takeshi Ohta Tetsuya Hiyama Yasuhiro Izumi Osmund Mwandemele Morio Iijima |
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| Affiliation: | 1. Graduate school of Bioagricultural Sciences, Nagoya University, Nagoya, Japan;2. JST/JICA, SATREPS, Tokyo, Japan;3. Research Institute for Humanity and Nature, Kyoto, Japan;4. School of Environmental Science, The University of Shiga Prefecture, Hikone, Japan;5. Faculty of Agriculture and Natural Resources, University of Namibia, Windhoek, Namibia;6. School of Agriculture, Kinki University, Nara, Japan |
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| Abstract: | Land use changes in wetland areas can alter evapotranspiration, a major component of the water balance, which eventually affects the water cycle and ecosystem. This study assessed the effect of introduced rice‐cropping on evapotranspiration in seasonal wetlands of northern Namibia. By using the Bowen ratio–energy balance method, measurements of evapotranspiration were performed over a period of 2.5 years at two wetland sites—a rice field (RF) and a natural vegetation field (NVF)—and at one upland field (UF) devoid of surface water. The mean evapotranspiration rates of RF (1.9 mm daytime?1) and NVF (1.8 mm daytime?1) were greater than that in UF (1.0 mm daytime?1). RF and NVF showed a slight difference in seasonal variations in evapotranspiration rates. During the dry season, RF evapotranspiration was less than the NVF evapotranspiration. The net radiation in RF was less in this period because of the higher albedo of the non‐vegetated surface after rice harvesting. In the early growth period of rice during the wet season, evapotranspiration in RF was higher than that in NVF, which was attributed to a difference in the evaporation efficiency and the transfer coefficient for latent heat that were both affected by leaf area index (LAI). Evapotranspiration sharply negatively responded to an increase in LAI when surface water is present according to sensitivity analysis, probably because a higher LAI over a surface suppresses evaporation. The control of LAI is therefore a key for reducing evaporation and conserving water. Copyright © 2013 John Wiley & Sons, Ltd. |
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| Keywords: | evapotranspiration land use change leaf area index rice semi‐arid regions wetlands |
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