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Impact of land use and land cover transitions and climate on evapotranspiration in the Lake Naivasha Basin, Kenya

机译:土地利用和土地覆盖过渡与气候对肯尼亚湖纳瓦莎盆地蒸散的影响

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The Lake Naivasha Basin in Kenya has experienced significant land use cover changes (LUCC) that has been hypothesized to have altered the hydrological regime in recent decades. While it is generally recognized that LUCC will impact evapotranspiration (ET), the precise nature of such impact is not very well understood. This paper describes how land use conversions among grassland and croplands have influenced ET in the Lake Naivasha Basin for the period 2003 to 2012. MODIS data products were used in combination with the European Centre for Medium-Range Weather Forecasts (ECMWF) data sets to model ET using the Surface Energy Balance System (SEBS). The results indicate that conversions from grassland to cropland accounted for increases in ET of up to 12% while conversion from cropland back to grasslands (abandonment) reduced ET by similar to 4%.This suggests that recently cultivated agricultural lands could increase local water demands, while abandonment of the farms could decrease the water loss and eventually increase the water availability. Also, recovery of ET following reconversion from cropland to grassland might be impeded due to delayed recovery of soil properties since parts of the catchment are continuously being transformed with no ample time given for soil recovery. The annual ET over the 10 years shows an estimated decline from 724 mm to 650 mm (10%). This decline is largely explained by a reduction in net radiation, an increase in actual vapour pressure whose net effect also led to decrease in the surface-air temperature difference. These findings suggest that in order to better understand LUCC effects on water resources of Lake Naivasha, it is important to take into account the effect of LUCC and climate because large scale changes of vegetation type from grassland to cropland substantially will increase evapotranspiration with implications on the water balance. (C) 2019 Published by Elsevier B.V.
机译:肯尼亚湖纳维莎盆地经历了重大的土地利用封面变化(LUCC),已被假设近几十年来改变了水文制度。虽然人们普遍认识到,Lucc会影响蒸发(ET),但这种影响的确切性质并不是很好地理解。本文介绍了草地和农田在2003年至2012年湖南纳维莎盆地的土地使用程度影响了.MODIS数据产品与欧洲的中距离天气预报(ECMWF)数据集合使用了模型ET使用表面能平衡系统(SEB)。结果表明,从农田回到草地的转变为Gracklands(遗弃)的转换时,Grandland的转换占高达12%的增加,同样减少了4%。这表明最近培养的农业土地可以提高当地水需求,虽然放弃农场可能会降低水分,并最终提高水可用性。此外,由于土壤性质的延迟恢复,因此可能阻碍了在从农田到草地重新转化到草地之后的恢复,因为由于该节目的部位连续转化,因此没有给予土壤恢复的完整时间。 10年内的年度ET显示估计从724毫米达到650毫米(10%)下降。净辐射的降低,这种下降大大解释,实际蒸汽压力的增加,其净效应也导致表面空气温差降低。这些研究结果表明,为了更好地了解LUCC对Naivasha水资源的影响,重要的是考虑LUCC和气候的影响,因为从草地到农作物的植被类型的大规模变化大大增加了蒸发的影响水平衡。 (c)2019年由elestvier b.v发布。

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