首页> 外文会议>第21届国际摄影测量与遥感大会(ISPRS 2008)论文集 >USING REMOTE SENSING DATA TO MODEL GROUNDWATER RECHARGE POTENTIAL IN KANYE REGION, BOTSWANA
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USING REMOTE SENSING DATA TO MODEL GROUNDWATER RECHARGE POTENTIAL IN KANYE REGION, BOTSWANA

机译:使用遥感数据对博茨瓦纳坎耶地区的地下水补给潜力进行建模

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This study focuses on the groundwater recharge potential in the upper Limpopo catchment starting from Kanye region in South Botswana. Existing high resolution remote sensing data were used to estimate the spatial distribution of potential recharge and discharge of aquifers in this semi-arid region. 29 NOAA AVHRR images available for Southern and Central Botswana between 1996 and 2000 were analyzed to produce 29 Kc maps. The comparison of Kc maps in wet and dry seasons shows similar patterns over the upper Limpopo catchment in Kanye region. The conclusion can be drawn that the Kc pattern does not significantly change with time over the region. Therefore the time averaged Kc map can be used together with a map of potential evapotranspiration to calculate actual evapotranspiration for the period 1996-2005. Ten year averages of actual evapotranspiration and precipitation together with the averaged discharge of the catchment to the Limpopo River are then used to calculate a potential recharge/discharge map using the water balance equation. The problem of passing from the potential recharge/discharge map to the actual recharge/discharge map will have to be solved in future research.
机译:这项研究的重点是从博茨瓦纳南部的坎耶地区开始的林波波河上游流域的地下水补给潜力。现有的高分辨率遥感数据被用来估计该半干旱地区含水层的潜在补给和排泄的空间分布。分析了1996年至2000年期间在博茨瓦纳南部和中部可获得的29张NOAA AVHRR图像,生成了29张Kc图。比较干季和湿季的Kc图,在坎耶地区林波波河上游流域的相似模式。可以得出结论,该区域的Kc模式不会随时间显着变化。因此,可以将时间平均Kc图与潜在蒸散量图一起使用,以计算1996-2005年期间的实际蒸散量。然后,使用十年的实际蒸散量和降水量的平均值以及流域到林波波河的平均流量,使用水平衡方程式来计算潜在的补给量/流量图。从潜在的充/放电图转换到实际的充/放电图的问题将在未来的研究中得到解决。

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