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Meteorological impact assessment of possible large scale irrigation in Southwest Saudi Arabia

机译:西南沙特阿拉伯可能进行大规模灌溉的气象影响评估

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On continental to regional scales feedbacks between landuse and landcover change and climate have been widely documented over the past 10-15 years. In the present study we explore the possibility that also vegetation changes over much smaller areas may affect local precipitation regimes. Large scale (~ 10~5 ha) irrigated plantations in semi-arid environments under particular conditions may affect local circulations and induce additional rainfall. Capturing this rainfall 'surplus' could then reduce the need for external irrigation sources and eventually lead to self-sustained water cycling. This concept is studied in the coastal plains in South West Saudi Arabia where the mountains of the Asir region exhibit the highest rainfall of the peninsula due to orographic lifting and condensation of moisture imported with the Indian Ocean monsoon and with disturbances from the Mediterranean Sea. We use a regional atmospheric modeling system (RAMS) forced by ECMWF analysis data to resolve the effect of complex surface conditions in high resolution (Δx=4 km). After validation, these simulations are analysed with a focus on the role of local processes (sea breezes, orographic lifting and the formation of fog in the coastal mountains) in generating rainfall, and on how these will be affected by large scale irrigated plantations in the coastal desert. The validation showed that the model simulates the regional and local weather reasonably well. The simulations exhibit a slightly larger diurnal temperature range than those captured by the observations, but seem to capture daily sea-breeze phenomena well. Monthly rainfall is well reproduced at coarse resolutions, but appears more localized at high resolutions. The hypothetical irrigated plantation (3.25 10~5 ha) has significant effects on atmospheric moisture, but due to weakened sea breezes this leads to limited increases of rainfall, hi terms of recycling of irrigation gifts the rainfall enhancement in this particular setting is rather insignificant.
机译:在大陆到区域范围内,过去10到15年间,土地利用,土地覆盖变化和气候之间的反馈已得到广泛记录。在本研究中,我们探索了在较小区域内的植被变化也可能影响当地降水状况的可能性。在特定条件下在半干旱环境中进行大规模(〜10〜5公顷)灌溉人工林可能会影响当地的环流并引起额外的降雨。捕获降雨的“盈余”可以减少对外部灌溉源的需求,并最终导致水循环的自我维持。在沙特阿拉伯西南部的沿海平原上研究了这一概念,在此地区,阿西尔地区的山脉由于半岛地形的抬升和印度洋季风输入的水分的凝结以及地中海的干扰而表现出最高的半岛降雨量。我们使用由ECMWF分析数据强迫的区域大气建模系统(RAMS)来解决高分辨率(Δx= 4 km)中复杂地表条件的影响。验证之后,将对这些模拟进行分析,重点关注局部过程(海风,地形抬升和沿海山区雾的形成)在产生降雨中的作用,以及这些因素将如何受到当地大型灌溉人工林的影响。沿海沙漠。验证表明,该模型可以较好地模拟区域和本地天气。模拟显示的昼夜温度范围比观测值大,但似乎可以很好地捕获日常海风现象。在较粗的分辨率下,月降水量再现良好,而在较高分辨率的情况下,显得更为局限。假设的灌溉人工林(3.25 10〜5公顷)对大气湿度有显着影响,但是由于海风减弱,这导致降雨增加有限。就灌溉礼品的回收而言,在这种特殊环境下的降雨增加微不足道。

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