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Evidence of Urban-Induced Precipitation Variability in Arid Climate Regimes

机译:干旱气候条件下城市诱发的降水变化的证据

摘要

Water is essential to life in the Earth system. The water cycle components that sustain life are becoming more scarce and polluted. The most recent (1999-2004) drought experienced in the southwestern United States is the seventh worst in the approximately 500-year proxy tree-ring record. As a result, many regions contemplated drought emergencies in which severe water restrictions are implemented. Though larger weather and climate processes likely control drought processes, there is increasing evidence that anthropogenic or human-related activities can significantly alter precipitation processes. Urbanization is an example of anthropogenic forcing. Recent studies continue to provide evidence that urban environments can modify or induce precipitation under a specific set of conditions. Arid and semi-arid regions of the southwestern United States and other parts of the world are rapidly developing and placing greater demands on the environmental system. In the past fifty years, Phoenix has expanded from a predominantly agricultural center to an urbanized region with extent 700 percent larger than its size in the middle of the twentieth century. Riyadh's population grew from about a half million people in 1972 to almost two million by 2000. Saudi Arabia experienced urbanization later than many other countries; in the early 1970s its urban-rural ratio was still about 1:3. By 1990 the ratio had reversed to about 3:l. In the mid-1970s Riyadh's population was increasing by about 10 percent a year. Irrigation also significantly increased between 1972 and 1990 southeast of Riyadh. The study employs a 108-year precipitation historical data record, global climate observing network observations and satellite data to identify possible anomalies in rainfall in and around two major arid urban areas, Phoenix, Arizona and Riyadh, Saudi Arabia. It provides statistically sound evidence that rainfall distribution and magnitude is statistically different in post-urban than in pre-urban (1900-1950) Phoenix. The study hypothesis that a complex interaction between the city landscape, irrigated lands, and nearby mountains have created preferred regions for rainfall development. The study also provides early evidence that rapidly urbanizing parts of the arid Middle East may also be experiencing different precipitation regimes in response to urbanization and irrigation.
机译:水对于地球系统中的生命至关重要。维持生命的水循环成分变得越来越稀缺和污染。在美国西南部最近的一次干旱(1999-2004年)在大约500年的代理树年轮记录中排名第七。结果,许多地区考虑到干旱紧急情况,其中实行了严格的用水限制。尽管较大的天气和气候过程可能会控制干旱过程,但越来越多的证据表明,人为活动或与人类有关的活动会大大改变降水过程。城市化是人为强迫的一个例子。最近的研究继续提供证据,证明城市环境可以在特定条件下改变或诱发降水。美国西南部以及世界其他地区的干旱和半干旱地区正在迅速发展,并对环境系统提出了更高的要求。在过去的五十年里,凤凰城已经从一个主要的农业中心扩展到了一个城市化地区,其规模比20世纪中叶的规模大了700%。利雅得的人口从1972年的50万增加到2000年的近200万。沙特阿拉伯的城市化进程比其他许多国家都晚。在1970年代初,其城乡比例仍然约为1:3。到1990年,该比例已逆转至约3:1。在1970年代中期,利雅得的人口以每年约10%的速度增长。 1972年至1990年,利雅得东南部的灌溉也显着增加。这项研究使用了108年的降水历史数据记录,全球气候观测网络的观测数据和卫星数据,以识别两个主要干旱城市地区(亚利桑那州菲尼克斯和沙特阿拉伯利雅得)及其附近地区降雨的可能异常。它提供了统计上可靠的证据,表明市区后的降雨分布和强度与市区前(1900-1950年)的菲尼克斯有所不同。该研究假设认为,城市景观,灌溉土地和附近山区之间的复杂相互作用为降雨的发展创造了首选区域。这项研究还提供了早期证据,表明干旱的中东部分地区快速城市化可能也响应城市化和灌溉而经历了不同的降水制度。

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    Shepherd J. Marshall;

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  • 年度 2005
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