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The impact of urbanization on current and future coastal precipitation: a case study for Houston

机译:城市化对当前和未来沿海降水的影响:以休斯敦为例

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The approach of this study was to determine, theoretically, what impact current and future urban land use in the coastal city of Houston, Texas has on the space and time evolution of precipitation on a 'typical' summer day. Regional model simulations of a case study for 25 July 2001 were applied to investigate possible effects of urban land cover on precipitation development. Simulations in which Houston urban land cover was included resolved rain cells associated with the sea breeze front and a possible urban circulation on the northwest fringe of the city. Simulations without urban land cover did not capture the initiation and full intensity of the 'hypothesized' urban-induced rain cell. The response is given the terminology the 'urban rainfall effect' or URE. An urban growth model (UrbanSim) was used to project the urban land-cover growth of Houston, Texas from 1992 to 2025. A regional atmospheric-land surface model was then run with the 2025 urban land-cover scenario. Though we used a somewhat theoretical treatment, our results show the sensitivity of the atmosphere to urban land cover and illustrate how atmosphere-land interactions can affect cloud and precipitation processes. Two urban-induced features, convergence zones along the inner fringe of the city and an urban low-pressure perturbation, appear to be important factors that lead to enhanced rain clouds independently or in conjunction with the sea breeze. Simulations without the city (NOURBAN) produced less cumulative rainfall in the west-northwest Houston area than simulations with the city represented (URBAN). Future urban land-cover growth projected by UrbanSim (URBAN2025) led to a more expansive area of rainfall, owing to the extended urban boundary and increased secondary outflow activity. This suggests that the future urban land cover might lead to temporal and spatial precipitation variability in coastal urban microclimates. It was beyond the scope of the analysis to conduct an extensive sensitivity analysis of cause-effect relationships, though the experiments provide some clues as to why the rainfall evolution differs. This research demonstrates a novel application of urban planning and weather-climate models. It also raises viable questions concerning future planning strategies in urban environments in consideration of hydroclimate changes.
机译:这项研究的方法是从理论上确定德克萨斯州休斯顿沿海城市当前和将来的城市土地使用对“典型”夏季降水的时空演变有何影响。 2001年7月25日的案例研究的区域模型模拟被用于调查城市土地覆盖对降水发展的可能影响。休斯顿城市土地覆盖的模拟包括与海风锋线相关的已分解雨水单元以及该城市西北边缘的可能城市环流。没有城市土地覆盖的模拟并没有捕获“假想的”城市诱发的雨单元的启动和全部强度。该响应的术语称为“城市降雨效应”或URE。使用城市增长模型(UrbanSim)预测了1992年至2025年德克萨斯州休斯顿的城市土地覆盖率增长。然后,在2025年城市土地覆盖率情景下运行了区域大气-土地表面模型。尽管我们使用了某种理论上的处理方法,但我们的结果表明了大气对城市土地覆盖的敏感性,并说明了大气与土地的相互作用如何影响云和降水过程。两个城市诱发的特征,即城市内边缘的收敛带和城市低压扰动,似乎是导致独立或与海风一起增加雨云的重要因素。在没有城市(NOURBAN)的情况下,休斯敦西北偏西地区的累积降雨要比在以城市为代表的模拟(URBAN)时少。 UrbanSim(URBAN2025)预测的未来城市土地覆盖增长将导致降雨范围扩大,这是由于城市边界扩大和二次流出活动增加。这表明,未来的城市土地覆盖可能会导致沿海城市小气候的时空降水变化。尽管实验提供了有关降雨演变为何不同的一些线索,但对因果关系进行广泛的敏感性分析超出了分析的范围。这项研究证明了城市规划和气候模式的新颖应用。考虑到水气候的变化,它还提出了有关城市环境中未来规划策略的可行问题。

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  • 来源
    《Environment and Planning》 |2010年第2期|p.284-304|共21页
  • 作者单位

    Atmospheric Sciences Program, Department of Geography, University of Georgia, Athens, GA 30602, USA;

    Atmospheric Sciences Program, Department of Geography, University of Georgia, Athens, GA 30602, USA;

    Science Systems Applications Inc., NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA;

    Houston-Galveston Area Council, 555 Timmons Lane, Suite 120, Houston, TX 77027, USA;

    122 South Central Campus, Civil and Environmental Engineering, University of Utah, Salt Lake City, UT 84112, USA;

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  • 正文语种 eng
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  • 入库时间 2022-08-18 03:37:16

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