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Research demonstrating the biophysical benefits of urban trees are often used to justify investments in urban forestry. Far less emphasis, however, is placed on the non-bio-physical benefits such as improvements in public health. Indeed, the public-health benefits of trees may be significantly larger than the biophysical benefits, and, therefore, failure to account for the public-health benefits of trees may lead to underinvestment in urban forestry. In addition, the distribution of trees that maximizes bio-physical benefits may not maximize public-health benefits. 相似文献
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Depending on the spatial density of built cover and location within a catchment, residential areas make varying contributions to surface runoff throughout different rainfall events. This study examined these contributions and the associated effect of different surface covers and sustainable drainage systems on runoff generation. The Soil Conservation Service curve number (SCS-CN) method was applied to analyse urban development in the Höjeå river catchment in southern Sweden.The results indicated that identical amounts of surface runoff are generated by low-density residential areas on heavy clay soils and high-density residential areas on sandy soils. However, increasing the density of built-up areas on sandy soils is likely to be more disruptive to the hydrological balance and to generate a greatly increasing difference in runoff as building density and impermeable surface area increase. A similar pattern is likely to occur if rainfall intensity increases. It may therefore be appropriate to apply different planning considerations to residential developments depending on the existing soil group, e.g. conserving existing vegetated surfaces on sandy soil and incorporating permeable paving materials and sub-surface infiltration beds in development on clayey soils. Increased area of impermeable surface cover will increase surface runoff in all residential areas, irrespective of building density, soil group and rainfall intensity. However, adapting a systems approach in combining vegetative structures and permeable paving materials with subsurface infiltration beds can help mitigate the impact of surface runoff, particularly in urban developments on clay-rich soils. 相似文献
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[目的]研究2005年5月30日甘肃中部一次超级单体风暴三维结构及回波特征量。[方法]利用兰州CINRAD/CC多普勒雷达监测资料,对2005年5月30日发生在甘肃中部一次罕见的超级单体风暴三维结构特征进行分析,试图揭示青藏高原东北侧出现超级单体风暴的三维结构及其回波特征指标,以寻找这次出现罕见大冰雹的原因。[结果]这次大范围强风暴是在蒙古冷涡、低空急流、地面冷锋共同作用下造成的。主体回波发展成熟时期,在反射率因子图上,低层风暴左前方呈现明显的倒"V"字型结构,右后侧呈现典型的钩状、"人"字型回波特征;低层有界弱回波区(穹隆)与高层强回波悬垂体相对应;强反射率因子区超过60 dBz;相应的径向速度图上呈现一个弱中气旋。VIL的跃增特性可作为判断冰雹增长开始的指标之一,几乎所有VIL密度≥4.00 g/m3的风暴对于判断降大冰雹(直径≥20 mm)的可能性比VIL具有更明显的指示意义。[结论]该研究为强对流天气的临近预报和人工防雹提供参考。 相似文献
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“韦帕”台风暴雨过程分析 总被引:1,自引:1,他引:1
从天气形势、数值预报产品等方面,对"韦帕"台风暴雨过程进行分析总结,探讨了汛末由于台风影响而产生暴雨的形成机制。 相似文献
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G.H.McTainsh 《干旱区资源与环境》1993,(Z1)
<正> Meteorological records of dust storm frequencies have recently been used to describebroadscale wind erosion in several regions of the world (West Africa-Middleton 1985, Mid-dle East-Middeton 1986, USA-Nicking & Brazel 1984) and in Australia significant recentprogress has been made (Middleton 1984, McTainsh and Pitblado 1987, Burgess etal, 1988, Mctainsh et al, 1989, 1990). These studies demonstrate the utility of thismethodology for measuring wind erosion on a broadscale. There remains significant room 相似文献
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基于农业气象灾害系统构成体系和灾害风险理论,依据海南岛18个气象台站1961-2012年9-11月逐日降水数据、地理信息数据、耕地面积和冬种瓜菜种植面积资料,借助GIS技术,采用加权法和自然断点法对海南岛冬种瓜菜暴雨洪涝灾害致灾因子危险性、孕灾环境敏感性、承灾体易损性进行指标构建和风险分析,在此基础上构建冬种瓜菜暴雨洪涝灾害综合风险指数,并将该指数应用于海南岛冬种瓜菜暴雨洪涝灾害的风险区划。结果表明,海南岛东部和东北部地区为冬种瓜菜暴雨洪涝灾害高和次高危险区,其中万宁市大部、琼海市和屯昌县南部、陵水县中部风险最高;西部为次低和低风险区;其余地区为中等风险区。灾情验证结果表明,实际灾情的空间分布与风险区划结果基本吻合。研究结果可为海南冬种瓜菜生产布局、避减灾害风险提供依据。 相似文献
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Michael Rodgers Mark O’Connor Mark Gerard Healy Connie O’Driscoll Zaki-ul-Zaman Asam Mika Nieminen Russell Poole Markus Müller Liwen Xiao 《Forest Ecology and Management》2010
The aim of this study was to investigate the release of phosphorus (P) to receiving waters resulting from harvesting 34-year-old lodgepole pine trees in an upland peat catchment. The study site was within a 25.3-hectare (ha) area, and was drained by a stream that received flows from ploughed furrows, mainly, via collector drains, and discharged directly to the salmonid Shrahrevagh River, Burrishoole, Co. Mayo, Ireland. The study site was divided into two parts: the upstream part was left intact and the downstream part was harvested in early Autumn 2005 following implementation of forest guidelines. Good management practices such as proper use of brash mats and harvesting only in dry weather were implemented. Two instrumented stations were established – one just upstream (US) and the other just downstream (DS) of the clearfelled area. The measurement of P concentrations at the two stations commenced in May 2005, two months before the harvesting started. The daily mean P concentration at the DS station increased from about 6 μg L−1 of total reactive phosphorus (TRP) during pre-clearfelling to 429 μg L−1 in August 2006. By October 2009, four years after clearfelling, the P concentrations at the DS station had returned to pre-clearfelling levels. In the first three years after harvesting, up to 5.15 kg ha−1 of TRP was released from the harvested catchment to the receiving water; in the second year alone, 2.3 kg ha−1 of TRP was released. Linear regression can be used to describe the relationship between TRP load and water discharge. About 80% of the total phosphorus (TP) in the study stream was soluble and more than 70% of the P release occurred in storm events, indicating that traditional buffer strips with widths of 15–20 m might not be efficient for P immobilization. The P concentrations were affected by antecedent weather conditions and highest concentrations occurred during storm events following prolonged drought periods. The water extractable phosphorus (WEP) contents in the soil were significantly higher below windrow/brash material than in brash-free areas, and whole-tree harvesting should be studied as one of the means to decrease P export from blanket peats. 相似文献