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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Potential contributions of climate change and urbanization to precipitation trends across China at national, regional and local scales
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Potential contributions of climate change and urbanization to precipitation trends across China at national, regional and local scales

机译:气候变化和城市化在国家,区域和地方尺度下降水趋势的潜在贡献

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Climate change and urbanization collectively influence precipitation changes. However, their separate potential contributions to precipitation changes are not well understood due to their complex interactions. Hence, a trajectory-based method was used to separate their potential contributions across national, regional and local scales in China. Precipitation changes in non-urban regions can be regarded as representing the influence of climate change and can serve as a reference for isolating precipitation changes due to urbanization in urban areas. Our results revealed that climate change was the dominant factor for precipitation trends, while urbanization exhibited a relatively weak influence, especially for extreme precipitation at the national scale. At the regional scale, the impacts of urbanization on precipitation became more significant. About 20.2 and -30.6% of positive and negative trends in total precipitation originated from urbanization. At the local scale, the potential contribution of urbanization was strongly correlated with local environmental characteristics. Although there were differences in the potential contributions of climate change and urbanization at national, regional and local scales, climate change was the dominant factor for precipitation trends and urbanization acted as a regulator to drying or wetting due to precipitation under climate change. In general, urbanization causes a greater impact on total precipitation than on precipitation extremes. Due to this, attribution approach is static and broad-based and does not render the level of confidence that is needed for scale-aware attribution, future studies are needed to understand the physical mechanisms of impacts of local environment changes on precipitation trends at different geographical locations over China.
机译:气候变化和城市化共同影响降水变化。然而,由于其复杂的相互作用,它们对降水变化的单独潜在贡献并不充分理解。因此,基于轨迹的方法用于将其在中国的国家,区域和当地级别的潜在贡献分开。非城市地区的降水变化可被视为代表气候变化的影响,并可作为在城市地区的城市化因城市化而分离降水变化的参考。我们的研究结果表明,气候变化是降水趋势的主要因素,而城市化呈现出相对薄弱的影响,特别是在全国范围内极端降水。在区域规模,城市化对降水的影响变得更加重要。大约20.2和-30.6%的积极和负面趋势的总降水来自城市化。在当地规模,城市化的潜在贡献与当地环境特征密切相关。虽然国家,区域和地方尺度的气候变化和城市化潜在潜在贡献存在差异,但气候变化是降水趋势和城市化的主要因素,作为气候变化下降水导致的调节器令调节剂或润湿。一般来说,城市化导致对总降水的影响大于降水极端。由于这一目标,归因方法是静态和广泛的,并且没有呈现比例感知归属所需的信心水平,需要进行未来的研究来了解当地环境变化对不同地理的降水趋势的影响中国的位置。

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