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Global hydrobelts and hydroregions: Improved reporting scale for water-related issues?

机译:全球水带和水域:改进了与水有关问题的报告规模?

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Global-scale water issues such as its availability, water needs or stress, or management, are mapped at various resolutions and reported at many scales, mostly along political or continental boundaries. As such, they ignore the fundamental heterogeneity of hydroclimates and natural boundaries of river basins. Here we describe the continental landmasses at two levels: eight hydrobelts strictly limited by river basins, defined at a 30' (0.5) resolution, which are decomposed on continents as 26 hydroregions. The belts were defined and delineated, based primarily on the annual average temperature (T) and run-off (q), to maximise inter-belt differences and minimise intra-belt variability. This new global puzzle defines homogeneous and near-contiguous entities with similar hydrological and thermal regimes, glacial and postglacial basin histories, endorheism distribution and sensitivity to climate variations. The mid-latitude, dry and subtropical belts have northern and southern analogues and a general symmetry can be observed for T and q between them. The boreal and equatorial belts are unique. Population density between belts and between the continents varies greatly, resulting in pronounced differences between the belts with analogues in both hemispheres. Hydroregions (median size 4.7 M km ~2) are highly contrasted, with the average q ranging between 6 and 1393 mm yr~(-1) and the average T between-9.7 and +26.3 C, and a population density ranging from 0.7 to 0.8 p km~(-2) for the North American boreal region and some Australian hydroregions to 280 p km~(-2) for some Asian hydroregions. The population/run-off ratio, normalised to a reference pristine region, is used to map and quantify the global population at risk of severe water quality degradation. Our initial tests suggest that hydrobelt and hydroregion divisions are often more appropriate than conventional continental or political divisions for the global analysis of river basins within the Earth system and of water resources. The GIS files of the hydrobelts and hydroregions are available at the supplement of this article and at doi:10.1594/PANGAEA.806957 as well as hrefCombining double low line"geotypes.net"targetCombining double low line"- blank">geotypes.
机译:全球规模的水问题,例如其可用性,水需求或压力或管理,以各种决议进行绘制,并在许多规模上得到报告,主要是沿着政治或大陆边界。因此,他们忽略了水气候的基本异质性和流域的自然界线。在这里,我们在两个层次上描述了大陆陆块:八个受河流域严格限制的水带,以30'(0.5)的分辨率定义,这些水带在大陆上被分解为26个水区。皮带的定义和划分主要基于年平均温度(T)和径流(q),以使皮带间的差异最大,并使皮带内的可变性最小。这个新的全球难题定义了具有相似的水文和热态,冰川和冰川后盆地历史,背胶分布和对气候变化的敏感性的均质和近邻的实体。中纬度,干燥和亚热带带具有北部和南部的类似物,并且可以观察到它们之间的T和q大致对称。北方和赤道带是独特的。各带之间以及各大洲之间的人口密度差异很大,导致两个半球中带类似物的带之间存在明显差异。水域(中位面积470 M km〜2)形成鲜明对比,平均q范围在6至1393 mm yr〜(-1)之间,平均T在-9.7至+26.3 C之间,人口密度在0.7至北美寒带区和一些澳大利亚水区为0.8 p km〜(-2),亚洲水区为280 p km〜(-2)。相对于原始原始区域进行标准化的人口/径流比率用于绘制地图并量化面临严重水质退化风险的全球人口。我们的初步测试表明,对于地球系统内的流域和水资源的全球分析,与传统的大陆或政治分区相比,水带和水域分区通常更合适。可在本文的补编和doi:10.1594 / PANGAEA.806957以及geotypes中获得水带和水域的GIS文件。

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