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Classifying streams on the basis of elevation above mean sea level- A universal approach

机译:根据平均海平面以上的海拔对河流进行分类-一种通用方法

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Till date, more than 20 different stream classification systems have been proposed and yet none of them have been accepted universally. Here, we introduce "elevation above mean sea level" as the new universal stream classifying parameter. 873 field values describing hydraulic geometry of UK, USA and Canadian streams were compiled and divided into 5 distinct elevation zones. Modal and most probable values (MPVs) of aspect ratio (Ar), channel slope (Sc) and sinuosity (P) occurring concurrently in nature were calculated for each of the 5 elevation zones. Ar initially increased while moving upstream and then decreased above 5000 ft. Sc always exhibited an increasing trend with elevation. P showed high values only at 0-250 ft range and for all other zones was observed to be fairly constant. When datasets of sandy, gravel and cobble streams were divided separately into these 5 elevation zones, similar behavior was observed in the MPVs of Ar, Sc, and P for each stream type.
机译:迄今为止,已经提出了20多种不同的流分类系统,但是没有一个被普遍接受。在此,我们介绍“平均海平面以上的海拔”作为新的通用流分类参数。编制了描述英国,美国和加拿大河流的水力几何形状的873个场值,并将其划分为5个不同的高程区。对于5个高程区域,分别计算了自然界中同时出现的纵横比(Ar),通道斜率(Sc)和弯曲度(P)的模态和最可能值(MPV)。 Ar最初是在向上游移动时增加,然后在5000 ft以上下降。Sc总是显示出随海拔升高而增加的趋势。 P仅在0-250英尺范围内显示高值,并且对于所有其他区域,P值都相当恒定。当将沙,砾石和卵石流的数据集分别划分为这5个海拔区域时,对于每种流类型,在Ar,Sc和P的MPV中观察到类似的行为。

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