Similarity of stream width distributions across headwater systems.

Similarity of stream width distributions across headwater systems.
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DOI:
10.1038/s41467-018-02991-w
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发表时间:
2018-02-09
影响因子:
16.6
通讯作者:
Gleason CJ
Gleason CJ
中科院分区:
综合性期刊1区
文献类型:
--
作者:
Allen GH;Pavelsky TM;Barefoot EA;Lamb MP;Butman D;Tashie A;Gleason CJ

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The morphology and abundance of streams control the rates of hydraulic and biogeochemical exchange between streams, groundwater, and the atmosphere. In large river systems, the relationship between river width and abundance is fractal, such that narrow rivers are proportionally more common than wider rivers. However, in headwater systems, where many biogeochemical reactions are most rapid, the relationship between stream width and abundance is unknown. To constrain this uncertainty, we surveyed stream hydromorphology (wetted width and length) in several headwater stream networks across North America and New Zealand. Here, we find a strikingly consistent lognormal statistical distribution of stream width, including a characteristic most abundant stream width of 32 ± 7 cm independent of discharge or physiographic conditions. We propose a hydromorphic model that can be used to more accurately estimate the hydromorphology of streams, with significant impact on the understanding of the hydraulic, ecological, and biogeochemical functions of stream networks. The morphology and abundance of streams control the rates of hydraulic and biogeochemical exchange between streams, groundwater and the atmosphere. Here, the authors show that stream hydromorphology is predictable within headwater catchments with implications for stream-atmosphere gas exchange estimates.
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