Tasneem Haq Meem, Bruce L. Rhoads, Quinn W. Lewis, Muhammad Umar, Alexander Sukhodolov
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Length Scales, Rates, and Variability of Mixing Downstream of River Confluences
Past work on lateral mixing downstream of river confluences has focused on mixing at individual confluences, limiting general knowledge of this process. This study evaluates the average length scales, rates, and variability of lateral mixing downstream at 43 confluences for 150 events based on contrasts in gray-scale intensity of confluent flows captured by aerial images. Only 45% of the events exhibit complete mixing over the length of the imaged downstream reach. The average dimensionless length scale (sd) of complete mixing is 7.4 times the downstream flow width and varies from sd = 1.1–26.3, but not all flows completely mix. A nonlinear spatial pattern of mixing, consistent with relations derived from shallow flow theory, reveals that mixing rates are substantially higher immediately downstream of confluences with most mixing occurring over sd < 15. The findings confirm that confluences are important locations of accelerated mixing in river networks.
期刊介绍:
Geophysical Research Letters (GRL) publishes high-impact, innovative, and timely research on major scientific advances in all the major geoscience disciplines. Papers are communications-length articles and should have broad and immediate implications in their discipline or across the geosciences. GRLmaintains the fastest turn-around of all high-impact publications in the geosciences and works closely with authors to ensure broad visibility of top papers.