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. 2019 Nov 21;9:17522. doi: 10.1038/s41598-019-53956-y

Author Correction: Deep-sea Sediment Resuspension by Internal Solitary Waves in the Northern South China Sea

Yonggang Jia 1,2,7, Zhuangcai Tian 1,2, Xuefa Shi 2,3, J Paul Liu 4, Jiangxin Chen 2,5, Xiaolei Liu 1,2,7, Ruijie Ye 2,6, Ziyin Ren 1,2, Jiwei Tian 2,6,
PMCID: PMC6868124  PMID: 31748610

Correction to: Scientific Reports 10.1038/s41598-019-47886-y, published online 20 August 2019

The original version of this Article contained a typographical error in the Abstract.

“Specifically, we estimated that ISWs could induce and suspend 78.7 Mt/yr of sediment from shelf to deep-sea areas of the northern South China Sea.”

now reads:

“Specifically, we estimated that ISWs could induce and suspend 787 Mt/yr of sediment from shelf to deep-sea areas of the northern South China Sea.”

In addition, the original version of this Article contained a typographical error in the Conclusion.

“We estimated that ISWs could suspend 78.7 Mt/yr sediment from the shelf to the deep sea in the northern South China Sea, which accounted for 6.1% (16.4% of the contribution of Asian rivers) of the global river-discharged sediment transported to the sea.”

now reads:

“We estimated that ISWs could suspend 787 Mt/yr sediment from the shelf to the deep sea in the northern South China Sea, which accounted for 6.1% (16.4% of the contribution of Asian rivers) of the global river-discharged sediment transported to the sea.”

This has now been corrected in the PDF and HTML versions of the Article.


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