Luo Yiming
Geophysical Institute, University of Bergen and Bjerknes Centre for Climate Research, Allegaten 70, 5020, Bergen, Norway.
Department of Oceanography, Dalhousie University, 1355 Oxford Street, Halifax, NS B3L2H4, Canada.
Sci Rep. 2017 Mar 29;7(1):505. doi: 10.1038/s41598-017-00604-y.
Understanding Th distributions in the global ocean is important to support and guide the use of this important radioactive nuclide in multiple aspects of oceanographic research, and this issue is now revisited. Based on estimates of export productivity (EP) over 2003-2010 and assuming Th scavenging at equilibrium at seven Pacific stations where linear Th profiles are found, an empirical equilibrium-state Th-scavenging versus EP correlation is established. This correlation demonstrates the relationship between Th-scavenging intensity and EP in the absence of advection. With this correlation, other Th profiles from global oceans are reinterpreted. My findings provide alternative explanations of signals carried by Th distributions with regard to advection, by a reassessment of the Th deficits in deep waters. Such an equilibrium-state Th-scavenging versus EP correlation provides a basis for convenient parameterization for use in 3D modeling studies of the Th distributions.
了解全球海洋中钍(Th)的分布对于支持和指导这一重要放射性核素在海洋学研究多个方面的应用至关重要,现在我们重新审视这个问题。基于2003 - 2010年期间的输出生产力(EP)估计值,并假设在七个发现线性钍剖面的太平洋站点处于平衡状态下的钍清除情况,建立了一个经验性的平衡态钍清除与EP的相关性。这种相关性展示了在没有平流的情况下钍清除强度与EP之间的关系。利用这种相关性,对全球海洋的其他钍剖面进行了重新解释。通过对深水中钍亏缺的重新评估,我的研究结果为钍分布中关于平流所携带信号提供了替代解释。这种平衡态钍清除与EP的相关性为钍分布的三维建模研究中方便的参数化提供了基础。