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Using flushing rate to investigate spring-neap and spatial variations of gravitational circulation and tidal exchanges in an estuary

机译:用冲洗速度调查河口重力和环流的春季变化和空间变化

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Spring-neap and spatial variations of gravitational circulation and tidalexchanges in the Sumjin River Estuary (SRE) were investigated using theflushing rate. The flushing rate was calculated between multiple estuarinesegments and the adjacent bay to examine the spatial variation of twoexchanges. The strength of gravitational circulation and tidal exchangesmodulated significantly between spring and neap tides, where stratificationalternated between well-mixed and highly-stratified conditions over thespring-neap cycle. Tide-driven dispersive flux of salt dominated overgravitational circulation exchange near the mouth during spring tide due tothe larger tidal amplitude that caused well-mixed conditions and rapidexchange. In contrast, the central and inner regimes were found to bepartially stratified during spring tide due to the reduction in tidalamplitude where both gravitational circulation and tidal exchanges wereimportant in transporting salt. The combined contributions of two fluxeswere also found during neap tide along the SRE due to the significantreduction in vertical mixing that accompanied strong stratification. Gravitationalcirculation exchange almost entirely dominated in transporting salt at theupstream end during spring and neap tides.
机译:利用冲洗率研究了津津河河口(SRE)的春季负重力和环流变化。计算多个河口段和相邻海湾之间的冲水率,以检查两次交换的空间变化。在春季和春季潮汐之间,重力循环和潮汐交换的强度显着调节,在春季-春季周期中,分层在充分混合和高度分层的条件之间交替。在春季潮汐期间,潮汐驱动的盐分分散通量主导着重力引力环流交换,这是由于较大的潮汐振幅引起了充分混合的条件和快速交换。相反,由于潮汐振幅的减小,在重力作用下盐分和潮汐交换都对盐分的输送很重要,因此春季和春季潮汐中部和内部区域被部分分层。在沿SRE的潮汐潮汐中也发现了两种通量的组合贡献,这是由于伴随强分层的垂直混合的显着减少。引力环流交换几乎完全在春季和潮汐潮汐期末的盐分输送中占主导地位。

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