The Temporal Response of the Length of a Partially Stratified Estuary to Changes in River Flow and Tidal Amplitude

摘要

The temporal response of the length of a partially mixed estuary to changes in freshwater discharge Q_f and tidal amplitude U_T is studied using a 108-day time series collected along the length of the Hudson River estuary in the spring and summer of 2004 and a long-term (13.4 yr) record of Q_f, U_T, and near-surface salinity. When Q_f was moderately high, the tidally averaged length of the estuary L_5, here denned as the distance from the mouth to the up-estuary location where the vertically averaged salinity is 5 psu, fluctuated by more than 47 km over the spring-neap cycle, ranging from 28 to >75 km. During low flow periods, L_5 varied very little over the spring-neap cycle and approached a steady length. The response is quantified and compared to predictions of a linearized model derived from the global estuarine salt balance. The model is forced by fluctuations in Q_f and U_t relative to average discharge Q_o and tidal amplitude U_(To) and predicts the linear response time scale τ and the steady-state length L_o for average forcing. Two vertical mixing schemes are considered, in which 1) mixing is proportional to U_T and 2) dependence of mixing on stratification is also parameterized. Based on least squares fits between L_5 and estuary length predicted by the model, estimated τ varied by an order of magnitude from a period of high average discharge (Q_o = 750 m~3 s~(-1), τ = 4.2 days) to a period of low discharge (Q_o = 170 m~3 s~(-1), τ = 40.4 days). Over the range of observed discharge, L_o ∝ Q_o~(-0.30±0.03); consistent with the theoretical scaling for an estuary whose landward salt flux is driven by vertical estuarine exchange circulation. Estimated τ was proportional to the discharge advection time scale (L_oA/Q_o, where A is the cross-sectional area of the estuary). However, t was 3-4 times larger than the theoretical prediction. The model with stratification-dependent mixing predicted variations in L_5 with higher skill than the model with mixing proportional to U_T. This model provides insight into the time-dependent response of a partially stratified estuary to changes in forcing and explains the strong dependence of the amplitude of the spring-neap response on freshwater discharge. However, the utility of the linear model is limited because it assumes a uniform channel, and because the underlying dynamics are nonlinear, and the forcing Q_f and U_T, can undergo large amplitude variations. River discharge, in particular, can vary by over an order of magnitude over time scales comparable to or shorter than the response time scale of the estuary.