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- Rivers, Estuaries, Deltas - Woods Hole Oceanographic Institution
Rivers, estuaries, and deltas are key to understanding the chemical structure of seawater, and are home to some of the world's most diverse ecosystems
- Brackish Water: Where Fresh Water Rivers Meet A Salt Water Sea
How does an estuary work? From a physicist’s point of view, the density difference between fresh and salt water makes estuaries interesting When river water meets sea water, the lighter fresh water rises up and over the denser salt water Sea water noses into the estuary beneath the outflowing river water, pushing its way upstream along the bottom Often, as in the Fraser River, this occurs
- jc006893 1. - Woods Hole Oceanographic Institution
In the absence of rotational effects, stratification in the estuary decreases following both down-estuary and up-estuary winds, but stratification experiences larger reduction and takes longer to recover under up-estuary winds
- New perspectives on radium behavior within a subterranean estuary
Many studies have used the unique geochemical signal originating from the subterranean estuary to determine rates of transport of such cons- tituents to the coastal ocean via submarine groundwater discharge (Burnett et al , 2006 and references therein)
- Episodic and Long-Term Sediment Transport Capacity in The Hudson River . . .
Abstract A tidally averaged model of estuarine dynamics is used to estimate sediment transport in the Hudson River estuary over the period 1918 to 2005 In long-term and seasonal means, along-channel gradients in sediment flux depend on the estuarine salinity gradient and along-channel depth profile Lateral depth variation across the estuary affects the near-bottom baroclinic circulation and
- Eglinton, T - Woods Hole Oceanographic Institution
Walker, S E , Dickhut, R M , Chisholm-Brause, C , Sylva, S , and Reddy, C M , Molecular and isotopic identification of PAH sources in a highly industrialized urban estuary, Organic Geochemistry, 2005; v36, 619-632 Sources of polycyclic arom hydrocarbons (PAHs) in sediments in the Elizabeth River, VA, a highly industrialized urban estuary, were examd using multiple source identification
- Subtidal Salinity and Velocity in the Hudson River Estuary . . .
A tidally and cross-sectionally averaged model based on the temporal evolution of the quasi-steady Hansen and Rattray equations is applied to simulate the salinity distribution and vertical exchange flow along the Hudson River estuary The model achieves high skill at hindcasting salinity and residual velocity variation during a 110-day period in 2004 covering a wide range of river discharges
- Distribution of anaerobic ammonia-oxidizing bacteria in a subterranean . . .
The ladderane fatty acid pro le shows three regions of high con-fi centration within the subterranean estuary at depths that correspond to the URTZ, MRTZ, and DRTZ, in addition to high concentration in a surface sample that had a soil-like consistency
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