In the Delaware Estuary, the tidal range at the mouth of the estuary becomes amplified, resulting in a larger range (difference between high and low tide water surface elevation) further up the estuary.  One way to visualize this effect is via violin plots.  The data below is from the NOAA PORTS system in the Delaware Estuary:

River mile 0 corresponds to the mouth of the estuary, where Delaware Bay meets the Atlantic Ocean.

This effect is especially notable in comparison to the same plot for Chesapeake Bay (where tidal amplification is not observed).
My Blog List
My Blog List
Subscribe
Subscribe
Blog Archive
About Me
About Me
I am an engineer working in water resources and the environmental field. On the side, I work with small businesses to help automate their data processing functions. I offer reasonable rates and am very efficient. Send me an e-mail at JYagecic@gmail.com
Loading
Copyright 2016. Dynamic Views theme. Powered by Blogger. Report Abuse.