Tidal Amplification – Chesapeake versus Delaware

December 15, 2015
By

[This article was first published on AdventuresInData, and kindly contributed to R-bloggers]. (You can report issue about the content on this page here)
Want to share your content on R-bloggers? click here if you have a blog, or here if you don't.

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).

To leave a comment for the author, please follow the link and comment on their blog: AdventuresInData.

R-bloggers.com offers daily e-mail updates about R news and tutorials about learning R and many other topics. Click here if you're looking to post or find an R/data-science job.
Want to share your content on R-bloggers? click here if you have a blog, or here if you don't.



If you got this far, why not subscribe for updates from the site? Choose your flavor: e-mail, twitter, RSS, or facebook...

Comments are closed.

Search R-bloggers

Sponsors

Never miss an update!
Subscribe to R-bloggers to receive
e-mails with the latest R posts.
(You will not see this message again.)

Click here to close (This popup will not appear again)