The beach water table as a response variable of the beach-ocean-atmosphere system

Fluctuations of the water table in a marine beach over a rising half-tide cycle were investigated as a function of variations in local still water level, swash runup distance, distance of a sampling station from the shoreline, and atmospheric pressure. The data were taken from a 30-day time series o...

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Bibliographic Details
Main Author: Fausak, Leland Edward
Format: Others
Language:English
Published: W&M ScholarWorks 1970
Subjects:
Online Access:https://scholarworks.wm.edu/etd/1627407592
https://scholarworks.wm.edu/cgi/viewcontent.cgi?article=7170&context=etd