Determining Water Levels in Maumee and Vedra Valles Using Equilibrium Sediment Transport Theory

Details Determining Water Levels in Maumee and Vedra Valles Using Equilibrium Sediment Transport Theory Determining Water Levels in Maumee and Vedra Valles Using Equilibrium Sediment Transport Theory

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1256t&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1256

Physics

Scientific paper

Equilibrium discharge requires water depths between 100 m and 250 m in
Vedra Valles and between 125 and 440 m in Maumee Valles in response to
longitudinal variations in channel width.

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