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At the same time water piled up over the southeast Grand Banks where the mean water depth is relatively shallow (~50 m).
The bathymetric map shows a very shallow lake of 4 m mean water depth and an almost flat lake bottom.
A method is also proposed to calculate the time-dependent first passage probability for the case where wave climate and mean water depth change with time.
Estimates based on the mean water depth resulted in a ∼40% higher annual rate of 204 g C m− 2 y− 1.
Locations closer to shore, where the mean water depth is less than 50 m, tended to exhibit lower omnidirectional wave power, but were more uniform directionally.
This study explores typical characteristics of the mean and turbulent profiles at a mixed low tidal energy site (40 m mean water depth) where the waves have limited effects on the currents.
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Fish passage performance was investigated in a full-scale experimental VSF under two different slot configurations (C1 and C2), which require different discharges for equal mean water depths in the pools (Q = 110 L s−1, for C1, and Q = 81 L s−1, for C2).
According to the results, the mean water table depth changes from 1 to 30 m and the mean transmissivity of the aquifer formations changes from 75 to 3250 (m2/day) in the studied plain.
At first, quantitative values of the network input parameters included the mean water table depth, the transmissivity of aquifer formations, distance from the pollutant centers, site elevation and the numbers of households were estimated using the secondary data of water resources, maps and digital layers in the GIS environment for the 85 studied drinking water wells.
These eight input patterns with fixed network architecture were implemented to simulate groundwater quality and the results show that optimized structure of network inputs consists of three inputs included the mean water table depth, the transmissivity of aquifer formations and distance from the pollutant centers.
Model simulation yields both hourly and daily time series of several catchment hydrologic variables, including mean water table depth (WTD), percent surface saturation, and total surface runoff.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com