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The mean annual flow of the river at Krâchéh in Cambodia is about 500,000 cubic feet (14,200 cubic metres) per second, which is about twice the flow of the Columbia River in North America.
Mean annual flow was positively related to minimum flows, suggesting that potential future declines in mean annual flows will correspond with declines in minimum flows.
The Amu Darya River is at the south of the Aral Sea basin, and has a mean annual flow of 70 80 km3/year.
Quantifying mean annual flow of rivers (MAF) at ungauged sites is essential for assessments of global water supply, ecosystem integrity and water footprints.
This study investigates streamflow variations and evaluates the impacts of climate variability and human activity on the mean annual flow in the MRYRB.
Four commonly used indices, including mean annual flow, annual center timing, 100-year daily high streamflow, and 10-year 7-day average low streamflow were used for evaluation.
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Mean annual flows in the Lewis Creek are estimated as 3.1 m3/s, based on historic records for a nearby US Geological Survey gaging station located nearly 6.5 180 km downstream with a drainage area of 199 199 km2.
The simulation of the water surface along the Po River for different flow conditions (high, low and mean annual flows) is performed with inputs from a quasi-2D model implemented using detailed topographic and bathymetric information (LiDAR, 2 m resolution).
The average annual flow recorded there was from 1923 to 1966.
Four contrasting methods for estimating mean flow, proportion of flow in February, 7-day mean annual low flow, mean annual high flow, the all-time flow duration curve and the February flow duration curve at ungauged sites across New Zealand were compared.
An empirical relationship was developed for mean annual minimum flow as a function of catchment area, mean annual rainfall and mean annual evaporation.
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