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River runoff is significant to the north of Lisbon where several rivers contribute fresh water input to the shelf [25].
On the average, groundwater contributes to total river runoff about 30 percent of its water on a global basis.
The chemistry of groundwater and river runoff is being modified by human activities on a global scale.
This section focuses on term R in equation (9) representing groundwater and river runoff losses from the soil moisture zone.
Surface-water temperature varies with season, latitude, and surface circulation; surface salinity is the balance between precipitation, evaporation, and river runoff.
Water quantity data included river runoff.
River runoff was more sensitive to precipitation than to temperature.
Human intervention has strongly altered patterns of river runoff.
Only 8.4 Tg of sulfate is supplied by river runoff [55].
This was manifested by the negative correlation between river runoff and total ion concentrations.
Briefly, the increased water salinity is dependent upon precipitation, river runoff and evaporation.
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