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Wang, C.Y., D. Dreger, M. Manga, A. Wong, 2004, Streamflow increase due to rupturing of hydrothermal reservoirs: Evidence from the 2003 San Simeon, California, earthquake, Geophys.
The cropland is identified as the most important contributor in the response of streamflow increase for the region.
Across different climate models precipitation and streamflow increase in northern Europe and decrease in southern Europe, but the latitude at which this change occurs varies depending on the GCM.
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Winter streamflow increased in the two most recent decades, which resulted from the reservoir release.
Interaction of water with earthquakes: Earthquake-induced hydrological changes, including liquefaction, groundwater changes and streamflow increases during and after earthquakes.
SSC increased as streamflow increased for the entire range of observed streamflow in the Atchafalaya River.
Annual streamflow increased significantly in past decades in the southern Tianshan, especially in spring and winter months.
Here we show that in the Council Creek watershed in north-central Oklahoma, the baseflow component of streamflow increased from 1938 to 1992 during which time tree cover increased from 5% to 18% of the watershed area.
Results show that streamflow increased significantly (p < 0.05) in 35% (19/55) of watersheds (median 2.4 ± 0.3 mm/year), baseflow increased in 58% of watersheds (median 1.1 ± 0.4 mm/year), and baseflow index (baseflow/streamflow, BFI) increased in 42% of watersheds (median 0.2 ± 0.1%/year).
Decreases in evapotranspiration and associated streamflow increases in response to ambient CO2 exposures are expected to episodically increase the frequency and severity of flood and affect flow-dependent aquatic biota in forested watersheds.
During wet or very wet conditions (large rainfall events or peak snowmelt), saturation overland flow increased due to the expansion of the saturated areas and riparian groundwater and hillslope subsurface flow to streamflow increased as well.
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