River corridor science: Hydrologic exchange and ecological consequences from bedforms to basins
Previously regarded as the passive drains of watersheds, over the past 50 years, rivers have
progressively been recognized as being actively connected with off‐channel environments …
progressively been recognized as being actively connected with off‐channel environments …
Advances in understanding river‐groundwater interactions
River‐groundwater interactions are at the core of a wide range of major contemporary
challenges, including the provision of high‐quality drinking water in sufficient quantities, the …
challenges, including the provision of high‐quality drinking water in sufficient quantities, the …
Widespread potential loss of streamflow into underlying aquifers across the USA
Most rivers exchange water with surrounding aquifers,. Where groundwater levels lie below
nearby streams, streamwater can infiltrate through the streambed, reducing streamflow and …
nearby streams, streamwater can infiltrate through the streambed, reducing streamflow and …
Hydrologic connectivity as a framework for understanding biogeochemical flux through watersheds and along fluvial networks
T Covino - Geomorphology, 2017 - Elsevier
Hydrologic connections can link hillslopes to channel networks, streams to lakes, subsurface
to surface, land to atmosphere, terrestrial to aquatic, and upstream to downstream. These …
to surface, land to atmosphere, terrestrial to aquatic, and upstream to downstream. These …
Quantifying surface water–groundwater interactions using time series analysis of streambed thermal records: Method development
CE Hatch, AT Fisher, JS Revenaugh… - Water Resources …, 2006 - Wiley Online Library
We present a method for determining streambed seepage rates using time series thermal
data. The new method is based on quantifying changes in phase and amplitude of …
data. The new method is based on quantifying changes in phase and amplitude of …
Channel water balance and exchange with subsurface flow along a mountain headwater stream in Montana, United States
Channel water balances of contiguous reaches along streams represent a poorly
understood scale of stream‐subsurface interaction. We measured reach water balances …
understood scale of stream‐subsurface interaction. We measured reach water balances …
Spatial and temporal variations in streambed hydraulic conductivity quantified with time-series thermal methods
We gauged and instrumented an 11.42-km long experimental reach of the Pajaro River,
central coastal California, to determine rates of streambed seepage (loss and hyporheic …
central coastal California, to determine rates of streambed seepage (loss and hyporheic …
Assessment of managed aquifer recharge site suitability using a GIS and modeling
We completed a two‐step regional analysis of a coastal groundwater basin to (1) assess
regional suitability for managed aquifer recharge (MAR), and (2) quantify the relative impact …
regional suitability for managed aquifer recharge (MAR), and (2) quantify the relative impact …
From hillslope to stream: methods to investigate subsurface connectivity
T Blume, HJ Van Meerveld - Wiley Interdisciplinary Reviews …, 2015 - Wiley Online Library
Hydrologic connectivity is the linkage of separate regions of a catchment via water flow.
Knowledge of hillslope–stream connectivity (both at the surface and in the subsurface) is …
Knowledge of hillslope–stream connectivity (both at the surface and in the subsurface) is …
Assessing spatial and temporal connectivity between surface water and groundwater in a regional catchment: Implications for regional scale water quantity and quality
It is common for surface water–groundwater interaction assessments to investigate river
reaches at a local scale and as discrete individual systems, which are generally classified as …
reaches at a local scale and as discrete individual systems, which are generally classified as …