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Stream flow between precipitation events
Baseflow (also called drought flow, groundwater recession flow, low flow, low-water flow, low-water discharge and sustained or fair-weather runoff) is
Baseflow
Baseflow residence time (often mean baseflow residence time) is a parameter useful in describing the mixing of waters from the infiltration of precipitation
Baseflow_residence_time
Graph showing the rate of water flow
and climate conditions and changes. However, the process of separating “baseflow” from “direct runoff” is an inexact science. In part this is because these
Hydrograph
Physical parameter of a drainage basin
that baseflow into streams is inversely related to the drainage density of the drainage basin: Q b a s e f l o w ∝ D d − 2 . {\displaystyle Q_{baseflow}\propto
Drainage_density
Groundwater that recharges an aquifer
(WB) methods (including groundwater models (GMs)); and the estimation of baseflow (BF) to rivers. Groundwater recharge can occur through diffuse or focused
Groundwater_recharge
Highland region in central-southern United States
[citation needed] Ozark rivers and streams are typically clear water, with baseflows sustained by many seeps and springs, and flow through forests along limestone
Ozarks
Syrian plateau occupied by Israel
higher elevations, which are snow-covered in the winter and help sustain baseflow for rivers and springs during the dry season. The Heights receive significantly
Golan_Heights
City in Canterbury, New Zealand
(May 2007). "Waterways, Swamps and Vegetation of Christchurch in 1856 and Baseflow Discharge in Christchurch Streams" (PDF). GNS Science Consultancy Report
Christchurch
Water located beneath the ground surface
(WB) methods (including groundwater models (GMs)); and the estimation of baseflow (BF) to rivers. An aquifer is an underground layer of water-bearing material
Groundwater
Body of surface water flowing down a channel
inflow is not observed above the channel, the observed water is likely baseflow. Another perennial stream indication is an abundance of red rust material
Stream
Situation where there is a shortage of water
They can also lead to land subsidence, degraded springs and reduced baseflows. The main cause of water scarcity as a result of consumption is the extensive
Water_scarcity
Type of soil in frozen state
2023). "Detecting Permafrost Active Layer Thickness Change From Nonlinear Baseflow Recession". Water Resources Research. 57 (1) e2022WR033154. Bibcode:2023WRR
Permafrost
Flow of water in streams and other channels
intersects the water table, providing a steady supply of water, termed baseflow, during both dry and rainy periods. Because of the large supply of groundwater
Streamflow
Industrial wastewater Sewage River measurement and modelling Baer's law Baseflow Bradshaw model Discharge (hydrology) Drainage density Exner equation Groundwater
List of countries and dependencies without rivers
List_of_countries_and_dependencies_without_rivers
Biogeochemical cycle for movement of water on Earth
artificially contribute to groundwater recharge, resulting in higher stream baseflow conditions and groundwater contamination. Groundwater depletion, however
Water_cycle
River that runs through mountains
Industrial wastewater Sewage River measurement and modelling Baer's law Baseflow Bradshaw model Discharge (hydrology) Drainage density Exner equation Groundwater
Mountain_river
Small natural stream
Industrial wastewater Sewage River measurement and modelling Baer's law Baseflow Bradshaw model Discharge (hydrology) Drainage density Exner equation Groundwater
Brook_(stream)
Water table aquifer beneath the Great Plains in the United States of America
(groundwater recharge from the surface), what is leaving (water pumped out and baseflow to streams), and what the net changes in storage are (rise, fall or no
Ogallala_Aquifer
Sub-field of hydrology concerned with above-earth water
categorized as groundwater, and the rate at which this occurs determines baseflow needs for instream flow, as well as subsurface water levels in wells. While
Surface-water_hydrology
Village in Egypt
sills that made navigation difficult for Nile ships, especially during baseflow. Today, both cataracts near Aswan and Wadi Halfa are covered by Lake Nasser
Abu_Simbel_(village)
Type of aquatic ecosystem with flowing freshwater
Industrial wastewater Sewage River measurement and modelling Baer's law Baseflow Bradshaw model Discharge (hydrology) Drainage density Exner equation Groundwater
River_ecosystem
Formerly natural waterway flowing through heavily populated area
Other common shifts in hydrology driven by urbanization include lower baseflows. This can cause problems during flood discharges. For example, flood discharges
Urban_stream
Rivers rising from chalk bedrock
Industrial wastewater Sewage River measurement and modelling Baer's law Baseflow Bradshaw model Discharge (hydrology) Drainage density Exner equation Groundwater
Chalk_stream
Lagoon near Florida, US
driver of climate variability on a global scale. Research has shown that baseflow of the Flint River has increased by 10% during El Niño and decreased by
Apalachicola_Bay
Term in fluid dynamics
to effectively degrade nutrients. Anaerobic digestion § Residence time Baseflow residence time Estuarine water circulation § Residence time Lake retention
Residence_time
River in England – third-longest in the UK
the carboniferous limestone in Derbyshire. Not only do these provide baseflows to the major tributaries, the groundwater is an important source for public
River_Trent
River
River 5 miles (8.0 km) upstream from the mouth of Big Coldwater Creek. Baseflow makes up just over half of the flow in Big Juniper Creek, while the rest
Big_Juniper_Creek
River in Greater Toronto, Ontario, Canada
Retrieved 2012-03-15. {{cite book}}: |work= ignored (help) Section 4.0 - Baseflow and water use (PDF). Toronto and Region Conservation Authority. 2010.
Etobicoke_Creek
Municipality in Lower Saxony, Germany
Lower Saxon Wadden Sea National Park, like the islands, and is very dry at Baseflow. Below the island, at a depth of about 15 meters, there is the Geest base
Wangerooge
Phosphate-producing region in Central Florida
turn, reduces baseflow to the Peace River. Some studies have indicated that reclaimed lands actually provide a more consistent baseflow because the sandier
Bone_Valley
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Qarano_River
Swiss company
company's Chief Executive Officer, previously founded a company called Baseflow, which later merged into The Network State Company before being renamed
CitizenX
Groundwater discharge into a stream
be obstructed by permafrost. Subsurface flow Groundwater energy balance Baseflow Ecohydrology Groundwater Hydrogeology Catchment hydrology Chorley, R.J
Groundwater_flow
Stream in Santa Rosa County, Florida
southward to merge into the Blackwater River near the city of Milton, Florida. Baseflow makes up about 60% of the flow in Big Coldwater Creek, while 40% is surface
Big_Coldwater_Creek
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has not been decreased due to interventions
Korowya
Water that originates during precipitation events and snow/ice melt
little infiltrates the soil, replenishes groundwater, or supplies stream baseflow in dry weather. A first flush is the initial runoff of a rainstorm. During
Stormwater
Municipality in Tigray Region, Ethiopia
temperatures are much larger than seasonal contrasts. As there is very poor baseflow in the permanent rivers, the presence of springs is of utmost importance
Haddinnet
River in the Tembien highlands of Ethiopia
Ethiopia, this contributes to groundwater recharge and increased river baseflow. Runoff mostly happens in the form of high runoff discharge events that
Graliwdo
Volcano in Peru
comes from glaciers. Meltwater from the glaciers on Coropuna sustains the baseflow of the rivers during dry periods; Coropuna is an important source of water
Coropuna
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Tsaliet
River in the Caucasus region
the year (generally in June and July), and a relatively low sustainable baseflow. Forest cover is sparse, especially in the Kura and Aras headwaters, and
Kura_(South_Caucasus_river)
Moraine in Niagara Peninsula, Canada
committed $85,000 toward the study of groundwater flow, discharge, and baseflow measurements. The original town of Fonthill is perched on the moraine,
Fonthill_Kame
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Afedena_River
in May for the Euphrates (shortly after or during the harvest). Their baseflow occurs in summer at the time of greatest heat, when evapotranspiration
Agriculture_in_Mesopotamia
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. In contrast to neighbouring rivers such as May Meqa, May Sho'ate or Graliwdo
Ab'aro
Environmental problems from uncontrolled mining
Problem? Mountaintop Removal Coal Mining Enhances and Sustains Saline Baseflows of Appalachian Watersheds". Environmental Science & Technology. 51 (15):
Environmental impact of mining
Environmental_impact_of_mining
Hydrology of drainage basins
taken from the glossary of terms in Kendall and McDonnell, 1998: aquifer baseflow delineation catchment drainage divide evaporation evapotranspiration event
Catchment_hydrology
River in the Tigray highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. These flash floods mostly occur during the evening or night, because the
May_Gabat
River in the Tembien highlands of Ethiopia
less flooding and better baseflow. Besides springs and reservoirs, irrigation is strongly dependent on the river's baseflow. Such irrigated agriculture
Qortem_Zer'a
Sediments deposited by streams exposed when water level falls
vertical distribution lies between the levels of bankfull and the typical baseflow of the river. Therefore, eroding river banks are ERS because they are usually
Exposed_riverine_sediments
Field of geochemistry and hydrology
ages. Another application involves the separation of groundwater flow and baseflow from streamflow in the field of catchment hydrology (i.e. a method of hydrograph
Isotope_hydrology
Earth's surface where water is frozen
2023). "Detecting Permafrost Active Layer Thickness Change From Nonlinear Baseflow Recession". Water Resources Research. 57 (1) e2022WR033154. Bibcode:2023WRR
Cryosphere
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Gra_Adiam
River in the Tigray highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. These flash floods mostly occur during the evening or night, because the
Giba_River
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Zeyi_River
River in the Tigray highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. These flash floods mostly occur during the evening or night, because the
Sulluh
adequate salt export to the sea through environmental flows. Additionally, baseflows in rivers must be restored by curbing excessive groundwater extraction
Water_resources_in_India
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
May_Zegzeg
Type of river
floodplain. Natural hydrograph components such as storm events (floods), baseflows, snowmelt peaks, and recession limbs, are the river-specific catalysts
Alluvial_river
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has, however, been decreased due
Amblo
Waterway in the floodplain of the Columbia River in Oregon, U.S.
Heavy rain in the winter months recharged the groundwater and provided baseflows to the slough during dry summers. Urban development, which replaced vegetation
Columbia_Slough
Wetland complex in Ontario, Canada
flooding in other areas downstream and helping to maintain and moderate baseflow conditions during the summer months. By doing so it improves both the overall
Hay_Swamp
River in Hertfordshire and Bedfordshire, England
2 in) per km fall. The River Ivel is a chalk stream, because it receives baseflow from underlying chalk aquifers. The river and its catchment area, particularly
River_Ivel
Biolog Conservation 35(2) 97–110 Closea ME & Davies‐Colley RJ (1990) Baseflow water chemistry in New Zealand rivers 2. Influence of environmental factors
Klecka's_tau
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Adawro_River
River in California, United States
in 1977. Runoff peaks in the winter and early spring, with a low summer baseflow of less than 50 cubic feet per second (1.4 m3/s). Historically, flood flows
Stony Creek (Sacramento River tributary)
Stony_Creek_(Sacramento_River_tributary)
River in the Tembien highlands of Ethiopia
floods often have a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has, however, been decreased due
May_Ayni
River in the Tigray highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. These flash floods mostly occur during the evening or night, because the
Inda_Sillasie_River
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has, however, been decreased due
Shimbula
River in the Tigray highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. These flash floods mostly occur during the evening or night, because the
Ilala_River
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Agefet
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Ch'eqofo_River
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Ruba_Bich'i_River
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Tsech'i_River
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Azef_River
Annual music industry award ceremony
Henga-Phoka Water Association, Acades, Micromek Limited, Partners in Hope, Baseflow, Atsikana Paulendo, Tengani Water Association, Tingathe, Kibebe, as well
Zikomo_Presidential_Awards
Municipality in Ethiopia
"geotourism". Geosites in the tabia include: May Qoqah river with permanent baseflow and gully control structures (log dams and check dams) Views on Melfa,
Lim'at
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
May_Meqa
River in the Tigray highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. These flash floods mostly occur during the evening or night, because the
Genfel
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has somewhat been decreased due
May_Harena
River in Wisconsin, United States
River itself, upstream of Gays Mills, are good trout habitat due to the baseflow from coldwater springs and watershed and stream projects carried out over
Kickapoo_River
River in Santa Cruz County, California, United States
bacteria and pathogen level. Groundwater use impacts on surface water baseflow supporting anadromous fisheries for coho salmon and steelhead, particularly
San_Lorenzo_River
Reduction in water level over time within a water well
This may result in poor water quality in these local water bodies as baseflow water contribution is reduced, which could result in perennial streams
Drawdown_(hydrology)
Topics referred to by the same term
The term base flow may refer to: Baseflow in hydrology Base flow (random dynamical systems) in the study of random dynamical systems in mathematics This
Base_flow
Organic carbon classification
organic matter. In the absence of extensive wetlands, bogs, or swamps, baseflow concentrations of DOC in undisturbed watersheds generally range from approximately
Dissolved_organic_carbon
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Ferrey_River
Stream in Los Angeles County, California
Press. p. 338. ISBN 978-0-520-26619-3. Zachary Croyle (2009). Analysis of Baseflow Trends Related to Upland Groundwater Pumping for Las Garzas, San Clemente
San Jose Creek (Monterey County, California)
San_Jose_Creek_(Monterey_County,_California)
River in France
its lower course by a pluvio-nival regime of meridional type with high baseflow in summer, 9.8 cubic metres per second (350 cu ft/s) in August at Moussan
Aude_(river)
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Arwadito
Aquifer in British Columbia and Washington state
Although the aquifer comprises a significant portion of the Sumas river baseflow, the majority of surface and groundwater in the region flows into the Nooksack
Abbotsford–Sumas_Aquifer
River in the Tigray highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. These flash floods mostly occur during the evening or night, because the
Agula'i_River
River in New Zealand
rivers and usually meets the water quality requirements for swimming under baseflow conditions. "Motueka River Trout Fishing". Archived from the original on
Motueka_River
Charitable humanitarian organisation
encompassed in global catchment management initiatives. As a consequence the baseflow in rivers improves, and the water can be used to establish irrigation schemes
Relief_Society_of_Tigray
Predicting and managing water resources
hydro-electric power generation), flow processes (e.g., overland, interflow, baseflow, channel flow), transport processes (e.g., sediments, nutrients, pathogens)
Hydrological_model
Dam in Taoyuan City, Taiwan
release of 299.6 million m3 (242,900 acre feet) is maintained to provide a baseflow in the lower Dahan River. About 386.3 million m3 (313,200 acre feet) of
Shihmen_Dam
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
Hurura
Unincorporated community in California, United States
on February 15, 2017. Retrieved May 3, 2022. "Hydrologic Conditions in Baseflow Reaches Pursuant to Conditions" (PDF). Archived (PDF) from the original
Santa_Lucia_Preserve
River in the United States
colonies/100mL during baseflow. The investigators compared this with fecal streptococci (stormflow: 1 to 310,000 colonies/mL; baseflow: less than 1 to 960
Shoal_Creek,_Austin,_Texas
River in the Tembien highlands of Ethiopia
floods have often a 50 to 100 times larger discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to
May_Qoqah
and soft sandstone has poor recharge and transmissivity but sustains the baseflow of many different streams. Other aquifers are situated in Cretaceous sandstones
Geology of the Democratic Republic of the Congo
Geology_of_the_Democratic_Republic_of_the_Congo
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BASEFLOW
BASEFLOW
BASEFLOW
BASEFLOW
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BASEFLOW
BASEFLOW
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BASEFLOW
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