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Relevant bibliographies by topics / Streamflow discharge

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Academic literature on the topic 'Streamflow discharge'

Author: Grafiati

Published: 4 June 2021

Last updated: 4 February 2022

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Journal articles on the topic "Streamflow discharge"

1

Gao, P., X. M. Mu, F. Wang, and R. Li. "Changes in streamflow and sediment discharge and the response to human activities in the middle reaches of the Yellow River." Hydrology and Earth System Sciences 15, no. 1 (2011): 1–10. http://dx.doi.org/10.5194/hess-15-1-2011.

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Abstract. The changes in streamflow and sediment discharge in the middle reaches of the Yellow River are a focus. In this paper, based on the precipitation, streamflow and sediment discharge series data (1950–2008), the streamflow and sediment discharge variation and its impact on precipitation/response to human activities have been analysis. The results show that significant decreasing trends in annual streamflow and sediment discharge have existed since the late 1950s in the middle reaches of the Yellow River (P = 0.01). Change-point analyses further revealed that transition years existed an

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Et. al., Dhanendra Bahekar,. "Estimation of River Discharge from Satellite Observations." Turkish Journal of Computer and Mathematics Education (TURCOMAT) 12, no. 4 (2021): 1072–83. http://dx.doi.org/10.17762/turcomat.v12i4.603.

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The role of streamflow is very important in any type of hydrologic. For very effective flood routing and hydraulic structure design, it is important to have a large dataset of past years. We now have a conceptual rainfall-runoff model that can predict streamflow based on pre-existing datasets. Because there is no or very little observed data in un-gauged basins, calibrating these models to predict daily streamflow becomes difficult. Nowadays, parameters for example river width can be observed using satellite images, and some studies show a promising associated relation between discharge and ri

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Belleville, Arnaud, Alexandre Hauet, Amélie Tacnet, and Damien Sevrez. "Recalculation of historical streamflow series. Impact assessment and valorization." E3S Web of Conferences 40 (2018): 06024. http://dx.doi.org/10.1051/e3sconf/20184006024.

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Rating curves used to calculate discharge from water level must be extrapolated beyond the range of measured discharges, due to the difficulty of measuring flood discharge. This induces large uncertainties and the flood discharge series can be unreliable. This paper presents a methodology to update and correct historical flood flows, so as to propose homogeneous and less biased data. The benefit of using hydraulic modeling is discussed. This methodology is applied to a large sample of hydrometric stations of the EDF (Electricité De France) network, and the impact on peak flows deviations is an

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Oliveira, Alisson Souza de, Antônio Marciano da Silva, Carlos Rogério de Mello, and Geovane Junqueira Alves. "Stream flow regime of springs in the Mantiqueira Mountain Range region, Minas Gerais State." CERNE 20, no. 3 (2014): 343–49. http://dx.doi.org/10.1590/01047760201420031268.

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The stream flow regime of four springs located in the Mantiqueira Mountain Range region (MG) was evaluated and correlated to the respective recharge area, relief characteristics, land cover and physical and hydrologic soil characteristics. The streamflow regime was characterized by monitoring of discharges, calculating the surface runoff and specific discharge and by modeling the discharge over the recession period using the Maillet method. As all recharge areas have similar relief the effect of it on the streamflow was not possible to identify. Analysis included determining the effect of drai

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Safeeq, M., G. E. Grant, S. L. Lewis, M. G. Kramer, and B. Staab. "A hydrogeologic framework for characterizing summer streamflow sensitivity to climate warming in the Pacific Northwest, USA." Hydrology and Earth System Sciences 18, no. 9 (2014): 3693–710. http://dx.doi.org/10.5194/hess-18-3693-2014.

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Abstract. Summer streamflows in the Pacific Northwest are largely derived from melting snow and groundwater discharge. As the climate warms, diminishing snowpack and earlier snowmelt will cause reductions in summer streamflow. Most regional-scale assessments of climate change impacts on streamflow use downscaled temperature and precipitation projections from general circulation models (GCMs) coupled with large-scale hydrologic models. Here we develop and apply an analytical hydrogeologic framework for characterizing summer streamflow sensitivity to a change in the timing and magnitude of recha

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Gao, P., X. M. Mu, F. Wang, and R. Li. "Changes in streamflow and sediment discharge and the response to human activities in the middle reaches of the Yellow River." Hydrology and Earth System Sciences Discussions 7, no. 5 (2010): 6793–822. http://dx.doi.org/10.5194/hessd-7-6793-2010.

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Abstract. The objectives of this work are: (a) to statistically test and quantify the decreasing trends of streamflow and sediment discharge in the middle reaches of the Yellow River in China during 1950–2008, (b) to identify change points or transition years of the decreasing trends, and (c) to diagnose whether the decreasing trends were caused by precipitation changes or human intervention, or both. The results show that significant decreasing trends in annual streamflow and sediment discharge have existed since the late 1950s in the middle reaches of the Yellow River (P=0.01). Change-point

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Safeeq, M., G. E. Grant, S. L. Lewis, M. G. Kramer, and B. Staab. "A geohydrologic framework for characterizing summer streamflow sensitivity to climate warming in the Pacific Northwest, USA." Hydrology and Earth System Sciences Discussions 11, no. 3 (2014): 3315–57. http://dx.doi.org/10.5194/hessd-11-3315-2014.

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Abstract. Summer streamflows in the Pacific Northwest are largely derived from melting snow and groundwater discharge. As the climate warms, diminishing snowpack and earlier snowmelt will cause reductions in summer streamflow. Most assessments of the impacts of a changing climate to streamflow make use of downscaled temperature and precipitation projections from General Circulation Models (GCMs). Projected climate simulations from these GCMs are often too coarse for planning purposes, as they do not capture smaller scale topographic controls and other important watershed processes. This uncert

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Santos, Ana Clara, Maria Manuela Portela, Andrea Rinaldo, and Bettina Schaefli. "Analytical flow duration curves for summer streamflow in Switzerland." Hydrology and Earth System Sciences 22, no. 4 (2018): 2377–89. http://dx.doi.org/10.5194/hess-22-2377-2018.

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Abstract. This paper proposes a systematic assessment of the performance of an analytical modeling framework for streamflow probability distributions for a set of 25 Swiss catchments. These catchments show a wide range of hydroclimatic regimes, including namely snow-influenced streamflows. The model parameters are calculated from a spatially averaged gridded daily precipitation data set and from observed daily discharge time series, both in a forward estimation mode (direct parameter calculation from observed data) and in an inverse estimation mode (maximum likelihood estimation). The performa

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Bidwell, V. J., R. Stenger, and G. F. Barkle. "Dynamic analysis of groundwater discharge and partial-area contribution to Pukemanga Stream, New Zealand." Hydrology and Earth System Sciences 12, no. 4 (2008): 975–87. http://dx.doi.org/10.5194/hess-12-975-2008.

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Abstract. The proportion and origin of groundwater contribution to streamflow from agricultural catchments is relevant to estimation of the effects of nitrate leached from the soil on the quality of surface waters. This study addresses the partitioning of streamflow contributions from near-surface runoff and from groundwater, each with different contributing land area, on a steep pastoral hillslope in a humid climate. The 3 ha headwater catchment of the perennial Pukemanga Stream, in the North Island of New Zealand, was instrumented for continuous observation of climatic data, streamflow and g

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Adam, Jennifer C., and Dennis P. Lettenmaier. "Application of New Precipitation and Reconstructed Streamflow Products to Streamflow Trend Attribution in Northern Eurasia." Journal of Climate 21, no. 8 (2008): 1807–28. http://dx.doi.org/10.1175/2007jcli1535.1.

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Abstract River runoff to the Arctic Ocean has increased over the last century, primarily during the winter and spring and primarily from the major Eurasian rivers. Some recent studies have suggested that the additional runoff is due to increased northward transport of atmospheric moisture (and associated increased precipitation), but other studies show inconsistencies in long-term runoff and precipitation trends, perhaps partly due to biases in the observational datasets. Through trend analysis of precipitation, temperature, and streamflow data, the authors investigate the extent to which Eura

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Dissertations / Theses on the topic "Streamflow discharge"

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Mueses-Pérez, Auristela. "Generalized non-dimensional depth-discharge rating curves tested on Florida streamflow." [Tampa, Fla] : University of South Florida, 2006. http://purl.fcla.edu/usf/dc/et/SFE0001781.

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Tecle, Aregai, Charles A. III Henke, and Charles C. Avery. "Assessing Similarities in Precipitation and Streamflow Discharge Among Three Upland Subwatersheds." Arizona-Nevada Academy of Science, 1998. http://hdl.handle.net/10150/296492.

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Mueses-PÃ©rez, Auristela. "Generalized non-dimensional depth-discharge rating curves tested on Florida streamflow." Scholar Commons, 2006. http://scholarcommons.usf.edu/etd/2639.

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A generalized non-dimensional mathematical expression has been developed to describe the rating relation of depth and discharge for intermediate and high streamflow of natural and controlled streams. The expressions have been tested against observations from forty-three stations in West-Central Florida. The intermediate-flow region model has also been validated using data from thirty additional stations in the study area. The proposed model for the intermediate flow is a log-linear equation with zero intercept and the proposed model for the high-flow region is a log-linear equation with a vari

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Meyer, Neil. "Discharge measurement in terms of pressure differences at bridge piers." Thesis, Stellenbosch : Stellenbosch University, 2000. http://hdl.handle.net/10019.1/51731.

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Thesis (M.Eng.)--Stellenbosch University, 2000.<br>ENGLISH ABSTRACT: This study entailed the investigation and evaluation of a new methodology for measuring high discharges passing through bridges. Pressure differences generated around bridge piers have been measured and related to the discharges. These pressure differences are mainly functions of downstream flow conditions. The pressure differences have been converted into velocities by applying Newton's second law expressed in terms of the laws of conservation of energy; momentum; and of power. The energy principle was re-evaluated fol

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Darienzo, Matteo. "Detection and estimation of stage-discharge rating shifts for retrospective and real-time streamflow quantification." Thesis, Université Grenoble Alpes, 2021. http://www.theses.fr/2021GRALU006.

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Les séries temporelles de débit des rivières sont établies à l'aide de "courbes de tarage", qui sont des modèles avec les hauteurs d’eau en entrée et les débits en sortie. Malheureusement, de nombreuses stations hydrométriques ont une relation hauteur-débit instable, notamment à cause de l’évolution du lit de la rivière lors des crues. Ces "détarages" posent problème à la fois pour l'établissement des séries hydrologiques de long-terme (analyse rétrospective) et pour la fourniture de données en temps réel, par exemple pour la prévision des inondations, avec des incertitudes quantifiées et fiab

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Agafonov, Leonid I., David M. Meko, and Irina P. Panyushkina. "Reconstruction of Ob River, Russia, discharge from ring widths of floodplain trees." ELSEVIER SCIENCE BV, 2016. http://hdl.handle.net/10150/622663.

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The Ob is the third largest Eurasian river supplying heat and freshwater to the Arctic Ocean. These inputs influence water salinity, ice coverage, ocean temperatures and ocean circulation, and ultimately the global climate system. Variability of Ob River flow on long time scales is poorly understood, however, because gaged flow records are short. Eleven tree-ring width chronologies of Pinus sibirica and Larix sibirica are developed from the floodplain of the Lower Ob River, analyzed for hydroclimatic signal and applied as predictors in a regression model to reconstruct 8-month average (Decembe

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Mwangi, Hosea M., Stefan Julich, Sopan D. Patil, Morag A. McDonald, and Karl-Heinz Feger. "Relative contribution of land use change and climate variability on discharge of upper Mara River, Kenya." Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2017. http://nbn-resolving.de/urn:nbn:de:bsz:14-qucosa-227067.

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Study region Nyangores River watershed, headwater catchment of Mara River basin in Kenya. Study focus Climate variability and human activities are the main drivers of change of watershed hydrology. The contribution of climate variability and land use change to change in streamflow of Nyangores River, was investigated. Mann Kendall and sequential Mann Kendall tests were used to investigate the presence and breakpoint of a trend in discharge data (1965–2007) respectively. The Budyko framework was used to separate the respective contribution of drivers to change in discharge. Future response o

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Mwangi, Hosea M., Stefan Julich, Sopan D. Patil, Morag A. McDonald, and Karl-Heinz Feger. "Relative contribution of land use change and climate variability on discharge of upper Mara River, Kenya." Elsevier, 2016. https://tud.qucosa.de/id/qucosa%3A30418.

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Study region Nyangores River watershed, headwater catchment of Mara River basin in Kenya. Study focus Climate variability and human activities are the main drivers of change of watershed hydrology. The contribution of climate variability and land use change to change in streamflow of Nyangores River, was investigated. Mann Kendall and sequential Mann Kendall tests were used to investigate the presence and breakpoint of a trend in discharge data (1965–2007) respectively. The Budyko framework was used to separate the respective contribution of drivers to change in discharge. Future response o

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Zmijewski, Nicholas. "Effects of Watershed Dynamics on Water Reservoir Operation Planning : Considering the Dynamic Effects of Streamflow in Hydropower Operation." Doctoral thesis, KTH, Vattendragsteknik, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-201612.

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Water reservoirs are used to regulate river discharge for a variety of reasons, such as flood mitigation, water availability for irrigation, municipal consumption and power production purposes. Recent efforts to increase the amount of renewable power production have seen an increase in intermittent climate-variable power production due to wind and solar power production. The additional variable energy production has increased the need for regulating the capacity of the electrical system, to which hydropower production is a significant contributor. The hydraulic impact on the time lags of flows

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Nalder, Guinevere Vivianne. "Submerged Thin Plate Weirs With Unequal Upstream and Downstream Beds." The University of Waikato, 2006. http://hdl.handle.net/10289/2383.

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This thesis describes a short study to examine the behaviour of submerged flow over a thin plate weir with differing upstream and downstream bed levels i.e. an unequal bed weir as opposed to an equal bed weir where the upstream and downstream beds are at the same level. As submerged weir flow is a function of downstream conditions, it was thought that a lower downstream bed would make submerged flow over the weir easier, This is turn suggested that; The shape of the upstream head (Hu) vs downstream head (Hd) graph would change, being initially more steep in the unequal bed case. The Froude

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Books on the topic "Streamflow discharge"

1

Lowham, H. W. Estimating streamflow from concurrent discharge measurements. Lowham Engineering, 2009.

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2

Sauer, Vernon B. Determination of error in individual discharge measurements. U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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3

Raines, Timothy H. Peak-discharge frequency and potential extreme peak discharge for natural streams in the Brazos River basin, Texas. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Raines, Timothy H. Peak-discharge frequency and potential extreme peak discharge for natural streams in the Brazos River basin, Texas. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Raines, Timothy H. Peak-discharge frequency and potential extreme peak discharge for natural streams in the Brazos River basin, Texas. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Raines, Timothy H. Peak-discharge frequency and potential extreme peak discharge for natural streams in the Brazos River basin, Texas. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Raines, Timothy H. Peak-discharge frequency and potential extreme peak discharge for natural streams in the Brazos River basin, Texas. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Raines, Timothy H. Peak-discharge frequency and potential extreme peak discharge for natural streams in the Brazos River basin, Texas. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Raines, Timothy H. Peak-discharge frequency and potential extreme peak discharge for natural streams in the Brazos River basin, Texas. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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10

Harmon, Jerry G. Streamflow, sediment discharge, and streambank erosion in Cache Creek, Yolo County, California, 1953-86. Dept. of the Interior, Geological Survey, 1989.

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Book chapters on the topic "Streamflow discharge"

1

Misra, Debasmita, Ronald P. Daanen, and Anita M. Thompson. "Discharge/Streamflow." In Encyclopedia of Earth Sciences Series. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_115.

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Irwin, Ross W., and Graham Bryant. "Effect of Subsurface Drain Discharge on Streamflow." In Hydraulic Design in Water Resources Engineering: Land Drainage. Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-662-22014-6_23.

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Bathurst, James C., Steve J. Birkinshaw, Felipe Cisneros Espinosa, and Andrés Iroumé. "Forest Impact on Flood Peak Discharge and Sediment Yield in Streamflow." In River System Analysis and Management. Springer Singapore, 2016. http://dx.doi.org/10.1007/978-981-10-1472-7_2.

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Wang, Chi-Yuen, and Michael Manga. "Stream Flow." In Lecture Notes in Earth System Sciences. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-64308-9_7.

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AbstractChanges in stream discharge after earthquakes are among the most interesting hydrologic responses because they are visible at Earth’s surface and can be dramatic. Here we focus on changes that persist for extended periods but have no obvious source. Such increases have been documented for a long time but their origins are still under debate. We first review some general characteristics of streamflow responses to earthquakes; we then discuss several mechanisms that have been proposed to explain these responses and the source of the extra water. The different hypotheses imply different crustal processes and different water–rock interactions during the earthquake cycle. In most instances, these hypotheses are under-constrained. We suggest that multiple mechanisms may be activated by an earthquake.

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Schmidt, John C., and David M. Rubin. "Regulated streamflow, fine-grained deposits, and effective discharge in canyons with abundant debris fans." In Geophysical Monograph Series. American Geophysical Union, 1995. http://dx.doi.org/10.1029/gm089p0177.

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"The stage-discharge relation." In Streamflow Measurement. CRC Press, 2002. http://dx.doi.org/10.1201/9781482271485-10.

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"The stage–discharge relation." In Streamflow Measurement. CRC Press, 2008. http://dx.doi.org/10.1201/9781482265880-13.

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"The stage–fall–discharge method of streamflow measurement." In Streamflow Measurement. CRC Press, 2008. http://dx.doi.org/10.1201/9781482265880-18.

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"The stage-fall-discharge method of stream flow measurement." In Streamflow Measurement. CRC Press, 2002. http://dx.doi.org/10.1201/9781482271485-14.

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Gore, James A. "Discharge Measurements and Streamflow Analysis." In Methods in Stream Ecology. Elsevier, 2007. http://dx.doi.org/10.1016/b978-012332908-0.50005-x.

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Conference papers on the topic "Streamflow discharge"

1

Clayton, Noah, W. Payton Gardner, and Hilary Martens. "RELATING GEODETIC DEFLECTION TO STREAMFLOW DISCHARGE THROUGH STORAGE-DISCHARGE RELATIONSHIP." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359345.

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Capesius, Joseph P., Joseph R. Sullivan, Cory A. Williams, and Greg B. O'Neill. "Ice-Affected Streamflow Records Using Tracer-Dilution Discharge Methods." In Hydraulic Measurements and Experimental Methods Specialty Conference (HMEM) 2002. American Society of Civil Engineers, 2002. http://dx.doi.org/10.1061/40655(2002)53.

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Areerachakul, Sirilak, and Prem Junsawang. "Rainfall-Runoff relationship for streamflow discharge forecasting by ANN modelling." In 2014 World Congress on Sustainable Technologies (WCST). IEEE, 2014. http://dx.doi.org/10.1109/wcst.2014.7030090.

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Ledvinka, Ondrej, and Pavel Coufal. "DEVELOPMENT OF STREAMFLOW DROUGHT INDICES IN THE MORAVA RIVER BASIN." In XXVII Conference of the Danubian Countries on Hydrological Forecasting and Hydrological Bases of Water Management. Nika-Tsentr, 2020. http://dx.doi.org/10.15407/uhmi.conference.01.14.

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The territory of Czechia currently suffers from a long-lasting drought period which has been a subject of many studies, including the hydrological ones. Previous works indicated that the basin of the Morava River, a left-hand tributary of the Danube, is very prone to the occurrence of dry spells. It also applies to the development of various hydrological time series that often show decreases in the amount of available water. The purpose of this contribution is to extend the results of studies performed earlier and, using the most updated daily time series of discharge, to look at the situation

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Ferry, Veronica, Dakota Little, and J. P. Gannon. "CONCENTRATION-DISCHARGE RELATIONSHIPS HIGHLIGHT DIFFERENCES IN STREAMFLOW GENERATION BETWEEN TWO TRIBUTARIES IN A HEADWATER CATCHMENT." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-312496.

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Kiang, Julie, Robert Mason, and Timothy Cohn. "A survey of the uncertainty in stage-discharge rating curves and streamflow records in the United States." In The International Conference On Fluvial Hydraulics (River Flow 2016). CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-114.

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Miranda, Danny, and Jonathan A. Nourse. "REAL-TIME RESPONSE OF STREAMFLOW AND SPRING DISCHARGE TO PRECIPITATION RECHARGE EVENTS IN ICEHOUSE CANYON WATERSHED, EASTERN SAN GABRIEL MOUNTAINS, CALIFORNIA." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274722.

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Prestegaard, Karen, Haley Talbot-Wendlandt, Dilanka Athukorala, and Susan Ziegler. "STREAMFLOW IN A BOREAL CATCHMENT IS PRIMARILY VIA SUBSURFACE FLOW PATHS, BUT RAPID SUBSURFACE FLOW THROUGH SHALLOW MOSS AND ORGANIC HORIZONS CONTRIBUTES NEW WATER TO STREAM DISCHARGE." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359295.

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Ferris, Gerry, Patrick Grover, and Aron Zahradka. "Real Time Rainfall Monitoring for Pipeline Geohazards." In ASME-ARPEL 2021 International Pipeline Geotechnical Conference. American Society of Mechanical Engineers, 2021. http://dx.doi.org/10.1115/ipg2021-63162.

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Abstract Oil and gas pipelines are subjected to multiple types of geohazards which cause pipeline failures (loss of containment); two of the most common types occur at watercourse crossings and at landslides. At watercourse crossings, the most common geohazard which causes pipeline failures is flooding during which excessive scour may result in the exposure of the buried pipeline and if the exposure results in a free spanning pipeline, then this may fail due to fatigue caused by cyclic loading from vortex-induced vibration. Fortunately the free span length and water velocity combinations that

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Reports on the topic "Streamflow discharge"

1

Hamill, Daniel, and Gabrielle David. Hydrologic analysis of field delineated ordinary high water marks for rivers and streams. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/41681.

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Streamflow influences the distribution and organization of high water marks along rivers and streams in a landscape. The federal definition of ordinary high water mark (OHWM) is defined by physical and vegetative field indicators that are used to identify inundation extents of ordinary high water levels without any reference to the relationship between streamflow and regulatory definition. Streamflow is the amount, or volume, of water that moves through a stream per unit time. This study explores regional characteristics and relationships between field-delineated OHWMs and frequency-magnitude

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Wagner, Anna, Christopher Hiemstra, Glen Liston, Katrina Bennett, Dan Cooley, and Arthur Gelvin. Changes in climate and its effect on timing of snowmelt and intensity-duration-frequency curves. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/41402.

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Snow is a critical water resource for much of the U.S. and failure to account for changes in climate could deleteriously impact military assets. In this study, we produced historical and future snow trends through modeling at three military sites (in Washington, Colorado, and North Dakota) and the Western U.S. For selected rivers, we performed seasonal trend analysis of discharge extremes. We calculated flood frequency curves and estimated the probability of occurrence of future annual maximum daily rainfall depths. Additionally, we generated intensity-duration-frequency curves (IDF) to find r

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Streamflow, sediment discharge, and streambank erosion in Cache Creek, Yolo County, California, 1953-86. US Geological Survey, 1989. http://dx.doi.org/10.3133/wri884188.

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Computer programs for describing the recession of ground-water discharge and for estimating mean ground-water recharge and discharge from streamflow record. US Geological Survey, 1993. http://dx.doi.org/10.3133/wri934121.

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SWGW; a computer program for estimating ground-water discharge to a stream using streamflow data. US Geological Survey, 1996. http://dx.doi.org/10.3133/wri964071.

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Potential errors associated with stage-discharge relations for selected streamflow-gaging stations, Maricopa County, Arizona. US Geological Survey, 2001. http://dx.doi.org/10.3133/wri004224.

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Computer programs for describing the recession of ground-water discharge and for estimating mean ground-water recharge and discharge from streamflow records-update. US Geological Survey, 1998. http://dx.doi.org/10.3133/wri984148.

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Automatic tracer-dilution method used for stage-discharge ratings and streamflow hydrographs on small Iowa streams. US Geological Survey, 1990. http://dx.doi.org/10.3133/wri894187.

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Streamflow, ground-water recharge and discharge, and characteristics of surficial deposits in Buzzards Bay basin, southeastern Massachusetts. US Geological Survey, 1995. http://dx.doi.org/10.3133/wri954234.

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Relations between discharge and wetted perimeter and other hydraulic-geometry characteristics at selected streamflow-gaging stations in Massachusetts. US Geological Survey, 1998. http://dx.doi.org/10.3133/wri984094.

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