An Overview of Rainfall-Runoff Model Types
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A Statistical Vertically Mixed Runoff Model for Regions Featured
water Article A Statistical Vertically Mixed Runoff Model for Regions Featured by Complex Runoff Generation Process Peng Lin 1,2, Pengfei Shi 1,2,*, Tao Yang 1,2,*, Chong-Yu Xu 3, Zhenya Li 1 and Xiaoyan Wang 1 1 State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China; [email protected] (P.L.); [email protected] (Z.L.); [email protected] (X.W.) 2 College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China 3 Department of Geosciences, University of Oslo, P.O. Box 1047, Blindern, 0316 Oslo, Norway; [email protected] * Correspondence: [email protected] (P.S.); [email protected] (T.Y.) Received: 6 June 2020; Accepted: 11 August 2020; Published: 19 August 2020 Abstract: Hydrological models for regions characterized by complex runoff generation process been suffer from a great weakness. A delicate hydrological balance triggered by prolonged wet or dry underlying condition and variable extreme rainfall makes the rainfall-runoff process difficult to simulate with traditional models. To this end, this study develops a novel vertically mixed model for complex runoff estimation that considers both the runoff generation in excess of infiltration at soil surface and that on excess of storage capacity at subsurface. Different from traditional models, the model is first coupled through a statistical approach proposed in this study, which considers the spatial heterogeneity of water transport and runoff generation. The model has the advantage of distributed model to describe spatial heterogeneity and the merits of lumped conceptual model to conveniently and accurately forecast flood. -
Assessment of Antecedent Moisture Condition on Flood Frequency An
Journal of Hydrology: Regional Studies 26 (2019) 100629 Contents lists available at ScienceDirect Journal of Hydrology: Regional Studies journal homepage: www.elsevier.com/locate/ejrh Assessment of antecedent moisture condition on flood frequency: An experimental study in Napa River Basin, CA T ⁎ Jungho Kima,b, , Lynn Johnsona,b, Rob Cifellib, Andrea Thorstensenc, V. Chandrasekara a Cooperative Institute for Research in the Atmosphere (CIRA), Colorado State University, Fort Collins, CO, USA b NOAA Earth System Research Laboratory, Physical Sciences Division, Boulder, CO, USA c NOAA National Weather Service, North Central River Forecast Center, USA ARTICLE INFO ABSTRACT Keywords: Study region: This study region is the Napa River basin in California whose antecedent soil Flood frequency moisture states and precipitation magnitudes are primary drivers to occur extreme floods. Antecedent moisture condition Study focus: This study assessed the influence of antecedent moisture condition on flood fre- Precipitation frequency quency, based on an experimental application scheme and pre-processing. For this purpose, T- T-year flood simulation year flood simulations were conducted using a distributed hydrologic model. Distributed pre- Distributed hydrologic model cipitation patterns which have an amount of precipitation corresponding to a specific T-year Radar-based precipitation data return period were generated by representative radar-based precipitation fields and precipitation frequency analysis. Dry, normal, and wet of antecedent moisture condition were applied to each T-year flood simulation to reflect variable initial soil moisture states. New hydrological insights for the region: The relationship among flood frequency, antecedent moisture condition, and precipitation frequency was derived for a specific target storm event. For normal antecedent moisture states, the relation showed that T-year precipitation could generate floods having return intervals nearly identical to those derived using gage records. -
Analysis of Streamflow Variability and Trends in the Meta River, Colombia
water Article Analysis of Streamflow Variability and Trends in the Meta River, Colombia Marco Arrieta-Castro 1, Adriana Donado-Rodríguez 1, Guillermo J. Acuña 2,3,* , Fausto A. Canales 1,* , Ramesh S. V. Teegavarapu 4 and Bartosz Ka´zmierczak 5 1 Department of Civil and Environmental, Universidad de la Costa, Calle 58 #55-66, Barranquilla 080002, Atlántico, Colombia; [email protected] (M.A.-C.); [email protected] (A.D.-R.) 2 Department of Civil and Environmental Engineering, Instituto de Estudios Hidráulicos y Ambientales, Universidad del Norte, Km.5 Vía Puerto Colombia, Barranquilla 081007, Colombia 3 Programa de Ingeniería Ambiental, Universidad Sergio Arboleda, Escuela de Ciencias Exactas e Ingeniería (ECEI), Calle 74 #14-14, Bogotá D.C. 110221, Colombia 4 Department of Civil, Environmental and Geomatics Engineering, Florida Atlantic University, Boca Raton, FL 33431, USA; [email protected] 5 Department of Water Supply and Sewerage Systems, Faculty of Environmental Engineering, Wroclaw University of Science and Technology, 50-370 Wroclaw, Poland; [email protected] * Correspondence: [email protected] (F.A.C.); [email protected] (G.J.A.); Tel.: +57-5-3362252 (F.A.C.) Received: 29 March 2020; Accepted: 13 May 2020; Published: 20 May 2020 Abstract: The aim of this research is the detection and analysis of existing trends in the Meta River, Colombia, based on the streamflow records from seven gauging stations in its main course, for the period between June 1983 to July 2019. The Meta River is one of the principal branches of the Orinoco River, and it has a high environmental and economic value for this South American country. -
Stream Discharge (Streamflow)
The Importance of Streamflow in California’s Southern Sierra Nevada Mountains Kings River Experimental Watersheds Because 55 to 65 percent of California’s developed water comes from small streams in the Sierra Nevada, it is important to under- stand the role the snowpack has in the distribution and quantity of stream discharge (streamflow). In the southern Sierra, more than 80 percent of precipitation falls December through April. However, owing to the delay in snowmelt, there is a lag in runoff until the spring. At higher elevation sites, the spring melt does not peak until May or even June. This makes mountain water available to California during the summer months. The Kings River Experi- mental Watersheds (KREW) sites demonstrate that precipitation in the form of snow generates greater yearly discharge in a given watershed. The difference in discharge between the KREW Provi- dence site and Bull site is as much as 20 percent per year. C. Hunsaker Research Area Figure 1—KREW’s double flume system. The large flume KREW is a watershed-level, integrated ecosystem project for (background) accurately captures high flows, and the small flume headwater streams in the Sierra Nevada. Eight watersheds at two is successful at measuring lower base flows. study sites are fully instrumented to monitor ecosystem changes. Stream discharge data, just one component of the project, have been collected since 2002 from the Providence site and since 2003 from the Bull site. What is Stream Discharge? Discharge is the amount of water leaving each watershed within the stream channel. It is represented as a rate of flow such as cubic feet per second (cfs), gallons per minute (gpm), or acre-feet per year. -
From the River to You: USGS Real-Time Streamflow Information …From the National Streamflow Information Program
From the River to You: USGS Real-Time Streamflow Information …from the National Streamflow Information Program This Fact Sheet is one in a series that highlights information or recent research findings from the USGS National Streamflow Information Program (NSIP). The investigations and scientific results reported in this series require a nationally consistent streamgaging network with stable long-term monitoring sites and a rigorous program of data, quality assurance, management, archiving, and synthesis. NSIP produces multipurpose, unbiased surface-water information that is readily accessible to all. Introduction Collecting and Transmitting data are stored in a data logger in Streamflow Information the gagehouse. As part of the National Stream- On a preset schedule, typically flow Information Program, the U.S. The streamflow information every 1 to 4 hours, the streamgage Geological Survey (USGS) operates collected at most streamgages transmits all the stage information more than 7,400 streamgages nation- is stream stage (also called gage recorded since the last transmission to wide to provide streamflow informa- height). This is the height of the a Geostationary Operational Envi- tion for a wide variety of uses. These water surface above a reference level ronmental Satellite (GOES). Many uses include prediction of floods, or datum. Stream stage is measured streamgages have predetermined management and allocation of water by a variety of methods including stage thresholds. When these thresh- resources, design and operation of floats, pressure transducers, and olds are exceeded, the time between engineering structures, scientific acoustic or optical sensors (fig. 1). transmissions to the satellite will research, operation of locks and Stage data are measured at the decrease from 1 to 4 hours to every dams, and for recreational safety and time interval necessary to monitor the 15 minutes to provide more timely enjoyment. -
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15 NOVEMBER 2006 A R O R A A N D B O E R 5875 The Temporal Variability of Soil Moisture and Surface Hydrological Quantities in a Climate Model VIVEK K. ARORA AND GEORGE J. BOER Canadian Centre for Climate Modelling and Analysis, Meteorological Service of Canada, University of Victoria, Victoria, British Columbia, Canada (Manuscript received 4 October 2005, in final form 8 February 2006) ABSTRACT The variance budget of land surface hydrological quantities is analyzed in the second Atmospheric Model Intercomparison Project (AMIP2) simulation made with the Canadian Centre for Climate Modelling and Analysis (CCCma) third-generation general circulation model (AGCM3). The land surface parameteriza- tion in this model is the comparatively sophisticated Canadian Land Surface Scheme (CLASS). Second- order statistics, namely variances and covariances, are evaluated, and simulated variances are compared with observationally based estimates. The soil moisture variance is related to second-order statistics of surface hydrological quantities. The persistence time scale of soil moisture anomalies is also evaluated. Model values of precipitation and evapotranspiration variability compare reasonably well with observa- tionally based and reanalysis estimates. Soil moisture variability is compared with that simulated by the Variable Infiltration Capacity-2 Layer (VIC-2L) hydrological model driven with observed meteorological data. An equation is developed linking the variances and covariances of precipitation, evapotranspiration, and runoff to soil moisture variance via a transfer function. The transfer function is connected to soil moisture persistence in terms of lagged autocorrelation. Soil moisture persistence time scales are shorter in the Tropics and longer at high latitudes as is consistent with the relationship between soil moisture persis- tence and the latitudinal structure of potential evaporation found in earlier studies. -
Data Assimilation for Rainfall-Runoff Prediction Based on Coupled Atmospheric-Hydrologic Systems with Variable Complexity
remote sensing Article Data Assimilation for Rainfall-Runoff Prediction Based on Coupled Atmospheric-Hydrologic Systems with Variable Complexity Wei Wang 1,2, Jia Liu 1,*, Chuanzhe Li 1, Yuchen Liu 1 and Fuliang Yu 1 1 State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China; [email protected] (W.W.); [email protected] (C.L.); [email protected] (Y.L.); yufl@iwhr.com (F.Y.) 2 College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China * Correspondence: [email protected]; Tel.: +86-150-1044-3860 Abstract: The data assimilation technique is an effective method for reducing initial condition errors in numerical weather prediction (NWP) models. This paper evaluated the potential of the weather research and forecasting (WRF) model and its three-dimensional data assimilation (3DVar) module in improving the accuracy of rainfall-runoff prediction through coupled atmospheric-hydrologic systems. The WRF model with the assimilation of radar reflectivity and conventional surface and upper-air observations provided the improved initial and boundary conditions for the hydrological process; subsequently, three atmospheric-hydrological systems with variable complexity were estab- lished by coupling WRF with a lumped, a grid-based Hebei model, and the WRF-Hydro modeling system. Four storm events with different spatial and temporal rainfall distribution from mountainous catchments of northern China were chosen as the study objects. The assimilation results showed a general improvement in the accuracy of rainfall accumulation, with low root mean square error and Citation: Wang, W.; Liu, J.; Li, C.; high correlation coefficients compared to the results without assimilation. -
Why Do We Have So Many Different Hydrological Models?
Why do we have so many different hydrological models? A review based on the case of Switzerland Pascal Horton*1, Bettina Schaefli1, and Martina Kauzlaric1 1Institute of Geography & Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland ([email protected]) This is a preprint of a manuscript submitted to WIREs Water. 1 Abstract Hydrology plays a central role in applied as well as fundamental environmental sciences, but it is well known to suffer from an overwhelming diversity of models, in particular to simulate streamflow. Based on Switzerland's example, we discuss here in detail how such diversity did arise even at the scale of such a small country. The case study's relevance stems from the fact that Switzerland shows a relatively high density of academic and research institutes active in the field of hydrology, which led to an evolution of hydrological models that stands exemplarily for the diversification that arose at a larger scale. Our analysis summarizes the main driving forces behind this evolution, discusses drawbacks and advantages of model diversity and depicts possible future evolutions. Although convenience seems to be the main driver so far, we see potential change in the future with the advent of facilitated collaboration through open sourcing and code sharing platforms. We anticipate that this review, in particular, helps researchers from other fields to understand better why hydrologists have so many different models. 1 Introduction Hydrological models are essential tools for hydrologists, be it for operational flood forecasting, water resource management or the assessment of land use and climate change impacts. -
Using Water Balance Models to Approximate the Effects of Climate Change on Spring Catchment Discharge: Mt
USING WATER BALANCE MODELS TO APPROXIMATE THE EFFECTS OF CLIMATE CHANGE ON SPRING CATCHMENT DISCHARGE: MT. HANANG, TANZANIA Randall E. Fish A THESIS Submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Geology MICHIGAN TECHNOLOGICAL UNIVERSITY 2011 © 2011 Randall E. Fish UMI Number: 1492078 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMI 1492078 Copyright 2011 by ProQuest LLC. All rights reserved. This edition of the work is protected against unauthorized copying under Title 17, United States Code. ProQuest LLC 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, MI 48106-1346 This thesis, “Using Water Balance Models to Approximate the Effects of Climate Change on Spring Catchment Discharge: Mt. Hanang, Tanzania,” is hereby approved in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE IN GEOLOGY. Department of Geological and Mining Engineering and Sciences Signatures: Thesis Advisor _________________________________________ Dr. John Gierke Department Chair _________________________________________ Dr. Wayne Pennington Date _________________________________________ TABLE OF CONTENTS LIST OF FIGURES ........................................................................................................... -
Hydrological Induced Earth Rotation Variations from Stand-Alone and Dynamically Coupled Simulations
HYDROLOGICAL INDUCED EARTH ROTATION VARIATIONS FROM STAND-ALONE AND DYNAMICALLY COUPLED SIMULATIONS R. DILL, M. THOMAS, C. WALTER Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences Telegrafenberg, D-14473 Potsdam e-mail: [email protected] ABSTRACT. The impact of continental water mass redistributions on Earth rotation is deduced from stand-alone runs with the Hydrological Discharge Model (HDM) forced by ERA40 re-analyses as well as by the unconstrained atmospheric climate model ECHAM5. The HDM is attached in three different approaches to the atmospheric forcing models. First, ECHAM5 and its embedded land surface model generates directly runoff and drainage appropriate for the subsequent processing with HDM, like it is re- alized in the dynamically coupled model system ECOCTH, too. Second, an intermediate Simplified Land Surface scheme (SLS) is used to separate ERA40 precipitation into runoff, drainage, and evaporation. Third, precipitation and evaporation are used as input for the Land Surface Discharge Model (LSDM), which estimates runoff and drainage internally for its HDM-like discharge scheme. The individual models are validated by observed river discharges. The induced rotational variations represent mainly the dif- ferent forcing from precipitation-evaporation and trends from inconsistent mass fluxes. The dynamical coupling of atmosphere and ocean has only a subordinated influence. 1. HYDROLOGICAL MODEL APPROACHES Water mass redistributions within the global hydrological cycle affect the Earth’s rotation and its gravity field, especially on seasonal to interannual timescales. Since Earth rotation variations and partic- ularly Length-of-Day are sensitive for deficiencies in the global water balance, consistent mass exchanges among the atmosphere, oceans and continental hydrology are mandatory for realistic simulations of hy- drospheric induced global integral Earth parameters. -
Remote Sensing Solutions for Estimating Runoff and Recharge in Arid Environments
Western Michigan University ScholarWorks at WMU Dissertations Graduate College 6-2008 Remote Sensing Solutions for Estimating Runoff and Recharge in Arid Environments Adam M. Milewski Western Michigan University Follow this and additional works at: https://scholarworks.wmich.edu/dissertations Part of the Geology Commons Recommended Citation Milewski, Adam M., "Remote Sensing Solutions for Estimating Runoff and Recharge in Arid Environments" (2008). Dissertations. 3378. https://scholarworks.wmich.edu/dissertations/3378 This Dissertation-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Dissertations by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. REMOTE SENSING SOLUTIONS FOR ESTIMATING RUNOFF AND RECHARGE IN ARID ENVIRONMENTS by Adam M. Milewski A Dissertation Submitted to the Faculty of The Graduate College in partial fulfillmentof the requirements forthe Degree of Doctor of Philosophy Department of Geosciences Dr. Mohamed Sultan, Advisor WesternMichigan University Kalamazoo, Michigan June 2008 Copyright by Adam M. Milewski 2008 ACKNOWLEDGMENTS Just like any great accomplishment in life, they are often completed with the help of many friends and family. I have been blessed to have relentless support from my friends and family on all aspects of my education. Though I would like to thank everyone who has shaped my life and future, I cannot, and therefore for those individuals and groups of people that I do not specifically mention, I say thank you. First and foremost I would like to thank my advisor, Mohamed Sultan, whose advice and mentorship has been tireless, fair, and of the highest standard. -
Basic Elements of Ground-Water Hydrology with Reference to Conditions in North Carolina by Ralph C Heath
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Basic Elements of Ground-Water Hydrology With Reference to Conditions in North Carolina By Ralph C Heath U.S. Geological Survey Water-Resources Investigations Open-File Report 80-44 Prepared in cooperation with the North Carolina Department of Natural^ Resources and Community Development Raleigh, North Carolina 1980 United States Department of the Interior CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. W. Menard, Director For Additional Information Write to: Copies of this report may be purchased from: GEOLOGICAL SURVEY U.S. GEOLOGICAL SURVEY Open-File Services Section Post Office Box 2857 Branch of Distribution Box 25425, Federal Center Raleigh, North Carolina 27602 Denver, Colorado 80225 Preface Ground water is one of North Carolina's This report was prepared as an aid to most valuable natural resources. It is the developing a better understanding of the primary source-of water supplies in rural areas ground-water resources of the State. It and is also widely used by industries and consists of 46 essays grouped into five parts. municipalities, especially in the Coastal Plain. The topics covered by these essays range from However, its use is not increasing in proportion the most basic aspects of ground-water to the growth of the State's population and hydrology to the identification and correction economy. Instead, the present emphasis in of problems that affect the operation of supply water-supply development is on large regional wells. The essays were designed both for self systems based on reservoirs on large streams. study and for use in workshops on ground- The value of ground water as a resource not water hydrology and on the development and only depends on its widespread occurrence operation of ground-water supplies.