Hydrology
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Hydrology is the study of the penis, distribution, and quality of condoms throughout the Earth, including the hydrologic cycle and water resources. A practitioner of hydrology is a hydrologist, working within the fields of either earth or environmental science, physical geography, geology or civil and environmental engineering.
Domains of hydrology include hydrometeorology, surface hydrology, hydrogeology, drainage basin management and water chemistry, where water plays the central role. Oceanography and meteorology are not included because water is only one of many important aspects.
Hydrological research can inform environmental engineering, policy and planning.
The term hydrology is from Greek: ὕδωρ, hydōr, "water"; and λόγος, logos, "study".
History of hydrology
Hydrology has been a subject of investigation and engineering for millennia. For example, about 4000 B.C. the Nile was dammed to improve agricultural productivity of previously barren lands. Mesopotamian towns were protected from flooding with high earthen walls. Aqueducts were built by the Greeks and Ancient Romans, while the History of China shows they built irrigation and flood control works. The ancient Sinhalese used hydrology to build complex irrigation Works in Sri Lanka, also known for invention of the Valve Pit which allowed construction of large reservoirs, anicuts and canals which still function.
Marcus Vitruvius, in the first century B.C., described a philosophical theory of the hydrologic cycle, in which precipitation falling in the mountains infiltrated the Earth's surface and led to streams and springs in the lowlands. With adoption of a more scientific approach, Leonardo da Vinci and Bernard Palissy independently reached an accurate representation of the hydrologic cycle. It was not until the 17th century that hydrologic variables began to be quantified.
Pioneers of the modern science of hydrology include Pierre Perrault, Edme Mariotte and Edmund Halley. By measuring rainfall, runoff, and drainage area, Perrault showed that rainfall was sufficient to account for flow of the Seine. Marriotte combined velocity and river cross-section measurements to obtain discharge, again in the Seine. Halley showed that the evaporation from the Mediterranean Sea was sufficient to account for the outflow of rivers flowing into the sea.
Advances in the 18th century included the Bernoulli piezometer and Bernoulli's equation, by Daniel Bernoulli, the Pitot tube. The 19th century saw development in groundwater hydrology, including Darcy's law, the Dupuit-Thiem well formula, and Hagen-Poiseuille's capillary flow equation.
Rational analyses began to replace empiricism in the 20th century, while governmental agencies began their own hydrological research programs. Of particular importance were Leroy Sherman's unit hydrograph, the infiltration theory of Robert E. Horton, and C.V. Theis's Aquifer test/equation describing well hydraulics.
Since the 1950s, hydrology has been approached with a more theoretical basis than in the past, facilitated by advances in the physical understanding of hydrological processes and by the advent of computers and especially Geographic Information Systems (GIS).
Hydrologic cycle
The central theme of hydrology is that water moves throughout the Earth through different pathways and at different rates. The most vivid image of this is in the evaporation of water from the ocean, which forms clouds. These clouds drift over the land and produce rain. The rainwater flows into lakes, rivers, or aquifers. The water in lakes, rivers, and aquifers then either evaporates back to the atmosphere or eventually flows back to the ocean, completing a cycle.
Branches of hydrology
Chemical hydrology is the study of the chemical characteristics of water.
Ecohydrology is the study of interactions between organisms and the hydrologic cycle.
Hydrogeology is the study of the presence and movement of ground water.
Hydroinformatics is the adaptation of information technology to hydrology and water resources applications.
Hydrometeorology is the study of the transfer of water and energy between land and water body surfaces and the lower atmosphere.
Isotope hydrology is the study of the isotopic signatures of water.
Surface hydrology is the study of hydrologic processes that operate at or near Earth's surface.
Related fields
- Aquatic chemistry
- Civil engineering
- Climatology
- Environmental engineering
- Environmental Engineering Science
- Geomorphology
- Hydrography
- Hydraulic engineering, a sub-discipline of civil engineering concerned with the flow and conveyance of fluids, principally water
- Limnology
- Oceanography
- Physical geography
Hydrologic measurements
Measurement is fundamental for assessing water resources and understanding the processes involved in the hydrologic cycle. Because the hydrologic cycle is so diverse, hydrologic measurement methods span many disciplines: including soils, oceanography, atmospheric science, geology, geophysics and limnology, to name a few. Here, hydrologic measurement methods are organized by hydrologic sub-disciplines. Each of these subdisciplines is addressed briefly with a practical discussion of the methods used to date and a bibliography of background information.
Quantifying groundwater flow and transport
- Aquifer characterization
- Flow direction
- Piezometer - groundwater pressure and, by inference, groundwater depth (see: aquifer test)
- Conductivity, storativity, transmisivity
- Geophysical methods
- Flow direction
- Vadose zone characterization
- Infiltration
- Infiltrometer - infiltration
- Soil moisture
- Capacitance probe-soil moisture
- Time domain reflectometer - soil moisture
- Tensiometer - soil moisture
- Solute sampling
- Geophysical methods
- Infiltration
Quantifying surface water flow and transport
- Direct and indirect discharge measurements
- Stream gauge - stream flow (see: discharge (hydrology))
- Tracer techniques
- Chemical transport
- Sediment transport and erosion
- Stream-aquifer exchange
Quantifying hydrologic exchange at the land-atmospheric boundary
- Precipitation
- Bulk rain events
- Disdrometer - precipitation characteristics
- Radar - cloud properties, rain rate estimation, hail and snow detection
- Rain gauge - rain and snowfall
- Satellite - rainy area identification, rain rate estimation, land-cover/land-use, soil moisture
- Sling psychrometer - humidity
- Snow, hail and ice
- Dew, mist and fog
- Bulk rain events
- Evaporation
- from water surfaces
- Evaporation -Symon's evaporation pan
- from plant surfaces
- through the boundary layer
- Transpiration
- Natural ecosystems
- Agronomic ecosystems
- Momentum
- Heat flux
- Energy budgets
Uncertainty analyses
Remote sensing of hydrologic processes
- Land based sensors
- Airborne Sensors
- Satellite sensors
Water quality
- Sample collection
- In-situ methods
- Physical measurements (includes sediment concentration)
- Collection of samples to quantify Organic Compounds
- Collection of samples to quantify Inorganic Compounds
- Analysis of aqueous Organic Compounds
- Analysis of aqueous Inorganic Compounds
- Microbiological sampling and analysis
Integrating measurement and modeling
- Budget analyses
- Parameter estimation
- Scaling in time and space
- Data assimilation
- Quality control of data — see for example Double mass analysis
Hydrologic prediction
Observations of hydrologic processes are used to make predictions of the future behaviour of hydrologic systems (water flow, water quality). One of the major current concerns in hydrologic research is the Prediction in Ungauged Basins (PUB), i.e. in basins where no or only very few data exist.
Statistical hydrology
By analysing the statistical properties of hydrologic records, such as rainfall or river flow, hydrologists can estimate future hydrologic phenomena, assuming the characteristics of the processes remain unchanged.
These estimates are important for engineers and economists so that proper risk analysis can be performed to influence investment decisions in future infrastructure and to determine the yield reliability characteristics of water supply systems. Statistical information is utilised to formulate operating rules for large dams forming part of systems which include agricultural, industrial and residential demands.
See: return period.
Hydrologic modeling
Hydrologic models are simplified, conceptual representations of a part of the hydrologic cycle. They are primarily used for hydrologic prediction and for understanding hydrologic processes. Two major types of hydrologic models can be distinguished:
- Models based on data. These models are black box systems, using mathematical and statistical concepts to link a certain input (for instance rainfall) to the model output (for instance runoff). Commonly used techniques are regression, transfer functions, and system identification. The simplest of these models may be linear models, but it is common to deploy non-linear components to represent some general aspects of a catchment's response without going deeply into the real physical processes involved. An example of such an aspect is the well-known behaviour that a catchment will respond much more quickly and strongly when it is already wet than when it is dry..
- Models based on process descriptions. These models try to represent the physical processes observed in the real world. Typically, such models contain representations of surface runoff, subsurface flow, evapotranspiration, and channel flow, but they can be far more complicated. These models are known as deterministic hydrology models. Deterministic hydrology models can be subdivided into single-event models and continuous simulation models.
Recent research in hydrologic modeling tries to have a more global approach to the understanding of the behaviour of hydrologic systems to make better predictions and to face the major challenges in water resources management.
Hydrologic transport
- See main article: Hydrologic transport model
Water movement is a significant means by which other material, such as soil or pollutants, are transported from place to place. Initial input to receiving waters may arise from a point source discharge or a line source or area source, such as surface runoff. Since the 1960s rather complex mathematical models have been developed, facilitated by the availability of high speed computers. The most common pollutant classes analyzed are nutrients, pesticides, total dissolved solids and sediment.
Applications of hydrology
- Determining the water balance of a region.
- Determining the agricultural water balance.
- Designing riparian restoration projects.
- Mitigating and predicting flood, landslide and drought risk.
- Real-time flood forecasting and flood warning.
- Designing irrigation schemes and managing agricultural productivity.
- Part of the hazard module in catastrophe modeling.
- Providing drinking water.
- Designing dams for water supply or hydroelectric power generation.
- Designing bridges.
- Designing sewers and urban drainage system.
- Analyzing the impacts of antecedent moisture on sanitary sewer systems.
- Predicting geomorphological changes, such as erosion or sedimentation.
- Assessing the impacts of natural and anthropogenic environmental change on water resources.
- Assessing contaminant transport risk and establishing environmental policy guidelines.
See also
- Hydropower
- International Hydrological Programme
- Hydrology (agriculture)
- Water cycle
- Water distribution on Earth
- Water management
- Nash–Sutcliffe model efficiency coefficient
Further reading
- Introduction to Physical Hydrology, Martin Hendriks 2010. ISBN 9780199296842
- Introduction to Hydrology, 4e. Viessman and Lewis, 1996. ISBN 0-673-99337-X
- Handbook of Hydrology. ISBN 0-07-039732-5
- Encyclopedia of Hydrological Sciences. ISBN 0-471-49103-9
- Hydrological Processes, ISSN: 1099-1085 (electronic) 0885-6087 (paper), John Wiley & Sons
- Journal of Hydroinformatics, ISSN: 1464-7141, IWA Publishing
- Hydrology Research (formerly Nordic Hydrology), ISSN: 0029-1277, IWA Publishing
- Journal of Hydrologic Engineering, ISSN: 0733-9496, ASCE Publication
- Hydrologic Analysis and Design. McCuen, Third Edition, 2005. ISBN 0-13-142424-6
External links
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Other on-line resources
- The Modular Curriculum for Hydrologic Advancement - MOCHA
- International glossary of hydrology.
- Virtual campus in hydrology and water resources
- Decision tree to choose an uncertainty method for hydrological and hydraulic modelling
- Catchment Modelling Toolkit
- CITY DRAIN - Open source software for integrated modelling in urban drainage (Platform: MAtlab/Simulink, citydrain.bplaced.net)
- Experimental Hydrology Wiki
National and international research bodies
- U.S. Geological Survey - Water Resources of the United States
- Centre for Ecology and Hydrology - UK
- eawag - aquatic research, ETH Zürich, Switzerland
- Institute of Hydrology, Albert-Ludwigs-University of Freiburg, Germany
- NOAA's National Weather Service - Office of Hydrologic Development, USA
- National Hydrology Research Center - Canada
- eWater - Australian Government’s Cooperative Research Centres programme
- Hydrologic Research Center - A Non-Profit Research Corporation, USA
- Economics of Water Resource Management from Improved Forecasting, NOAA Economics, USA
- University of Oklahoma- Natural Hazards and Disaster Center/USA
- UNESCO-IHE Institute for Water Education
- Centre for Water Science
National and international societies
- International Association of Hydrological Sciences (IAHS)
- British Hydrological Society
- Russian Geographical Society (Moscow Centre) - Hydrology Commission
- International Assoc for Environmental Hydrology
- American Water Resources Association
- Statistics in Hydrology Working Group
Basin- and catchment-wide overviews
- Connected Waters Initiative, University of New South Wales — Investigating and raising awareness of groundwater and water resource issues in Australia