Surface water hydrology explores the movement and distribution of water above ground. It examines rivers, lakes, and wetlands, focusing on processes like precipitation, runoff, and stream flow. Understanding these systems is crucial for managing water resources and mitigating flood risks.
This field investigates how surface water interacts with the broader hydrologic cycle. It covers topics such as watershed management, water quality, and flood frequency analysis. These concepts are essential for addressing real-world challenges in water resource management and environmental protection.
Hydrology studies the movement, distribution, and management of water resources on Earth
Watershed refers to an area of land that drains water to a common outlet point (river, lake, ocean)
Hydrologic cycle describes the continuous movement of water through evaporation, condensation, precipitation, and runoff
Driven by solar energy and gravity
Surface water includes water found in rivers, lakes, wetlands, and oceans
Accounts for a small percentage of Earth's total water supply
Groundwater is water stored beneath the Earth's surface in soil pores and rock fractures
Infiltration process by which water on the ground surface enters the soil
Evapotranspiration combination of evaporation from land and water surfaces and transpiration from plants
Runoff portion of precipitation that flows over land surfaces towards streams, rivers, or other water bodies
The Hydrologic Cycle
Continuous movement of water on, above, and below the surface of the Earth
Driven by solar energy, which causes evaporation and transpiration
Evaporated water condenses in the atmosphere to form clouds
Precipitation occurs when water vapor condenses and falls back to Earth as rain, snow, or hail
Infiltration allows water to enter the soil and recharge groundwater aquifers
Surface runoff flows over land towards streams, rivers, and other water bodies
Influenced by factors such as land use, soil type, and topography
Groundwater flow moves through soil pores and rock fractures, eventually discharging into surface water or the ocean
Human activities (water withdrawals, land use changes) can impact the hydrologic cycle
Surface Water Components
Rivers and streams primary conduits for surface water flow
Fed by precipitation, snowmelt, and groundwater discharge
Lakes and reservoirs natural or man-made water bodies that store surface water
Provide water supply, flood control, and recreational opportunities
Wetlands areas where water covers the soil or is present near the surface for a significant portion of the year
Play crucial roles in water purification, flood attenuation, and habitat provision
Oceans largest component of the Earth's surface water, covering approximately 71% of the planet
Glaciers and ice caps store a significant amount of freshwater in solid form
Melting of these ice masses contributes to sea level rise and changes in surface water dynamics
Estuaries transitional zones where rivers meet the ocean, characterized by a mix of fresh and saltwater
Floodplains low-lying areas adjacent to rivers that are subject to periodic inundation during high flow events
Precipitation and Runoff Processes
Precipitation primary input of water to the Earth's surface
Can occur as rain, snow, hail, or sleet
Interception process by which precipitation is caught and stored by vegetation or other surfaces before reaching the ground
Infiltration movement of water from the surface into the soil
Influenced by soil properties, land cover, and antecedent moisture conditions
Surface runoff flow of water over the land surface towards streams or other water bodies
Occurs when precipitation exceeds the rate of infiltration
Baseflow sustained flow in a stream or river derived from groundwater discharge
Overland flow movement of water over the land surface as a thin, continuous film
Channel flow movement of water within a defined stream channel
Influenced by channel geometry, roughness, and gradient
Hydrograph graphical representation of stream discharge over time, showing the response of a watershed to a precipitation event
Stream Flow Measurement and Analysis
Stream gauging measurement of water level (stage) and velocity to determine discharge
Discharge volume of water passing a specific point per unit time, typically expressed in cubic meters per second (m³/s)
Rating curve relationship between water level (stage) and discharge for a specific stream cross-section
Used to estimate discharge based on measured water levels
Hydrograph analysis study of the shape, timing, and magnitude of stream flow response to precipitation events
Rising limb steep increase in discharge following the onset of a precipitation event
Peak flow maximum discharge during a hydrograph
Recession limb gradual decrease in discharge following the peak flow
Baseflow separation techniques used to estimate the contribution of groundwater to stream flow
Flood routing methods used to predict the timing and magnitude of flood waves as they move downstream
Flow duration curve graphical representation of the percentage of time that specific discharge values are equaled or exceeded
Useful for characterizing the flow regime of a stream and assessing water resource availability
Flood Frequency and Risk Assessment
Flood frequency analysis statistical assessment of the likelihood of a flood event of a given magnitude occurring
Typically expressed as a return period (e.g., 100-year flood)
Probability of exceedance likelihood that a flood of a given magnitude will be equaled or exceeded in any given year
Annual exceedance probability (AEP) probability that a flood of a given magnitude will be equaled or exceeded in a given year
Inverse of the return period (e.g., 100-year flood has an AEP of 1%)
Flood risk assessment evaluation of the potential consequences of flooding, considering factors such as population, infrastructure, and economic activity
Flood hazard maps delineate areas at risk of flooding based on historical data and hydrologic modeling
Used for land use planning, insurance, and emergency management
Flood mitigation strategies measures taken to reduce the impact of flooding (levees, floodwalls, detention basins)
Non-structural measures policies and practices that reduce flood risk without physical infrastructure (building codes, land use regulations, early warning systems)
Water Quality in Surface Systems
Physical parameters characteristics of water that can be observed or measured (temperature, turbidity, dissolved oxygen)
Temperature influences chemical and biological processes in water bodies
Turbidity measure of water clarity, influenced by suspended sediment and organic matter
Chemical parameters concentrations of various substances in water (nutrients, metals, pesticides)
Nutrients (nitrogen and phosphorus) can lead to eutrophication and algal blooms when in excess
Metals (lead, mercury) can be toxic to aquatic life and human health
Biological parameters indicators of the health of aquatic ecosystems (bacteria, algae, macroinvertebrates)
Fecal coliform bacteria indicate the presence of human or animal waste and potential pathogens
Benthic macroinvertebrates sensitive to water quality changes and used as bioindicators
Point source pollution pollution originating from a single, identifiable source (wastewater treatment plants, industrial discharges)
Non-point source pollution pollution originating from diffuse sources over a wide area (agricultural runoff, urban stormwater)
Total Maximum Daily Load (TMDL) regulatory framework for identifying and restoring impaired water bodies by setting pollutant load limits
Best Management Practices (BMPs) strategies and techniques used to minimize water quality impacts from land use activities (buffer strips, retention ponds)
Practical Applications and Case Studies
Watershed management integrated approach to managing water resources within a watershed context
Involves stakeholder collaboration, land use planning, and water quality monitoring
Stormwater management strategies for managing runoff from urban areas to reduce flooding and water quality impacts
Green infrastructure (permeable pavement, rain gardens) mimics natural hydrologic processes
Flood forecasting and warning systems use hydrologic models and real-time data to predict and communicate flood risks
Early warning allows for evacuation and emergency response
Reservoir operations management of water levels and releases from dams to balance competing objectives (water supply, flood control, hydropower)
Instream flow requirements minimum water flows needed to maintain the ecological health of rivers and streams
Often established through legal or regulatory frameworks
Wetland restoration and construction projects that aim to restore or create wetland habitats for water quality, flood attenuation, and biodiversity benefits
Agricultural water management practices and technologies used to optimize irrigation efficiency and reduce water quality impacts from agricultural runoff (precision irrigation, cover crops)
Urban stream restoration projects that aim to restore the hydrologic and ecological function of degraded urban streams (channel reconfiguration, riparian buffers)