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Watersheds and Hydrology
What’s Water Got to Do with It? More water moves through ecosystems than any other material The materials that it carries and deposits and the energy that it expends are major drivers in shaping the contour of the land and the habitat availability/suitability for organisms. A resource that humans cannot live without Slide discussing water and ecosystems
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Watersheds and Hydrology Learning Objectives
Where do we find water? What is the hydrologic cycle? How many dimensions does a stream have? 4 How do we characterize stream water? 5 What do we want to know about stream flow?
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Where do we find water? Question 1
Slide listing objectives for session 9, river as habitat
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Global distribution of water
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Global distribution of freshwater
Water Storage Reservoir Percent (%) of total Percent freshwater Oceans 96.5 Ice and Permanent Snow 1.74 68.7 Groundwater 1.7 30.1 Lakes 0.013 0.91 Soil Moisture including permafrost 0.023 0.26 Atmosphere 0.001 0.04 Streams, Rivers, Swamps 0.036 Biosphere 0.0001 0.003 Igor Shikomanov “world fresh water resources in Gleick 1993 Water Crisis (Oxford Press)
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Watersheds and Hydrology
Where do we find water? What is the hydrologic cycle? How many dimensions does a stream have? 4 How do we characterize stream water? 5 What do we want to know about stream flow?
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Question 2 What is the hydrologic cycle?
Precipitation Interception Infiltration Evaporation Transpiration Runoff Ground water
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Watersheds and Hydrology
Where do we find water? What is the hydrologic cycle? How many dimensions does a stream have? 4 How do we characterize stream water? 5 What do we want to know about stream flow?
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How many dimensions does a stream have?
Question 3 How many dimensions does a stream have?
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Question 3 How many dimensions does a stream have?
Longitudinal (upstream to downstream) Lateral (bank to bank and valley wall to valley wall) Vertical (water surface to bed to hyporheic to ground water) Temporal (time: seconds to millennia)
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Longitudinal Changes in Streams
Certain characteristics of streams change ‘predictably’ from upstream to downsteam Channels become wider Flow becomes slower, but greater in volume Streams become deeper
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Longitudinal Changes – Reach Scale
Longitudinal changes are also observed at shorter scales than the entire river length We call this shorter scale the “reach” scale One example of reach scale changes is the pool-riffle pattern found in many streams draining areas with medium gradients Riffle is an area of rapid flow over coarse substrate (rocks) whereas the pool is a slower flowing stretch with finer substrate
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Lateral Patterns There are also some predictable changes laterally
The stream has its low flow channel, the low point of which is the thalweg The stream has banks which define its frequent flow limit The stream has a floodplain which defines its flow limit on less frequent events, annual or lesser frequency Thalweg
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Lateral Patterns Some streams and rivers will have a single dominant channel while others will have a network of interwoven channels
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Lateral Features As rivers increase in size they will develop a complex floodplain system
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Vertical dimensions Velocity changes with depth in stream channel
Diagram by:Eric G. Paterson Department of Mechanical and Nuclear Engineering The Pennsylvania State University
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Vertical Features Hyporheic (below stream) inter-actions
Exchanges occur with groundwater just below the stream
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Lateral and Vertical Patterns
In many large alluvial valleys, creatures that live in ground water and hyporheic water can be found in the subsurface water kilometers from the stream. In other words the stream extends well beyond its channel.
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Temporal dimension Stream flow changes Second by second Hourly Daily
Monthly Seasonally Annually Millenniumly
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Watersheds and Hydrology
Where do we find water? What is the hydrologic cycle? How many dimensions does a stream have? 4 How do we characterize stream water? 5 What do we want to know about stream flow?
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What are the major physical, chemical,
Question 4 What are the major physical, chemical, and biological components used to characterize water quality? Slide outlines the objectives for session 10
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Selected Important Habitat Factors
Light Substrate Temperature Oxygen levels Flow velocity Food availability pH Nutrient and sediment regimes Organic input and transport Toxics and other pollutants Biological communities
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Influence of temperature on growth rates
1.0 Midges Daily Growth Rate (mg/mg/day) 0.5 Blackflies Daily growth rates as a function of temperature for three aquatic insects in Georgia. Modified from Benke 1993. Mayflies 8 16 24 32 Temperature C Modified from Benke 1993
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Watersheds and Hydrology
Where do we find water? What is the hydrologic cycle? How many dimensions does a stream have? 4 How do we characterize stream water? 5 What do we want to know about stream flow?
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What do we want to know about stream flow?
Question 5 What do we want to know about stream flow? Magnitude - how much? Frequency - how often? Timing when? Duration how long? Rate of change – how fast? Slide of ways to characterize flow, emphasis on magnitude.
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Mean Monthly Flows Juanita Creek Water Years 2005-2009
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Mean daily flow (cfs) Juanita Creek Water Year 2010
Oct May
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Mean May Discharge Juanita Creek
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Hourly vs 15 Minute Measurements
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Mean Daily Flow Juanita Creek (cfs)
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15 minute flows Juanita Creek May 27-29, 2004
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Unregulated Regulated
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How much water is enough?
Depends on who or what is using the water Historically managed for minimum flows (what is the minimum flow that keeps fish alive) Legal issue of water rights complicates situation
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Stream flow functions Medium where aquatic organisms live and propagate Needs vary by species and life stage Focusing flow requirements on single species can result in unintended harm to other species Plays a role in stream temperature and oxygen levels
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Stream flow functions 2. Provides the forces that create and maintain in-channel and off-channel habitat, riparian patch communities, etc. New channel formation Wood recruitment and distribution Sediment recruitment and transport Removal of fines
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Stream flow functions 3. Rejuvenates floodplain soils and vegetation and recharge groundwater Maintain connectivity with hyporheic zones Redistribute soil and nutrients to floodplain forest Distribute seeds and prepare seed beds
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Examples of where to locate national data for watersheds and streams
Watershed data EPA Surf your watershed Climate data (national and international) Climate data (Washington)
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Examples of where to locate national data for watersheds and streams
Stream data- quantity and quality USGS Water Resources Data Soils data Aquatic biologic indicators
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Take – home messages Flow regimes play a major role in habitat
Land-use alters flow paths and storage components and hence, flow regimes Effects vary with spatial and temporal scales Research on which aspects of flow are most critical to various biotic responses are in progress Don’t forget the basic processes involved Summary slide of land use change and ecological effects.
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