Title: Watersheds%20and%20Hydrology
1Watersheds and Hydrology
- Whats 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
2Watersheds and HydrologyLearning 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?
3Question 1
4Global distribution of water
5Global distribution of freshwater
Water Storage Reservoir Percent () of total Percent () freshwater
Oceans 96.5 0
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 0.001 0.036
Biosphere 0.0001 0.003
6Watersheds 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?
7Question 2What is the hydrologic cycle?
- What is the hydrologic cycle?
Precipitation Interception Infiltration Evaporatio
n Transpiration Runoff Ground water
8Watersheds 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?
9Question 3
- How many dimensions does a stream have?
10Question 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)
11Longitudinal Changes in Streams
- Certain characteristics of streams change
predictably from upstream to downsteam - Channels become wider
- Channels become deeper
- Flow becomes slower, but greater in volume
12Longitudinal 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 (sediment) whereas the pool is a slower
flowing stretch with finer substrate
13Lateral 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
14Lateral Patterns
- Some streams and rivers will have a single
dominant channel while others have a network of
interwoven channels
15Lateral Features
- As rivers increase in size they will develop a
complex floodplain system
16Vertical dimensions
- Velocity changes with depth in stream channel
Diagram byEric G. Paterson Department of
Mechanical and Nuclear Engineering The
Pennsylvania State University
17Vertical Features
- Hyporheic (below stream) inter-actions
- Exchanges occur with groundwater just below the
stream
18Lateral 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
visible channel.
19Temporal dimension
- Stream flow changes
- Second by second
- Hourly
- Daily
- Monthly
- Seasonally
- Annually
- Millenniumly
- Channels migrate
- Riparian areas go through disturbance and
succession - Seasonal changes in inputs
20Watersheds 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?
21What are the major physical, chemical, and
biological components used to characterize water
quality?
22Selected Important Habitat Factors
- Light
- Substrate
- Temperature
- Oxygen levels
- Flow velocity
- Food availability
- pH
- Hydrologic, nutrient and sediment regimes
- Organic input and transport
- Toxics and other pollutants
- Biological communities
23 Influence of temperature on growth rates
1.0
Midges
Daily Growth Rate (mg/day)
0.5
Blackflies
Mayflies
0
0
8
16
24
32
Temperature C
Modified from Benke 1993
24Watersheds 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?
25What do we want to know about stream flow?
Question 5
- Magnitude - how much?
- Frequency - how often?
- Timing - when?
- Duration - how long?
- Rate of change how fast?
261982
27(No Transcript)
28(No Transcript)
29Mean daily flow (cfs)Juanita Creek Water Year
2010
Oct
May
30Mean Monthly FlowsJuanita Creek Water Years
2005-2009
31October flows Juanita Creek
32Oct 13 midnight
Oct 12 midnight
3315 minute flow (cfs) Juanita Creek Monday Oct
29-Wed Oct 31 2012
107
40
20
34November flows Juanita Creek
35Mean May DischargeJuanita Creek
36Hourly vs 15 Minute Measurements
37Mean Daily FlowJuanita Creek (cfs)
3815 minute flowsJuanita Creek May 27-29, 2004
May 28
39Daily vs hourly discharge (cfs)
40(No Transcript)
41Unregulated
Regulated
42Q
Discharge
43How 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
44Examples of where to locate national data for
watersheds and streams
- Watershed data
- EPA Surf your watershed http//www.epa.gov/surf/
- Climate data (national and international)
- http//www.ncdc.noaa.gov/oa/ncdc.html
- Climate data (Washington) http//www.wrcc.dri.edu/
summary/climsmwa.html
45Examples of where to locate national data for
watersheds and streams
- Stream data- quantity and quality
- USGS Water Resources Data http//water.usgs.gov/da
ta.html - Soils data
- http//soils.usda.gov/
- Aquatic biologic indicators
- http//www.epa.gov/bioindicators/
46Take 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 - Dont forget the basic processes involved