Freshwater and Society Module 1, part B
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s2 Watersheds
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s3 Hydrological cycle of a watershed
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s4 Watershed definition Watershed: An area of land that drains water, sediment and dissolved materials to a common receiving body or outlet The term is not restricted to surface water runoff and includes interactions with subsurface water Watersheds vary from the largest river basins to just acres or less in size
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s5 Organization of watersheds: A divide represents the boundary of a watershed Larger watersheds can often be divided into smaller units called subbasins, drainage areas, or water resource inventory areas xecmgmt/lyout2.htm
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s6 Watersheds
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s7 Watershed components Latitude, albedo & climate Geology Topography Land Use: Vegetation and impervious surfaces
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s8 Watershed components: Latitude Energy input into a watershed depends on solar height and length of daylight hours Determined by the latitude and season May 21, Seattle, WA solar altitude at noon is January 21, Seattle solar altitude at noon is
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s9 Watershed components: Albedo Albedo is the reflectance of a surface. The higher the reflectance the less energy input into a watershed. Surface CoverAlbedo (%) Water5-10 Bare soil (light colored, dry)20-35 Marsh and Bogs15-20 Forest (dense spruce)5-10 Forest (hardwoods in leaf)15-20 Snow (fresh)80-95 Snow (old)40-70
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s10 Temperature regime Relative humidity Precipitation patterns Watershed components: Climate
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s11 Watershed components: Climate Precipitation Temperature Relative humidity (RH) Wind
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s12 Watersheds: Average annual precipitation
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s13 Watersheds: Potential evapotranspiration
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s14 Watersheds: Water surplus or deficit
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s15 Bedrock Type and distribution of soils Watershed components: Geology doc/s2chap5.htm
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s16 The ease with which water penetrate or pass through a bulk mass of soil or a layer of soil Geology: Soil permeability Domino/vro/vroimages.nsf/Images/g loss-ferr/
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s17 Total porosity of a soil determines maximum water content at saturation; soils within zone of aeration are seldom saturated. Textural (primary) porosity: voids between aggregates. Structural (secondary) porosity: voids within aggregates – fracture or poor zones Geology: soil pore space and water content 168/Pp-limestone.jpg
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s18 Geology: Groundwater vs. soil moisture Groundwater: Subsurface water in the zone of saturation that is free to move under the influence of gravity, often horizontally to stream channels Soil Moisture: Subsurface water in the unsaturated zone held in place by capillary forces or osmotic pressure
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s19 Geology: moisture content of various soils
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s20 Infiltration is the flow of water downward through the upper layers of soil Geology: Infiltration
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s21 Geology: infiltration capacity during a storm
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s22 Geology: soil moisture profile after a rain event 1)Before Storm 2)End of Storm 3)One day after 4)Two days after 5)Three days after Adopted from: vro/vroimages.nsf/Ima ges/gloss-ferr/
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s23 Geology: seasonal infiltration trends
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s24 Geology: seasonal variation in watershed runoff
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s25 Geology: Saturation and runoff generation
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s26 Topography Slope Aspect Watershed components: Topography
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s27 Watershed components: Topographic interactions
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s28 Watershed components: Land use and vegetation Vegetation Slows runoff Reduces soil compaction Prevents soil erosion Reduces pace of raindrop splash Reduce soil material moving downslope Influences timing of snowmelt runoff Influences water yield
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s29 Land use: Stormwater discharge vs. land use
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s30 Land uses: Effects upon hydrology/water quality Natural Events Fires Wind storms Disease outbreaks Floods Volcanoes Climate change Land Uses Flood control Timber production Urban development Hydroelectric Agriculture Mining Water quality Watershed hydrology
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s31 Watershed components: land Use
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s32 Organization of a watershed
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s33 Water budget Evaluation of sources of supply vs. discharges with respect to a drainage basin Watershed: Water budgets Potlatch, Idaho Spearfish, South Dakota
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s34 Annual water budget for Lawrence Lake, Michigan, and Mirror Lake, New Hampshire Watershed: Water budgets
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s35 Watershed: Water budgets Water budgets provide a graphic depiction of the distribution of moisture throughout the year in any given area An idealized budget, however, is rarely achieved Examples from Los Angles, CA and Pullman, WA, illustrate the range of potential deviation from the “ideal” water budget Fig. 8.4
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s36 Watershed water budget: Pacific Northwest
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s37 Watershed: Aquatic ecoregions North America has been divided into eight major aquatic ecoregions: Arctic rivers and lakes Large temperate lakes Temperate headwaters and lakes Large temperate rivers Endorheic rivers, lakes, and springs Xeric-region rivers, lakes, and springs Temperate coastal rivers and lakes Subtropical coastal rivers and lakes
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s38 Aquatic Ecoregions of North America
Developed by: Munson, Richards, Svendsen Updated: Dec. 30, 2003 U1-m1b-s39 Geomorphology Climate Land uses Vegetation Watershed hydrology Albedo Watershed components