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Biogeochemical Cycles - 2
Class Lecture Goals Focus on the Water Cycle Unique aspects of water Understanding the behavior of water in streams (floods, power, salmon) Three case studies Chehalis River Flood Skagit Watershed: Loss of snow pack and glaciers Urban Watersheds
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Reading Science 2004
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The concern about loss of snow pack is because snow water makes up __% of stream water in the west
25 33 75 100
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Take-home messages Premise: Glaciers, permanent snow fields and snow pack are the ‘water towers’ of the mountains • Decreased snow packs • Biggest drops, lower elevations • Biggest drops, PNW • Snow is melting earlier in the spring • Disagreement: Mote vs. Taylor/Mass • Index year (1950) • Role of PDOs vs. climate change • Uncertainty • Shifts in timing of runoff • Impacts on summer water
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1913 Glacier National Park Austrian Alps 150 to 26 2005
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Water Cycle Properties of water Nature of stream flow (critical roles)
Three cases Chehalis River flood Skagit Watershed Urban watershed
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Quantities of Water Changes in Ice
If all glaciers & icecaps melted today the seas would rise about 230 feet (70 meters). During the last ice age, the sea level was about 400 feet (122 meters) lower than today. During the last warm spell, 125,000 years ago, the seas were about 18 feet (5.5 meters) higher than today.
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Unique Properties of Water
• Small molecule Three states: liquid, solid, gas Liquid from oC Takes lots of energy to change state or change temperature Transparent Solvent (C as skeleton of life, water as medium of life) Density of water (liquid vs. solid) O H - +
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Understand the behavior of a watershed
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Behavior of Water in a Watershed
Use of a hydrograph (stream gauge) Urban Agriculture Discharge Rain Forest-Ag Forest Time 12
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Behavior of Water in a Watershed
Westside, little or NO snow, Calawah, Forks Westside, lots of snow, Nooksack, Glacier
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Behavior of Water in a Watershed
Eastside, snow, NE WA Urban - suburban stream
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1. Chehalis River Flood 14 16 18
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Effects of trees vs. no trees
Assume 100” Amount & type of precipitation (ppt) - no difference. Trees intercept ppt (5 - 15%) Forest soil is drier: Trees transpire (20%) Snow stays colder under forest Snow accumulates more slowly under forest Roots provide strength Roads are bad
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2. Skagit Watershed Third largest on the west coast of US
3100 mile2 (about 1/6th in Canada) Major agriculture Major salmon National Park Seattle City Light
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Google Image of South Cascade River Watershed
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2005 South Cascade Glacier from ~1850 (see blue overlay) to 2005 (see above photo). 1928 2000
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South Cascade Glacier Data
Volume of South Cascade Glacier from ~1850 to Data for 1850 is an estimate. Glacier Volume (km3) Year 1928 2001 1890 2005 Take home lesson: snow pack is less, melting earlier, stored water in glaciers is being depleted
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3. Urban Watersheds - Thornton Creek
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Alternatives Storage system Green roofs Example from Sea-Streets
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Close-up a Sea-Street
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In your view, which alternative seems the most viable
Using cisterns (tanks) to collect runoff Requiring green roofs Using the S.E.A.-Street model
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Major (Climate) Change Issues
Premise: Clean, fresh water is a rare resource Quantity of water (+ in form of snow, ice) Seasonal and spatial distribution Rain on snow Loss of forests and vegetation Increases in impervious surfaces Demand for fresh water
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Summary: Water Cycle Water cycle: Quantity, Quality, Form, & Timing
Properties of water Watershed Climate, geographic location and water Three cases Chehalis Flood Skagit Watershed Urban Watersheds
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