Watershed concepts for community environmental planning

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Purpose and Objectives Watershed concepts for community environmental planning Dale Bruns, Wilkes University USDA Rural GIS Consortium May 2007 Provide background on basic concepts in watershed, stream, and river ecology Unifying theme streams are connected to their watersheds and Land use is a major impact on watersheds and stream and river ecology Review hydrologic cycle relative to land use impacts on Flooding Stream channel impacts Illustrate examples of land use impacts to streams Introduce GIS and geospatial data of watershed management Weather and Climate are drivers Hydrologic cycle Three major factors slopes, soils, land use (land cover) Illustrate examples of GIS data applied to Toby Creek Traditional watershed delineation had been done manually using contours on a topographic map. Upper Susquehanna- Lackawanna Watershed s Relationship to the Chesapeake Bay Ecosystem Outlet Point A watershed boundary can be sketched by starting at the outlet point and following the height of land defining the drainage divides using the contours on a map. Pennsylvania Chesapeake Bay Local watershed groups usually focus on smaller watersheds at the community level Lackawanna River Corridor Association Friends of Nescopeck Cr. The Hydrologic Cycle encompasses numerous processes that define all watersheds and form the basis for management 1

Suspended load (silt and sand) is carried in the water column Bedload (coarse sand and fine gravel) bounces along the stream bottom or channel Stream connection to the terrestrial environment: floodplain Extent of floodplain Stream bank Channel width Floodplain canyon wall to canyon wall 2

Note the forest community within the canyon area which constitutes the riparian zone Floodplain: canyon wall to canyon wall Dry, stream channel etched in the canyon floor of bedrock by torrential runoff during desert storms; note pool and riffle structure with meanders (scale: channel about 1 ft wide). Example from the Rocky Mountains Example from arid shrubsteppe ecoregion Riparian forest debris helps stabilize channels and provide aquatic habitat Figure from Miller (1990); Wadsworth Publishing Company. Cited in the FISRWG (1998). Zone 1 - Headwaters - Coarse sediments - Steep slopes Zone 3 Depositional - Fine sediments - flat terrain; sinuous 3

S d Q Headwater Streams to Rivers Bed material particle (grain) size (d) decreases downstream slope (S) also decreases Discharge (Q) increases downstream Channel width and depth increase also Four stream and river sizes along the continuum Principle Effects of Land Cover on Watershed Response Precipitation Evapotranspiration Land cover Infiltration Groundwater Interception Runoff Volume Peak Flow Sediment Yield Water Quality Ecological impacts from land use and land use change Unifying watershed concept: Streams and rivers are strongly connected to their terrestrial watersheds Characteristics and factors? Practical examples illustrated Stream channel morphology ( - Salmon R., Idaho) Stream water quality and turbidity ( - Salmon R., Idaho) Channel erosion flash flooding (Aravaipa Cr., Arizona) Urban waste and raw sewage in urban stream channel (China Biosphere Reserve and native culture and land use (China) Biosphere Reserve - glacial runoff and water quality (Rio Paine, Chile) Acid Mine Drainage in Solomon s Creek (PA) 4

Pristine Rocky Mountain stream? This is the real, natural stream channel and not the previous slide. Overgrazing by livestock on a local scale can impact stream habitat, food webs, and fish populations through changes in channel morphology A C D B Sawtooth and Salmon River Wilderness, ID Nearby Mining Activities Salmon River Impacted Water Quality Plume (of suspended sediment) 5

Best Management Practices (BMP): Sediment Retention Basins Fanjingshan Biosphere Reserve Industrial City: Airshed and urban stream Intensive land use is the typical situation in China with high human population densities GPS for locating (inset) sampling sites: Fan Jing Shan Biosphere Reserve, China Fanjingshan Biosphere Reserve: native agriculture 6

Bio-monitoring at sampling sites: Fan Jing Shan Biosphere Reserve, China High peak in the center of the Biosphere Reserve High peak area: Fan Jing Shan Biosphere Reserve, China 500 year old Buddhist sanctuary on the high peak Southern terminus of Patagonian glacial field Glacial till in Rio Paine Torres del Paine Biosphere Reserve, Chile; Global Monitoring Satellite Image for Field Reconnaissance Torres del Paine Biosphere Reserve, Chile False color Landsat satellite image Dark reds are beech forests Light reds are shrublands Glaciers in white 7

Torres del Paine Biosphere Reserve, Chile Southern terminus of Patagonian glacial field GPS for locating sampling sites: Torres del Paine Biosphere Reserve, Chile Glacial till in Rio Paine PA GIS Consortium Environmental Field Work: GPS locations of water quality problems PA GIS Consortium Photo: Mining Operation PA GIS Consortium Severely degraded stream with urban debris and mining sediments Persistent Water Quality Problems Focus area Tobys Creek DRIVER of Hydrologic Cycle Climate and Weather FACTORS for stream dynamics Slopes Soils Land Use and Land Cover Mapping mine outfall locations with GPS technologies 8

Rainfall type II for PA 2-yr, 24-hr rainfall event for Toby Creek, PA Most models can create the watershed extents based on flow characteristics derived from DIGITAL ELEVATION MODELS (DEM) TO REPESENT SLOPES FACTOR 1: SLOPES FACTOR 2: SOILS USDA NRCS STATSGO Soil classes only Usually adequate for modeling Used in modeling to calculate a curve #» The Curve Number (CN) is used to predict the runoff properties for a particular soil and ground cover. FACTOR 3: Land Use - Land Cover NLCD 2001 MRLC - NLCD (National Land Cover Dataset) Circa; 1992 Classified satellite imagery Modified Anderson level 2 classification Formal accuracy assessment 9

PA GIS Consortium www.pagis.org www.ruralgis.org 10