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This presentation, prepared by Dr. Donald R. Reichmuth, explores the dynamic interactions between stream systems and meteorological frameworks that affect floodplain management. Learn about temperature and pressure gradients, water sources, river basin definitions, and significant weather-affecting factors through various data analyses. The session also examines the hydrologic cycle, precipitation dynamics, and runoff behaviors that contribute to understanding flood risks and weather patterns across North America, specifically focusing on the mid-continental region.
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Floodplain ManagementSESSION 4 Stream Systems on Dynamic Earth Hydrosphere Prepared By Donald R. Reichmuth, PhD.
Meteorological Framework Objectives: • Show Temperature & Pressure Gradients • Show Water Sources • Define A River Basin • Explain Published Resource Data • Illustrate Factors Affecting Weather • Discuss Metrological processes within the context case study floodplains.
North American Temperature Data Mid-Continent: (North Central US & Canadian Plains) Normally has cold winters and hot summers that causes Mid-Continent Winter High Pressure & Summer Low Pressure
WinterTemperature Data Typical Winter Pattern: Coldest in Northern Mid-Continent 2004 Departure: From Mean
North American Air Flow Monsoon Pattern: Monsoon Defined: A wind system that reverses direction between summer and winter.
Earth’s Water Sources: Outer Space Volcanoes Rock Disintegration Total Volume: 309,000 Units One Unit (1) = 4475 Cubic Km (1070 Cubic Miles) 100 Units = Yearly Evaporation From Oceans 300,000 Units = Present Volume All Oceans
Hydrologic Cycle Evaporation From Oceans Wind Moves Moisture Laden Clouds Moisture Condenses & Falls Precipitation Falls Back Into Oceans Produces Stream Flow On Land Enters Groundwater On Land Water Returns To Oceans
Runoff Defined Runoff (Two Forms): Surface Stream Flow Controlled by Surface Topography Groundwater Flow Controlled by Subsurface Structure
Catchment Defined The surface catchment area is that area of a River Basin upstream from a given point on a stream where “surface runoff” is determined. The groundwater catchment area is all areas that contribute recharge water to the subsurface aquifer.
Basin Topographic Map Grand River • NOTE: Subbasins Marked
Moisture Forecasthttp://www.cpc.ncp.noaa.gov/ptoducts/analysis/monitoring/cdus/palmer_drought_outlook.gif
Hazards Assessment Briefinghttp://www.cpc.ncep.noaa.gov/products/predictions/threats
Precipitation Data National Resources Conservation Service (NRCS) National Water & Climate Center www.wcc.nrcs.usda.gov/ Snow Survey & Water Supply www.nrcs.gov/programs/snowsurvey/ Western Regional Climate Center (WRCC) wrcc@dri.edu
NRCS Snow Water Contenthttp://www.mt.nrcs.usda.gov/snow/data.current.htm
Flood Warning Example April 11, 2004 Red River, ND
Palmer Drought Severity Index • A “Meteorological” Drought Index • Widely Used In The USA • Measures Abnormality • Range +6 ---- Extremely Wet 0 ------ Near Normal -6 ----- Extremely Dry
Dendrochronology Example: Determining Past Climate Conditions
Drought Information Center(NOAA)http://www.drought.noaa.gov/index.html Home Page Menu Lists Links To Numerous Products Precipitation Soil Moisture Drought Fire Potential Temperature
Drought Predictionhttp://www.ncep.noaa.gov/products/expert_assessment/season_drought.gif
Local Microclimates Orographic Precipitation Caused by Anabatic (Blowing Up Slope) Wind Rain Shadows Caused by Katabatic (Blowing Down Slope) Wind Lake Effects Caused by Wind Blowing Over Water Heat Islands Caused by Urban Heat Sources Acid Rain Caused by SO4 Emissions
Average Runoff Patterns Low ----- Western Plains & Southwest High ----- New England, Appalachians, Gulf Coast & Pacific Northwest
Slide PresentationPrepared ByGeomax, P.C.Dr. Donald R. Reichmuth, President1023 W. 30th Ave.Spokane, WA 99203-1324Phone & FAX – 509-838-6390E-mail – geomax@comcast.net