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Recent trends in effective discharge in Northwest Washington R. Leif Embertson, MS, PE  River Restoration Northwest Conference February 1st , 2011
OBJECTIVE ,[object Object],Objective Definition Study Area Methods Results Next Steps Discussion
OBJECTIVE ,[object Object],Objective Definition Study Area Methods Results Next Steps Discussion
OBJECTIVE ,[object Object],Objective Definition Study Area Methods Results Next Steps Discussion 25-30% Increase
OBJECTIVE ,[object Object],Objective Definition Study Area Methods Results Next Steps Discussion
OBJECTIVE ,[object Object],Objective Definition Study Area Methods Results Next Steps Discussion
DEFINITION ,[object Object],Objective Definition Study Area Methods Results Next Steps Discussion
STUDY AREA ,[object Object]
NOOKSACK RIVER AT FERNDALE (LOWER WATERSHED)Objective Definition Study Area Methods Results Next Steps Discussion
STUDY AREA UPPER WATERSHED u LOWER WATERSHED ,[object Object],Objective Definition Study Area Methods Results Next Steps Discussion
METHODS ,[object Object]
Bin Size and Type
Arithmetic vs log
Sediment Transport (Observed or Equations)
If equations, Hydraulics R=aQb
Sensitivity analysisObjective Definition Study Area Methods Results Next Steps Discussion
RESULTS Objective Definition Study Area Methods Results Next Steps Discussion UPPER WATERSHED

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Effective Discharge Nooksack Watershed

Notes de l'éditeur

  1. Geomorphic paradigm; which events do the most work in shaping a channel and floodplain. Large infrequent events or smaller more frequent events