Sensitivity and Stability of Iowa Daily Erosion Project 2 to Variable Landscape and Rainfall Intensity Soil and Water Conservation Society Annual Meeting July 27, 2015 Brian Gelder R.M. Cruse, K. Gesch, D. James, D. Herzmann, T. Sklenar, J. Opsomer, J. Laflen, D. Flanagan
25
Embed
Sensitivity and Stability of Iowa Daily Erosion Project 2
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Sensitivity and Stability of Iowa Daily Erosion Project 2 to Variable Landscape and Rainfall
Intensity
Soil and Water Conservation Society Annual MeetingJuly 27, 2015Brian Gelder
R.M. Cruse, K. Gesch, D. James, D. Herzmann, T. Sklenar, J. Opsomer, J. Laflen, D. Flanagan
What Is the Iowa Daily Erosion Project?
• Estimates daily sheet and rill hill slope erosion spatially across Iowa;
• Gen 1 Debut 2002;• WEPP model is the ‘engine.’
IDEP Gen 1• Cox, C.; Hug, A.; Bruzelius, N. Losing Ground; Environmental
Harvest Public Media. April 12, 2011. http://harvestpublicmedia.org/article/519/soil-erosion-threatens-iowa-agriculture/5
• High prices sow seeds of erosion. William Neuman. New York Times. April 12, 2011
• Cruse, R.M., D. Flanagan, J. Frankenberger, B. Gelder, D. Herzmann, D. James, W. Krajewski, M. Kraszewski, J. Laflen, J. Opsomer, and D. Todey 2006. Daily estimates of rainfall, water runoff, and soil erosion in Iowa. J. Soil Water Conserv. 61:191-198. – Best Research Paper Award for Impact and Quality (Honorable Mention)
Major Geo-Spatial Components by HUC12• Soils - gSSURGO – 10m raster• Land Use - 2008-2013 NASS Crop Data Layer • Elevation - LiDAR-based, 3m resolution• 2009 crop-specific field boundaries
IDEP 2 Hillslope Profiles
• WEPP OFEs break at Land-use and Soils boundaries• Slope estimated for each OFE from DEM
OFE 2
OFE 3
OFE 1
OFE 4
15
HUC 12 Boundary
Stratified sampling units – subcatchments
SubcatchmentBoundary
13
CatchmentBoundary
Flowpath
Research Question: Is one flow path per subcatchment a sufficient sampling density to give a representative
HUC 12 average? CatchmentBoundary
Flowpath
Procedure
• Select 3 HUC12 watersheds per MLRA (10)• In 30 HUC12s, generate up to10 flowpaths per
sub-catchment• Run DEP using 1 through 10 flowpaths
Select HUC12s
Results
Results
Does IDEP Give Representative Soil Erosion Estimates?
• Compare to NRI– RUSLE technology– Long term average rainfall product– Linear hill slopes– Periodic site visits to determine management– Statewide average sheet and rill detachment &
• Average IDEP annual erosion = 5.71 tons/acre• 2007 and 2010 NRI = 5.25 and 5.42 ton/acre• Conclusions:– Over multiple years IDEP agrees with NRI– IDEP better captures annual & spatial variability
Conclusions
• IDEP long-term statewide averages agree with NRI (statewide average) suggesting estimates are realistic and inputs data are defendable.
• Increasing number of flowpaths modeled per sub-catchment has little impact on estimates across a representative sample of HUC 12s suggesting one flow path per subcatchment is suitable.