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@COBrogan - outline for today's meeting with Gopal
- Methodology: Analyze gages in terms of HSPF paradigm ie
Q = f(AGWS, AGWRC)- Also, in HSPF docs we see:
$AGWO_{t} = f(AGWO_{t-1}) = AGWRC * AGWO_{t-1}$
- Also, in HSPF docs we see:
- Is there hydraulic head varying baseflow/AGWRC?
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AGWRC = f(AGWS)in gage flow we can analyzeAGWRC = f(Q) - Evidence (Strasburg yes, Coote's maybe not)
- 2002 case study
- 2023 case study
- Approaches to modeling (special action, Cheri's augmentation)
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- Further validation of method (from meeting with Gopal):
- Step 1: Analyze runoff from a single landseg/landuse
- Step 2: Resegment model for Passage or Smith Creek (or Linville?) to find watershed with only 1 land segment overlapping. (note: may need to up the sophistication of our resegmentation routines to subdivide only a single land segment from the parent)
- Step 3: Compare to larger watershed.
- Step 4: Compare results to other "standard" baseflow separation techniques. Does our routine improve?
- Analysis of model baseflow inputs
- Phase 7 runoff
- Is the land hydro simulation streamlined in terms of number of LUs?
- This could help, as reduces complexity for outputting baseflow into river segments (not currently)
- Same WDM framework? Other?
- Basically, this is ideal time for us to start running this
- Draft modification to phase 5/6 WDM structure that separated local runoff inflow and upstream flow into DSN 10 & 11 (it worked sorta, for some reason my approach which just used the DSN basics double baseflow inputs to the model and I abandoned it). Add Local runoff inflows after ETM step meta_model#9
- Gopal has replaced ETM I think?
- Phase 7 runoff
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