Daily Analysis

PRE-ANALYSIS PROCEDURE (per-gauge facts for 2026-05-21):


1. PRECIPITATION SUMMARY

Zero QPE basin-wide. All 37 HUC12s record 0.000" 24-hr total. Second consecutive dry day. The forcing for today's activity is entirely Event 11 (Day 80) precipitation — Pruitt zone 1.93", St. Joe 1.60", Harriet 1.76", ungauged 2.21".

2. GAUGE RESPONSES

Today is a recession + propagation day. Five gauges in pure recession, two completed Event 11 peaks within the day:

3. RAINFALL-RESPONSE PAIRS (Event 11 FINAL closure)

With today's peaks closing out Event 11 at St. Joe and Harriet, full Event 11 transfer ratios are now finalized:

Gauge Peak (final) Total rise Lag (peak QPE → peak gauge) Transfer ratio Prior comparison
St. Joe 5.22 ft / 949 cfs @ D82 02:00 +1.74 ft / +751 cfs from 3.48 ft pre ~37 hr from peak QPE (Day 80 ~10 CDT) 1.09 ft/in (1.74/1.60) Event 8 (wet) ~1.5–2.0 ft/in; Event 10 (moist) ~1.3 ft/in. Dry-antecedent value lower as expected — within 30% of prior dry-event scaling.
Harriet 5.00 ft / 1130 cfs @ D82 13:15 +1.33 ft / +898 cfs from 3.67 ft pre ~51 hr from peak QPE 0.76 ft/in (1.33/1.76) Event 8 ~1.0–1.2 ft/in (wet). Dry-antecedent Harriet transfer 0.76 ft/in is ~25–35% lower than wet — consistent with dry-soil dampening. Within expected deviation.

Antecedent (Event 11, 7-day at Day 80): Pruitt 0.07", St. Joe 0.25", Harriet 0.22" — DRY-DRY match across all gauges. This event is the cleanest dry-antecedent calibration for the lower mainstem in the study.

Propagation lag refinement: Harriet peak lagged St. Joe peak by ~11.25 hr (02:00 → 13:15). Earlier I noted Harriet "≥35 hr" lag from QPE; final value ~51 hr from peak QPE (Day 80 14:02 UTC = 09:02 CDT → D82 13:15 CDT = ~52 hr). This is the longest peak-to-peak lag observed in the study and reflects the dry-soil + large drainage (2,775 km²) combination.

Bear Creek anomaly persists: 2.06 → 2.16 ft over Days 80–82 = +0.10 ft / 1.11" = 0.09 ft/in. Far below mainstem ratios. Confirms Bear Cr dry-antecedent dampening pattern from prior hypothesis (~0.07 ft/in). No revision needed; consistent within 30%.

4. DOWNSTREAM PROPAGATION

Final Event 11 mainstem cascade (peak-to-peak): - Boxley D81 01:30 → Pruitt D81 08:45 (Δ +7.25 hr) - Pruitt D81 08:45 → St. Joe D82 02:00 (Δ +17.25 hr) - St. Joe D82 02:00 → Harriet D82 13:15 (Δ +11.25 hr) - Total Boxley → Harriet: ~36 hr for dry-antecedent Event 11.

Compare to Event 8 (wet, multi-pulse): comparable Boxley→Harriet was ~24–28 hr. The ~30% longer dry-event propagation reflects pool-filling, slower wave celerity in dry channels, and reduced lateral inflow.

5. MULTI-DAY EVENTS

Event 11 is now substantially complete with the following final totals: - Duration of gauge response: ~60 hours (D80 morning → D82 evening, with Bear Cr still slowly rising). - Spatial: watershed-wide. - Recreational implications (height-based, more reliable than CFS per local knowledge): - Pruitt peaked at 4.60 ft — well into the Hailstone-equivalent boatable range, but Pruitt has no published thresholds; CFS peak 354 was in "Optimal" (200–2000). - St. Joe peak 949 cfs, Harriet peak 1130 cfs: both squarely in "Optimal" (200–8000 / 200–9370). No flood risk. - Richland peak 2.20 ft: below "Low but Floatable" threshold (3.2 ft). Did not produce a runnable upper Richland window — confirms local-knowledge expectation that dry-antecedent events rarely push Richland to boatable.

6. ANOMALIES OR SURPRISES