Streamflow

Above normal

Rio Grande at Otowi Bridge streamflow

Daily mean discharge, Rio Grande basin, New Mexico

Data through Sep 30, 2026 · source last checked Oct 1, 2026 · page revised Oct 1, 2026

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About this data
Source
US Geological Survey (USGS)
Series
Daily mean streamflow (discharge)
Geography
Rio Grande at Otowi Bridge
Unit
cfs
Calculation
Daily mean
Last observation
Sep 30, 2026
Update frequency
Daily

Now 1,440 cfs, 313% above the 5-yr median.

Rio Grande at Otowi Bridge discharged 1,440 cfs, up 93% on the week and 313% above the 5-year median. The flow jumped 388% month-over-month from 295 cfs.

The numbers
PeriodCurrentPriorChange
Week over week1,440 cfs746 cfs+93.0%
Month over month1,440 cfs295 cfs+388.1%
Year over year1,440 cfs329 cfs+337.7%
vs 5-yr median1,440 cfs349 cfs+312.6%
Typical flow for this week of the year (5-year record)
ReadingDischarge
Lowest on record for this week210 cfs
Median for this week349 cfs
Highest on record for this week1,540 cfs

Previous weeks

Week of Sep 23, 2026

Rio Grande at Otowi Bridge ran at 746 cfs, up 189% on the week from 258 cfs. The gauge is 67% above its 5-year median. Flows rose 268% month over month and 114% year over year.

Week of Sep 15, 2026

Rio Grande at Otowi Bridge ran 340 cfs, up 81.8% on the week and 36.5% from a month ago. The gauge is 6% below the 5-year median, down 6.3% year over year.

Week of Sep 2, 2026

Rio Grande flow at Otowi Bridge reached 590 cfs, up 233% on the week and 39% above the 5-year median. Year over year, discharge is up 50%.

Week of Aug 26, 2026

Discharge fell to 177 cfs, down 30.9% on the week. The gauge runs 78% below the 5-year median of 803 cfs. Year-over-year, flow has dropped 57.5%.

About Rio Grande at Otowi Bridge

USGS gage 08313000 measures the Rio Grande at Otowi Bridge in northern New Mexico, below the Rio Chama confluence and above Cochiti Dam. It is the accounting gage for the Rio Grande Compact: New Mexico's delivery obligation to Texas is calculated from the flow recorded here, which makes it one of the most legally consequential streamflow stations in the country.

Above it are the San Juan-Chama transbasin diversion, which imports Colorado River water into the Rio Grande system, and El Vado and Abiquiu reservoirs on the Chama. A normal year peaks with snowmelt from the San Juan and Sangre de Cristo mountains in May, then falls through a low summer punctuated by monsoon storm pulses in July and August. A weak spring peak here has immediate legal consequences, because a shortfall accrues as compact debt that New Mexico has to repay from storage in a later year.