River Report

Connecticut River river

10 streamgauges 132% of normal Last updated 2026-06-16
Aggregate flow
107,988cfs
% of normal
132%
Daily volume
214,192AF
Seasonal avg
81,963cfs

Total streamflow across the Connecticut River was last observed at 107,988 cfs, and is expected to yield approximately 214,192 acre-ft of water today; about 132% of normal. River levels are high. Average streamflow for this time of year is 81,963 cfs, with recent peaks last observed on 2014-04-17 when daily discharge volume was observed at 548,550 cfs.

Maximum discharge along the river is currently at the Connecticut River At North Walpole reporting a streamflow rate of 23,500 cfs. This is also the highest stage along the Connecticut River, with a gauge stage of 14.41 ft at this location. This river is monitored from 10 different streamgauging stations along the Connecticut River, the highest being situated at an altitude of 1,211 ft, the Connecticut R Below Indian Stream Nr Pittsburg.

Max discharge

Connecticut River At North Walpole

23,500cfs
Highest stage

Connecticut River At North Walpole

14.41ft
Highest-elevation gauge

Connecticut R Below Indian Stream Nr Pittsburg

1,211ft
Aggregate trend

River streamflow levels

Daily aggregate streamflow across every monitored gauge along the Connecticut River. Use the range buttons to zoom in on a specific period.

Total streamflow

Sum of all monitored streamgauges · daily

Per-gauge breakdown

Every streamgauge along the Connecticut River

All 10 USGS gauges Snoflo tracks for this river, with current flow, stage, recent change, percent of normal, and the gauge's all-time min / max. Click any header to sort. Cells are heatmapped relative to the column min/max -- darker blue = higher.

Streamgauge Streamflow (cfs) Gauge stage (ft) 24h Δ (%) % Normal Min (cfs) Max (cfs) Elevation (ft)
Connecticut R Below Indian Stream Nr Pittsburg NH
USGS 01129200
868 3.67 68.2 229% 130 5,220 1,211
Connecticut River At North Stratford NH
USGS 01129500
4,430 6.17 185.8 463% 279 26,900 885
Connecticut River Near Dalton NH
USGS 01131500
7,690 12.75 188.0 371% 291 36,400 813
Connecticut River At Wells River VT
USGS 01138500
11,600 5.91 220.4 560% 566 41,600 403
Connecticut River At West Lebanon NH
USGS 01144500
17,600 10.74 102.8 771% 423 135,000 322
Connecticut River At North Walpole NH
USGS 01154500
23,500 14.41 135.0 392% 1,060 84,100 223
Connecticut River At Montague City MA
USGS 01170500
19,900 13.70 95.1 220% 946 126,000 111
Connecticut R At Interstate 391 Bridge At Holyoke MA
USGS 01172010
9,870 7.46 -22.3 99% 889 107,000 43
Connecticut River At Thompsonville CT
USGS 01184000
11,100 8.69 -23.5 91% 1,810 128,000 36
Connecticut R At Middle Haddam CT
USGS 01193050
1,430 3.75 -93.4 7% 32 95,400 3
Annual peaks

Maximum streamflow discharge by year

The single highest aggregate discharge recorded each year. Spotting the multi-year trend reveals droughts vs. wet cycles long before the headline daily flow does.

Annual peak discharge

From the river's full record · one point per water year

Profile

Streamflow elevation profile

Each bubble is one gauge along the river, plotted by current streamflow (x-axis) vs elevation (y-axis), sized by gauge stage. Reading top-to-bottom traces the river from headwaters down to its mouth -- you can see flow accumulate as elevation drops.

Elevation vs streamflow

One point per monitored gauge · bubble size = gauge stage

About this river

Connecticut River

The Connecticut River is the longest river in New England, stretching for 410 miles from its source in New Hampshire to its mouth at Long Island Sound. The river played a significant role in the industrial development of the region, serving as a major transportation route for goods and people. Today, the river is an important source of hydroelectric power, with several large dams and reservoirs along its length, including the Moore, Wilder, and Vernon dams. The river also supports a range of recreational activities, such as fishing, boating, and hiking, and provides water for agriculture in the Connecticut River Valley. Despite decades of pollution, the river has seen significant improvements in water quality and biodiversity in recent years due to restoration efforts.

Track the Connecticut River in the Snoflo app

Set per-gauge push alerts (e.g. "alert me when flow at the Russian R Nr Healdsburg crosses 5,000 cfs"), and Snoflo's iOS app pushes the moment USGS reports the crossing.

FAQ

About the Connecticut River

Where does the data for the Connecticut River come from?

Streamflow and gauge stage data are sourced from the U.S. Geological Survey (USGS) National Water Information System. The aggregate flow shown at the top of the page is computed by Snoflo as the sum of all monitored gauges along the river.

How is "percent of normal" calculated?

Today's aggregate streamflow is compared to the historical average aggregate streamflow on this calendar day across the river's full record. 100% means right on average; values above 100% indicate above-normal flow (wet year); values below indicate below-normal (dry year or drought).

Why are some gauges showing very different flows?

Gauges along a river measure flow at different points: headwater gauges read what's coming off the snowpack or mountain runoff; downstream gauges integrate everything upstream, including tributary inputs. Wide spreads usually mean a tributary is contributing significantly between gauges.

What's the elevation profile chart showing?

Each bubble is one gauge along the river, plotted by streamflow (x-axis) and elevation (y-axis), sized by gauge stage. Reading top-down traces the river from headwaters to mouth -- you can see flow build as elevation drops.

Can I get alerts when a specific gauge crosses a threshold?

Yes -- alerts are managed in the Snoflo iOS app on a per-gauge basis. Open any individual streamgauge from the table above and favorite it to set a discharge threshold.