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ICE EFFECTS ON STREAMFLOW - During winter, ice formation may cause stage and discharge values to appear higher than expected. Ice effects may be minor (occurring only at night and early morning) with baseline flows obvious, or the effects may be major (stage constantly increases over several days or weeks) resulting in greatly erroneous discharge. Streamgages experiencing minor ice conditions will continue to display stage and discharge values to enable users to estimate the approximate base-line stage and discharge. Streamgages experiencing major ice conditions will have the discharge record temporarily disabled to prevent use of erroneous discharge values. The discharge record will resume when it is determined that ice conditions are no longer present. Daily mean discharges during periods of ice effect will be estimated after detailed data analysis.
* IMPORTANT: Next Generation Station Page

USGS 01191000 NORTH BRANCH PARK RIVER AT HARTFORD, CT

PROVISIONAL DATA SUBJECT TO REVISION

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Station operated in cooperation with the City of Hartford.

Gage is operated in conjunction with a co-located precipitation gage (station 414704072422901).

Available Parameters Available Period
  
2016-05-20  2019-12-13
2014-04-08  2019-12-13
2010-08-18  2019-12-13
2016-05-20  2019-12-13
2016-05-20  2019-12-13
2016-05-20  2019-12-13
2016-05-20  2019-12-13







 (7)
 

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Summary of all available data for this site
Instantaneous-data availability statement


Discharge, cubic feet per second

Most recent instantaneous value: 62.0 12-13-2019   07:00 EST
Graph of  Discharge, cubic feet per second

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Daily discharge, cubic feet per second -- statistics for Dec 13 based on 53 water years of record more
Min
(1947)
25th
percen-
tile
Median 75th
percen-
tile
Mean Most Recent
Instantaneous
Value Dec 13
Max
(1984)
3.90 13 20 38 50 62.0 494


Gage height, feet

Most recent instantaneous value: 2.23 12-13-2019   07:00 EST
Graph of  Gage height, feet

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